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Aunque varios de los soldados del avión mueren Grivtsov y Katya se salvan milagrosamente, mientras que Linko también sobrevive luego de saltar en paracaídas del avión. Pronto cada uno debe volver hacia sus propias fuerzas, mientras que deben de realizar tareas militares y mantenerse con vida mientras los alemanes y algunos aliados los atacan. The results show that Mpgv has a smaller standard deviation in comparison to Mpga when compared with the estimated magnitudes and provides a more accurate early assessment of earthquake magnitude. We test this new method to estimate the magnitude of the Tohoku earthquake and we present the results of this estimation. PGA and PGV from borehole recordings allow us to estimate the magnitude of this event s and s after the earthquake onset, respectively. We demonstrate that the incorporation of borehole strong ground-motion records immediately available after the occurrence of large earthquakes significantly increases the accuracy of earthquake magnitude estimation and the associated improvement in earthquake and tsunami early warning systems performance. Moment magnitude versus predicted magnitude Mpga and Mpgv. Numerous studies have tried to identify the core deficit of developmental dyscalculia DD , mainly by assessing a possible deficit of the mental representation of numerical magnitude. Research in healthy adults has shown that numerosity, duration, and space share a partly common system of magnitude processing and representation. However, in DD, numerosity processing has until now received much more attention than the processing of other non-numerical magnitudes. To assess whether or not the processing of non-numerical magnitudes is impaired in DD, the performance of 15 adults with DD and 15 control participants was compared in four categorization tasks using numerosities, lengths, durations, and faces as non- magnitude -based control stimuli. Results showed that adults with DD were impaired in processing numerosity and duration, while their performance in length and face categorization did not differ from controls' performance. Our findings support the idea of a nonsymbolic magnitude deficit in DD, affecting numerosity and duration processing but not length processing. Consideration of reinforcer magnitude may be important for maximizing the efficacy of treatment for problem behavior. Nonetheless, relatively little is known about children's preferences for different magnitudes of social reinforcement or the extent to which preference is related to differences in reinforcer efficacy. The purpose of the current study was to evaluate the relations among reinforcer magnitude , preference, and efficacy by drawing on the procedures and results of basic experimenta Integration and magnitude homogenization of the Egyptian earthquake catalogue. Hussein, H. The aim of the present work is to compile and update a catalogue of the instrumentally recorded earthquakes in Egypt, with uniform and homogeneous source parameters as required for the analysis of seismicity and seismic hazard assessment. This in turn requires a detailed analysis and comparison of the properties of different available sources, including the distribution of events with time, the magnitude completeness and the scaling relations between different kinds of magnitude reported by different agencies. The observational data cover the time interval and an area between The linear regressions between various magnitude types have been evaluated for different magnitude ranges. Using the best linear relationship determined for each available pair of magnitudes , as well as those identified between the magnitudes and the seismic moment, we convert the different magnitude types into moment magnitudes M W , through a multi-step conversion process. Analysis of the catalogue completeness, based on the MW thus estimated, allows us to identify two different time intervals with homogeneous properties. De esta manera los límites este y oeste quedaron establecidos por la confluencia de los ríos antes mencionados y la localidad de Bajada del Agrio, respectivamente. We illustrate two essential consequences of the systematic difference between moment magnitude and local magnitude for small earthquakes, illuminating the underlying earthquake physics. However, the relationship between local magnitude ML and moment is itself magnitude dependent. Just as importantly, if this relation is overlooked, prediction of large- magnitude ground motion from small earthquakes will be misguided. We also consider the effect of this magnitude scale difference on b-value. The oft-cited b-value of 1 should hold for small magnitudes , given M. This is of particular import when estimating the rate of large earthquakes when one has limited data on their recurrence, as is the case for induced earthquakes in the central US. The integrated theory of numerical development posits that a central theme of numerical development from infancy to adulthood is progressive broadening of the types and ranges of numbers whose magnitudes are accurately represented. The process includes four overlapping trends: 1 representing increasingly precisely the magnitudes of non-symbolic…. We investigated the relation between children's numerical- magnitude representations and their memory for numbers. Results of three experiments indicated that the more linear children's magnitude representations were, the more closely their memory of the numbers approximated the numbers presented. This relation was present for preschoolers and…. Non extensivity and frequency magnitude distribution of earthquakes. Starting from first principles in this case a non-extensive formulation of the maximum entropy principle and a phenomenological approach, an explicit formula for the magnitude distribution of earthquakes is derived, which describes earthquakes in the whole range of magnitudes. The Gutenberg-Richter law appears as a particular case of the obtained formula. Comparison with geophysical data gives a very good agreement. Trosclair-Lasserre, Nicole M. The purpose of the current…. The link between number and space has been discussed in the literature for some time, resulting in the theory that number, space and time might be part of a generalized magnitude system. To date, several behavioral and neuroimaging findings support the notion of a generalized magnitude system, although contradictory results showing a partial overlap or separate magnitude systems are also found. The possible existence of a generalized magnitude processing area leads to the question how individuals with developmental dyscalculia DD , known for deficits in numerical-arithmetical abilities, process magnitudes. By means of neuropsychological tests and functional magnetic resonance imaging fMRI we aimed to examine the relationship between number and space in typical and atypical development. Participants were 16 adolescents with DD In the fMRI paradigm participants had to perform discrete arrays of dots and continuous magnitude angles comparisons as well as a mental rotation task. In the neuropsychological tests, adolescents with dyscalculia performed significantly worse in numerical and complex visuo-spatial tasks. However, they showed similar results to TD peers when making discrete and continuous magnitude decisions during the neuropsychological tests and the fMRI paradigm. A conjunction analysis of the fMRI data revealed commonly activated higher order visual inferior and middle occipital gyrus and parietal inferior and superior parietal lobe magnitude areas for the discrete and continuous magnitude tasks. Moreover, no differences were found when contrasting both magnitude processing conditions, favoring the possibility of a generalized magnitude system. Group comparisons further revealed that dyscalculic subjects showed increased activation in domain general regions, whilst TD peers activate domain specific areas to a greater extent. In conclusion, our results point to the existence of a. The magnitude of an earthquake is one of its basic parameters and is a measure of its scale. It plays a significant role in seismology and earthquake engineering research, particularly in the calculations of the seismic rate and b value in earthquake prediction and seismic hazard analysis. However, several current types of magnitudes used in seismology research, such as local magnitude ML , surface wave magnitude MS , and body-wave magnitude MB , have a common limitation, which is the magnitude saturation phenomenon. Fortunately, the problem of magnitude saturation was solved by a formula for calculating the seismic moment magnitude MW based on the seismic moment, which describes the seismic source strength. Now the moment magnitude is very commonly used in seismology research. However, in China, the earthquake scale is primarily based on local and surface-wave magnitudes. In the present work, we studied the empirical relationships between moment magnitude MW and local magnitude ML as well as surface wave magnitude MS in the Chinese Mainland. Therefore, in China, if the moment magnitude of an earthquake is not reported by any agency in the world, we can use the equations mentioned above for converting ML to MW and MS to MW. These relationships are very important, because they will allow the China earthquake catalogs to be used more effectively for seismic hazard analysis, earthquake prediction, and other seismology research. We also computed the relationships of and where Mo is the seismic moment by linear regression using the Global Centroid Moment Tensor. The goal of tsunami forecast, as a system for predicting potential impact of a tsunami at coastlines, requires quick estimate of a tsunami magnitude. This goal has been recognized since the beginning of tsunami research. The work of Kajiura, Soloviev, Abe, Murty, and many others discussed several scales for tsunami magnitude based on estimates of tsunami energy. However, difficulties of estimating tsunami energy based on available tsunami measurements at coastal sea-level stations has carried significant uncertainties and has been virtually impossible in real time, before tsunami impacts coastlines. The slow process of tsunami magnitude estimates, including collection of vast amount of available coastal sea-level data from affected coastlines, made it impractical to use any tsunami magnitude scales in tsunami warning operations. Uncertainties of estimates made tsunami magnitudes difficult to use as universal scale for tsunami analysis. Historically, the earthquake magnitude has been used as a proxy of tsunami impact estimates, since real-time seismic data is available of real-time processing and ample amount of seismic data is available for an elaborate post event analysis. This measure of tsunami impact carries significant uncertainties in quantitative tsunami impact estimates, since the relation between the earthquake and generated tsunami energy varies from case to case. In this work, we argue that current tsunami measurement capabilities and real-time modeling tools allow for establishing robust tsunami magnitude that will be useful for tsunami warning as a quick estimate for tsunami impact and for post-event analysis as a universal scale for tsunamis inter-comparison. We present a method for estimating the tsunami magnitude based on tsunami energy and present application of the magnitude analysis for several historical events for inter-comparison with existing methods. New moment magnitude scale, evidence of stress drop magnitude scaling and stochastic ground motion model for the French West Indies. S-waves Fourier spectra are analysed to simultaneously determine source, path and site terms. The results show that the duration magnitude routinely estimated for the events that occurred in the region underestimate moment magnitude by 0. From the inverted seismic moments and corner frequencies, we compute Brune's stress drops. We show that stress drops increase with increasing magnitude. The same pattern is observed on apparent stresses i. However, the rate of increase diminishes at high magnitudes , which is consistent with a constant stress drop model for large events. Using the results of the inversions, we perform ground motion simulations for the entire data set using the SMSIM stochastic simulation tool. Although the magnitude -dependent stress drop model is giving better results than the constant stress drop model, the interevent variability remains high, which could suggest that stress drop depends on other parameters such as the depth of the hypocentre. In any case, the overall variability is of the same order of magnitude as usually observed in empirical ground motion prediction equations. This event is larger than previous one in terms of magnitude and showed that measured magnitude strongly depends on the frequency band of data. Relative spectral magnitude varies with frequencies and decreases as frequency increase. A methodology is presented for determining mb Pn magnitude of underground nuclear explosions from local Pn phase. The mb Pn estimates of regional events for Korean Peninsula are determined to be mb Pn? Systematic non-linearity does not observed at frequency band from 0. The magnitude of 6th event is mb Pn 6. Further research of applicable mb Pn magnitude scaling is required for all frequency band and. The bolometric, infrared and visual absolute magnitudes of Mira variables. Statistical parallaxes, as well as stars with individually known distances are used to derive bolometric and infrared absolute magnitudes of Mira Me variables. The derived bolometric magnitudes are in the mean about 0. The problem of determining the pulsation constant is discussed. Miras with periods greater than days probably pulsate in the first overtone. Those of shorter periods are anomalous and may be fundamental pulsators. It is shown that the absolute visual magnitudes at mean light of Miras with individually determined distances are consistent with values derived by Clayton and Feast from statistical parallaxes. Potencial del Agua del suelo. Full Text Available La energía potencial del agua presenta diferencias de un punto del suelo a otro; esas diferencias son las que originan el movimiento del agua de acuerdo a la tendencia universal de la materia en el sentido de moverse de donde la energía potencial es mayor a donde dicha energía es menor. En el suelo el agua en consecuencia se mueve hacia donde su energía decrece hasta lograr su estado de equilibrio. Se desprende entonces que la cantidad de energía potencial absoluta contenida en el agua, no es importante por sí misma, sino por su relación con la energía en diferentes lugares dentro del suelo. El concepto Potencial de agua del suelo es un criterio para esta energía. On the magnitude and recurence of Vrancea earthquakes. The moment- magnitude scale Msub W is proposed for the quantification of Vrancea earthquakes. The asperity model is found adequate to explain the observed quasi-cycles and super-cycles in the occurrence of large events. Disparities in the Magnitude of Human Immunodeficiency Virus HICs while tuberculosis, candidiasis, chronic diarrhea, and cryptococcosis were predominant Mohar A. Magnitude and factors associated with post-cesarean surgical site Magnitude and factors associated with post-cesarean surgical site infection at Hawassa University Teaching and referral hospital, southern Ethiopia: a Thus, it should be averted by implementing infection prevention techniques. Rapid earthquake magnitude determination for Vrancea early warning system. Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude from the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in order to avoid false alarms. A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into account that it is computed from only 3 stations in a very short time interval. Impact of magnitude uncertainties on seismic catalogue properties. Catalogue-based studies are of central importance in seismological research, to investigate the temporal, spatial and size distribution of earthquakes in specified study areas. Methods for estimating the fundamental catalogue parameters like the Gutenberg-Richter G-R b-value and the completeness magnitude Mc are well established and routinely applied. However, the magnitudes reported in seismicity catalogues contain measurement uncertainties which may significantly distort the estimation of the derived parameters. In this study, we use numerical simulations of synthetic data sets to assess the reliability of different methods for determining b-value and Mc, assuming the G-R law validity. After contaminating the synthetic catalogues with Gaussian noise with selected standard deviations , the analysis is performed for numerous data sets of different sample size N. The noise introduced to the data generally leads to a systematic overestimation of magnitudes close to and above Mc. This fact causes an increase of the average number of events above Mc, which in turn leads to an apparent decrease of the b-value. This may result to a significant overestimation of seismicity rate even well above the actual completeness level. The b-value can in general be reliably estimated even for relatively small data sets N magnitudes higher than the actual completeness level are used. Nevertheless, a correction of the total number of events belonging in each magnitude class i. Because magnitude uncertainties here with the form of Gaussian noise are inevitable in all instrumental catalogues, this finding is fundamental for seismicity rate and seismic hazard assessment analyses. Also important is that for some data analyses significant bias cannot necessarily be avoided by choosing a high Mc value for analysis. Qué frío!!! Yo incluso me puse mi chaqueta finita de plumas… Qué bien que me la traje!!! Ascender dunas es igual de cansino que montañas con nieve!!! Y llevad agua! Seguíamos los pasos de David, técnico de montaña, y en min. A mí no me apetecía dormir, así que fui a relacionarme con los dromedarios. Cuando volví, todos ya estaban preparados para visitar el pueblo cercano, a aprox. La verdad es que fue muy interesante: hay técnicas puras y mixtas, todos los materiales son naturales y alfombras creadas por mujeres de la zona. Aunque otra gente os diga que si que hay y es precioso! Translation Behav Med. An evaluation of a self-management program for patients with long-term conditions. Patient Educ Counsel. Relationship between health-disease process and cross-cultural care: contributions to nursing care. Rev Pesqui Cuidado Fundam. Application of telenursing in nursing practice: an integrative literature review. Appl Nurs Res. Information and communication technology and the prevention of diseases - literature review. Rev Pesq Cuid. PAIN Reports, ; e Rev Bras Ativ Saude. Obesity and socioeconomic status in developing countries: a systematic review. Obesity Rev. Gender-specific demographic factors and lifestyle habits related to physical inactivity. Rev Nutr. Physical exercises as a strategy to prevent and to treat obesity: physiological and methodological aspects. Women's meal frequency and nutritional and health profiles. Rev Esp Cardiol. Obesity, insulin resistance and comorbidities? Mechanisms of association..

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Sexi pipka Um das Video zu sehen, muss Javascript aktiviert werden. Free sext. Debía de ser nuestro día de suerte! En Rissani ya empezaba nuestra aventura organizada. Dejamos las mochilas en el maletero y fuimos a dar un paseo por el mercado, ya que justo fue el día apropiado! A parte de típicos puestos de todos los colores, fuimos a ver el mercado de animales domésticos y parking de burros! El hit de nuestra visita fue encargar la pizza bereber leímos sobre esta pizza en una de las guías. Para pedirla, hay un cierto ritual que hay que seguir: hay que comprar la carne que quieras al carnicero, y el se encarga de mandar a un niño al de la verdura y luego a la paderia y traerla de vuelta al carnicero en unos 40 min. Pagamos 10o Dhs entre 6, pero era tan grande que nos costó acabarla!!! Sobre las Bueno, si no os da cosa dormir en la cama donde duermen todos, ni hace falta el saco. Este aviso fue puesto el 13 de enero de Vitaliy Vorobyov. Ver todos los créditos IMDb. Six rectangular light-emitting diodes with independently adjustable duty cycles represent stars of magnitudes 1 through 6. Experimentally verifies the logarithmic response of the eye. Full Text Available La investigación contable orientada al mercado de capitales ha vuelto a dirigir recientemente su interés hacia los modelos de valoración de acciones. Este cambio se ha venido produciendo de manera paralela a la constatación empírica de la existencia de numerosas anomalías en el comportamiento del mercado y la capacidad de las variables contables para explicar las diferencias en las rentabilidades obtenidas por los títulos en el mercado. Todo ello ha propiciado el diseño y desarrollo de estrategias de inversión que permitían obtener rentabilidades anormales positivas. La determinación del valor intrínseco pasa necesariamente por el establecimiento de un modelo de valoración. El objetivo de este trabajo es analizar los fundamentos conceptuales del MRR. Después de indicar sus ventajas en comparación con los modelos tradicionales de valoración, nos centramos en la descripción de sus limitaciones tanto desde un punto de vista teórico como empírico. Esta mudança tem ocorrida de forma. Full Text Available OBJECTIVE: The present study sought to: a categorize youths into groups based on their level of alcohol use and number of symptoms of alcohol abuse and dependence defined in the Diagnostic and Statistical Manual of Mental Disorders DSM-IV, and b examine whether these categories were associated with other problem behaviors in which youths engage marijuana use, sexual intercourse, and having been arrested or having trouble with the law. Youths were categorized based on their alcohol use and alcohol problems. These categories were then examined for associations with lifetime marijuana use, lifetime sexual intercourse, and having been arrested or having had trouble with the law in the past year. The original eight categories of alcohol use were collapsed into six categories based on the results. RESULTS: For virtually every group characterized by higher severity of alcohol use and alcohol problems, researchers found an increasing prevalence of marijuana use in their lifetimes, increasing odds of sexual intercourse in their lifetimes, and having had trouble with the law in the past year. Scaling relations of moment magnitude , local magnitude , and duration magnitude for earthquakes originated in northeast India. In this study, we aim to improve the scaling between the moment magnitude M W , local magnitude M L , and the duration magnitude M D for earthquakes in Shillong-Mikir plateau and its adjoining region of northeast India by extending the M W estimates to lower magnitude earthquakes using spectral analysis of P-waves from vertical component seismograms. The scaling relationships investigated comply well with similar relationships in other regions in the world and in other seismogenic areas in the northeast India region. National Oceanic and Atmospheric Administration, Department of Commerce — These data contain shipboard current magnitudes and directions collected in the Pacific, both pelagic and near shore environments. Data is collected using an RD Magnitude conversion to unified moment magnitude using orthogonal regression relation. Homogenization of earthquake catalog being a pre-requisite for seismic hazard assessment requires region based magnitude conversion relationships. Linear Standard Regression SR relations fail when both the magnitudes have measurement errors. In this paper a technique is proposed for using such OSR for preparation of homogenized earthquake catalog in moment magnitude Mw. For derivation of orthogonal regression relation between mb and Mw, a data set consisting of events with observed body wave magnitudes mb,obs and moment magnitude Mw,obs values has been taken from ISC and GCMT databases for Northeast India and adjoining region for the period Firstly, an OSR relation given below has been developed using mb,obs and Mw,obs values corresponding to events from this data set. A linear relation is then developed between these mb,obs values and corresponding mb,proxy values given by the OSR line using orthogonality criterion. The accuracy of the above procedure has been checked with the rest of the data i. The improvement in the correlation coefficient value between mb,obs and Mw estimated using the proposed procedure compared to the correlation coefficient value between mb,obs and Mw,obs shows the advantage of OSR relationship for homogenization. The OSR procedure developed in this study can be used to homogenize any catalog containing various magnitudes e. The proposed procedure also remains valid in case the magnitudes have measurement errors of different orders, i. Absolute magnitudes by statistical parallaxes. As additional output, the algorithm provides one also with the dispersion in magnitude of the sample sigmasub M , the mean solar motion U,V,W and the corresponding velocity ellipsoid sigmasub u , sigmasub v , sigmasub w. The use of this algorithm is illustrated. Understanding Magnitudes to Understand Fractions. Fractions are known to be difficult to learn and difficult to teach, yet they are vital for students to have access to further mathematical concepts. This article uses evidence to support teachers employing teaching methods that focus on the conceptual understanding of the magnitude of fractions. The authors report four clinical cases of congenital lobar emphysema in the newborn. The chest x-ray at admission was suggestive of CLE and the diagnosis was confirmed by computorized tomography. The CLE affected the right upper lobe in three cases and the medium lobe in one case. All patients were treated with lobectomy. The pathological study of the surgical specimens confirmed the diagnosis in the four cases, and revealed hypoplasia of the bronquiolar tree cartilage in three. Conclusions: Our series is. The language of magnitude comparison. When two objects differ in magnitude , their relation can be described with a "smaller" comparative e. We show that, across multiple dimensions and tasks, English speakers preferentially use the latter. In sentence-completion tasks, this higher use of larger comparatives HULC effect is more pronounced when the larger item is presented on the left for simultaneous presentation or second for sequen Radiation doses - maps and magnitudes. These include the medical use of radiation, radioactive discharges to the environment, cosmic rays, gamma rays from the ground and buildings, radon gas and food and drink. A Pie chart represents the percentage contribution of each of those sources. Finally, the terms becquerel, microsievert and millisievert are explained. Solar Variability Magnitudes and Timescales. The former are directly observed as part of the on-going year long total solar irradiance climate data record, while the latter are inferred from solar proxy and stellar evolution models. Total solar irradiance has been measured from space since by a series of overlapping instruments. The year solar cycle has comparable irradiance variations with peaks near solar maxima. Secular variations are harder to discern, being limited by instrument stability and the relatively short duration of the space-borne record. Proxy models of the Sun based on cosmogenic isotope records and inferred from Earth climate signatures indicate solar brightness changes over decades to millennia, although the magnitude of these variations depends on many assumptions. Stellar evolution affects yet longer timescales and is responsible for the greatest solar variabilities. Theoretical considerations and empirical regressions show that, in the magnitude range between 3 and 5, local magnitude , ML, and moment magnitude , Mw, scale Previous studies suggest that for smaller magnitudes this scaling breaks down. Magnitude determination for large underground nuclear explosions. A method is presented for determining the local magnitudes for large underground nuclear explosions. The Gutenberg-Richter nomograph is applied to the peak amplitudes for 24 large underground nuclear explosions that took place in Nevada. The amplitudes were measured at 18 California Wood-Anderson stations located km from the explosion epicenter. The variation of the individual station magnitudes and magnitude corrections and the variation of the average and rms error estimates in the magnitude determinations are examined with respect to distance, azimuth, and event location. The magnitude prediction capability of the Gutenberg-Richter nomograph is examined on the basis of these two criteria, and certain corrections are suggested. The azimuthal dependence of the individual station magnitudes is investigated, and corrections for the California stations are calculated. Statistical weighting schemes for two-component data are employed, and the assumptions and limitations in the use of peak amplitudes are discussed. Extreme value distribution of earthquake magnitude. Probability distribution of maximum earthquake magnitude is first derived for an unspecified probability distribution of earthquake magnitude. A model for energy release of large earthquakes, similar to that of Adler-Lomnitz and Lomnitz, is introduced from which the probability distribution of earthquake magnitude is obtained. An extensive set of world data for shallow earthquakes, covering the period from to , is used to determine the parameters of the probability distribution of maximum earthquake magnitude. Because of the special form of probability distribution of earthquake magnitude , a simple iterative scheme is devised to facilitate the estimation of these parameters by the method of least-squares. The agreement between the empirical and derived probability distributions of maximum earthquake magnitude is excellent. The children's pretest numerical magnitude representations were found to be correlated with their pretest arithmetic knowledge and to be…. Representations of the Magnitudes of Fractions. We tested whether adults can use integrated, analog, magnitude representations to compare the values of fractions. The only previous study on this question concluded that even college students cannot form such representations and instead compare fraction magnitudes by representing numerators and denominators as separate whole numbers. Magnitude of localized magnetic moments in metals. The magnitude of the localized magnetic moment of a transition or rare earth element impurity in a metal is evaluated within the framework of the Anderson model. Rotational invariance is preserved throughout. Graphs of the magnitude of the magnetization as a function of the relevant parameters of the model are provided and discussed. Local magnitudes of small contained explosions. The relationship between explosive yield and seismic magnitude has been extensively studied for underground nuclear tests larger than about 1 kt. For monitoring smaller tests over local ranges within km , we need to know whether the available formulas can be extrapolated to much lower yields. Here, we review published information on amplitude decay with distance, and on the seismic magnitudes of industrial blasts and refraction explosions in the western U. Next we measure the magnitudes of some similar shots in the northeast. We find that local magnitudes ML of small, contained explosions are reasonably consistent with the magnitude -yield formulas developed for nuclear tests. These results are useful for estimating the detection performance of proposed local seismic networks. Discounting Behaviour and the Magnitude Effect. We evaluate the claim that individuals exhibit a magnitude effect in their discounting behaviour, where higher discount rates are inferred from choices made with lower principals, all else being equal. If the magnitude effect is quantitatively significant, it is not appropriate to use one discount Using data from a field experiment in Denmark, we find statistically significant evidence of a magnitude effect that is much smaller than is claimed. This evidence surfaces only if one controls Determination of the Meteor Limiting Magnitude. The limiting meteor magnitude of a meteor camera system will depend on the camera hardware and software, sky conditions, and the location of the meteor radiant. Some of these factors are constants for a given meteor camera system, but many change between meteor shower or sporadic source and on both long and short timescales. Since the limiting meteor magnitude ultimately gets used to calculate the limiting meteor mass for a given data set, it is important to have an understanding of these factors and to monitor how they change throughout the night, as a 0. The Magnitude of Atherogenic Dyslipidaemia among Geriatric June on consecutive geriatric patients with systemic hypertension Measuring radon source magnitude in residential buildings. A description is given of procedures used in residences for rapid grab-sample and time-dependent measurements of the air-exchange rate and radon concentration. The radon source magnitude is calculated from the results of simultaneous measurements of these parameters. Grab-sample measurements in three survey groups comprising US houses showed the radon source magnitude to vary approximately log-normally with a geometric mean of 0. Successive measurements in six houses in the northeastern United States showed considerable variability in source magnitude within a given house. In two of these houses the source magnitude showed a strong correlation with the air-exchange rate, suggesting that soil gas influx can be an important transport process for indoor radon. Comparar esse sistema a um sistema computacional de acesso livre. Time series of increments can be created in a number of different ways from a variety of physical phenomena. For example, in the phenomenon of volatility clustering-well-known in finance- magnitudes of adjacent increments are correlated. Here we define a model-independent test to measure the statistical significance of any observed asymmetry. We propose a simple stochastic process characterized by a an asymmetry parameter lambda and a method for estimating lambda. We illustrate both the test and process by analyzing physiological data. Local magnitude , duration magnitude and seismic moment of Dahshour earthquakes. Full Text Available Local magnitudes ML have been calculated for 56 earthquakes of the Dahshour sequence using simulated records of the KEG broadband station and the estimated calibration function of the Dahshour area. These were compared with their corresponding values of duration magnitudes obtained from the analog short period seismograms of the HLW station. Seismic moment has also been estimated for these events using simple measurements from the time domain records. These measurements based on the simulated Wood Anderson seismograms are used for the local magnitude ML estimation. The moment magnitude Mw and the energy magnitude Me: common roots and differences. Abstract Starting from the classical empirical magnitude -energy relationships, in this article, the derivation of the modern scales for moment magnitude Mw and energy magnitude Me is outlined and critically discussed. The formulas for Mw and Me calculation are presented in a way that reveals, besides the contributions of the physically defined measurement parameters seismic moment M0 and radiated seismic energy ES, the role of the constants in the classical Gutenberg? Richter magnit Colour- magnitude diagram of NGC The electronographic observations were obtained with an experimental Spectracon image-converter, having photocathode and exit window dimensions of 20 x 30 mm, mounted at the prime-focus of the in. Lick reflector. The photographic observations were obtained with the in. Carnegie astrograph and the in. Crossley reflector. The colour- magnitude diagram resembles that of M92, with the difference that a red horizontal branch is more pronounced than the asymptotic branch in NGC The topology of the horizontal branch is that of clusters with an intermediate metal content and is thus at variance with the mean period of the RR Lyr stars and the unreddened colour of the subgiant branch read at the magnitude level of the horizontal branch, both of which would indicate an extremely low metal content. Psychiatr Clin North Am. Adv Nutr. Trends in prevalence of overweight and obesity in adults in 26 Brazilian state capitals and the Federal District from to Rev Bras Epidemiol. Obesity: a plural perspective. Maintenance of weight loss or stability in subjects with obesity: a retrospective longitudinal analysis of a real-world population. Curr Med Res Opinion. Determinants of adherence to lifestyle intervention in adults with obesity: a systematic review. Clin Obes. 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Xxx Lukerya All Best Videos New Videos. Der wird mit Sicherheit neugierig darauf sein, welche Omas mehrfacher Orgasmus er zukünftig mit seiner Partnerin erleben könnte. Las niñas disfrutan la idea Video Porn cam. Localización de hipocentros y determinación de su magnitud en Tierra del Fuego y zonas aledañas. Full Text Available Nuevos hipocentros de sismos de baja a mediana magnitud han sido calculados con el fin de estudiar la sismicidad en la Isla de Tierra del Fuego y zonas aledañas. La región presenta un complejo escenario tectónico: la isla es atravesada por una falla transformante conocida como Falla de Magallanes-Fagnano la cual divide a Tierra del Fuego en dos bloques continentales. Esta falla constituye el mayor segmento continental del borde de las placas de Scotia y Sudamericana. A tal efecto se analizaron los registros de 5 estaciones sismológicas para el período enero - diciembre La mayoría de los sismos tienen un valor de magnitud mb que se concentra entre 2 y 4 grados. New hypocentre locations of earthquakes with low to medium magnitude have been calculated in. Full Text Available O enfisema pulmonar é um processo inflamatório pulmonar e tem repercussões extrapulmonares. O objetivo desta pesquisa é investigar os efeitos da laserterapia nessas alterações extrapulmonares. O diagnóstico clínico é confirmado por exames radiológicos simples. O tratamento de escolha nos casos graves é a lobectomia, que apresenta resultados superiores ao tratamento clínico. Nosso propósito é relatar um caso desta rara patologia em lactente atendida em nosso serviço com quadro de insuficiência respiratória grave, sendo submetida a exames complementares tendo diagnóstico presuntivo de ELC. Congenital Lobar Emphysema CLE is a rare malformation of lung development, which may be the cause of respiratory insufficiency in the suckling child. It is produced by the hyperinsufflation of one or more lung lobs with compression of the normal lung parenchyma and contralateral displacement of the mediastinum. Clinical diagnosis is confirmed by simple radiology exams. Lobectomy has better results than clinical treatment and should be chosen. Our purpose is to present one case of this rare illness in a newborn seen in our service with serious respiratory insufficiency and after complementary exams, CLE was confirmed. The patient was submitted to a surgical procedure lobectomy with an excellent post surgery evolution. Child is asymptomatic in long term follow up. Magnitudes y tendencias de la desnutrición en la niñez argentina durante la primera década del siglo XXI. Full Text Available En este artículo se presentan las principales magnitudes y tendencias que caracterizan a la desnutrición en la niñez argentina en los primeros años del siglo XXI. Para abordar este problema se elaboró un indicador denominado Tasa Integral de Mortalidad por Desnutrición en la Niñez TIMDN; se trata de un indicador de mortalidad que incluye tanto las causas directas de desnutrición Kwashiorkor, marasmo, etc. Se destacan entre estas causas las patologías infecciosas, diarreas, sarampión, parasitismo, bronquiolitis, neumonía, entre otras. En efecto, pudo observarse que, mientras la tasa nacional disminuyó, operaron diferentes comportamientos tanto regionales, con distintas magnitudes y tendencias, como provinciales, con algunos casos incluso de estancamiento y aumento de la desnutrición; esto resulta contrario a lo operado en el marco nacional y relacionado con un proceso de contra-transición epidemiológica señalado para el caso argentino. Enfisema subcutâneo maciço - Tratamento com drenos subcutâneos Massive subcutaneous emphysema - Management using subcutaneous drains. Na maior parte dos casos apenas causa sintomatologia minor e o tratamento é habitualmente conservador. Massive subcutaneous emphysema is a relatively common complication in invasive techniques, surgical practice and some medical conditions. Subcutaneous emphysema is usually treated conservatively and may only cause minimal symptoms. Even when it is severe, subcutaneous emphysema rarely has pathophysiologic consequences, but it is extremely uncomfortable for the patient. The authors report a case of massive and rapid developing subcutaneous emphysema following chest tube displacement in a patient with spontaneous secondary pneumothorax and large air leak. The emphysema was treated with two subcutaneous drains, inserted using local anesthesia, on both sides of the chest antero-superior thoracic wall, connected to drainage bags. The drains produced a dramatic clinical improvement and provided effective decompression of the subcutaneous emphysema. In this clinical case, the. Didactic revision of the operative magnitudes system ICRU for the evaluation of the equivalent dose in radiation external fields; Revision didactica del sistema de magnitudes operativas ICRU para la evaluacion de la dosis equivalente en campos externos de radiacion. Alvarez R, J. The objective is to present the basic concepts of the dosimetry for radiation external fields with purposes of radiological protection, because the assimilation lack and technological development of this dosimetric magnitudes system has persisted for near 50 years, in terms of practice of the radiological protection in Mexico. Rev Port Pneumol ; XVI 2: Abstract: Massive subcutaneous emphysema is a relatively common complication in invasive techniques, surgical practice and some medical conditions. The drains. Magnitude , tendência temporal e fatores associados à anemia em crianças do Estado da Paraíba Magnitud , tendencia temporal y factores asociados a la anemia en niños del Estado de Paraíba Magnitude , time trends and factors associate with anemia in children in the state of Paraíba, Brazil. Se consideraron para anemia valores OBJECTIVE: To estimate the magnitude of the anemia, to analyze the time trends and investigate the factors associated with this disturbance in children in the state of Paraíba, Brazil. Hemoglobin Hb in venous blood was analyzed with an automatic counter. The social-economic and demographic characteristics of children were obtained by questionnaire. Proportions were compared by Pearson's chi-squared test, and the association between hemoglobin concentrations and potential risk factors was tested by regression model Poisson. Atualmente, o enfisema é a quarta causa de morte nos EUA, afetando 14 milhões de pessoas. O presente artigo descreve as principais ferramentas no diagnóstico por imagem do enfisema , desde o início até os dias de hoje. Emphysema is a condition of the lung, characterized by the abnormal increase in the size of the airspace distal to the terminal bronchioles. Currently, emphysema is the fourth leading cause of death in the USA, affecting 14 million people. The present article describes the principal tools in the imaging diagnosis of emphysema, from the early days until the present. We describe traditional techniques, such as chest X-ray, together with the evolution of computed tomography CT to more advanced forms, such as high resolution CT, as well as three-dimensional CT densitometry and volumetric assessment. Teleseismic magnitude relations. Full Text Available Using available sets of magnitude determinations, primarily from Uppsala seismological bulletin, various extensions are made of the Zurich magnitude recommendations of Thus, body-wave magnitude m and surface-wave magnitudes M are related to each other for 12 different earthquake regions as well as world-wide. Depth corrections for M are derived for all focal depths. Formulas are developed which permit calculation of M also from vertical component long-period seismographs. Body-wave magnitudes from broad-band and narrow-band short-period seismographs are compared and relations deduced. Applications are made both to underground nuclear explosions and to earthquakes. The possibilities of explosion-earthquake discrimination on the basis of magnitudes are examined, as well as the determination of explosive yield from magnitudes. For earthquakes, relations between magnitudes of main earthquakes and largest aftershocks are investigated. A world-wide station network for more homogeneous magnitude determinations is suggested in order to provide the necessary reference system. Conducta anestésica en un lactante con enfisema lobar congénito Behavior of anesthesia in an infant with congenital lobar emphysema. Full Text Available Se presenta el caso clínico de un lactante con enfisema lobar congénito, tratado en el Hospital Infantil Sur de Santiago de Cuba con antecedentes de cuadros respiratorios recurrentes y varias hospitalizaciones previas. The case of an infant with congenital lobar emphysema is reported, who was treated in the Southern Children Hospital of Santiago de Cuba with history of recurrent respiratory symptoms and several previous hospitalizations. Initially he was admitted with bronchopneumonia and dyspnea, and the presence of pneumothorax was suspected, but a definitive diagnosis was obtained by radiological studies and surgical treatment was decided. Se observó una acción modificadora excelente para 0. El estroncio, sinembargo, mostró un efecto de la modificación muy duradero aproximadamente 3 h. Otro hallazgo interesante es laexistencia de un cierto periodo de incubación de aproximadamente 90 minutos después de agregar Sr. Although all these elements and combinations tend to counteract substantially the shrinkage formation, Sr appeared to bethe most effective to decrease top macro shrinkage whereas the combination Na-Ti led to the least formation of lateralmacro shrinkage. An excellent modifying action was observed for 0. However, strontiumshowed a very lasting modification effect about 3 h. Another interesting. Os volumes pulmonares foram normais em 7 pacientes. OBJECTIVE: To describe the clinical and functional findings recently reported in the medical literature for patients diagnosed with emphysema involving the upper lobes and idiopathic pulmonary fibrosis IPF involving the lower lobes. Moment magnitude scale. El objetivo de este experimento fue escalonar la percepción social del enfermero por los métodos de estimación de magnitudes y de categorías. Participaron alumnos de la enseñanza fundamental y de universidades, profesionales actuantes y jubilados en medicina, psicología, enfermería y odontología. This experiment aimed to rank nurses' social perception through the magnitude and category estimation methods. Study participants were high school and university students, active and retired professionals in the areas of medicine, psychology, nursing and dentistry. The results showed: 1 the characteristics neat, responsible, clean, careful and efficacious occupied the first positions in terms of nurses' social perception; whereas the characteristics useless, dishonorable, irresponsible and hateful occupied the. Right idea, wrong magnitude system. Leibovich et al. Evaluación de los beneficios del Método Mézières incluido al programa de fisioterapia respiratoria de los pacientes con enfermedad pulmonar obstructiva crónica. La Enfermedad Pulmonar Obstructiva Crónica EPOC , es un trastorno respiratorio causado mayoritariamente por el tabaquismo y caracterizado por una obstrucción progresiva y parcialmente reversible de las vías respiratorias, hiperinflación pulmonaria, manifestaciones sistémicas, expectoración anormal. Es la tercera causa de mortalidad en el mundo y se clasifica en 2: el enfisema y la bronquitis crónica. Nos centraremos en el aumento de deformaciones posturales, de la ansiedad y del dolor, la di Moment Magnitude discussion in Austria. A Moment Magnitude Catalogue was generated and compared with the Austrian Earthquake Catalogue and all available Magnitude solution of the neighbouring agencies. Integrated Circuit Stellar Magnitude Simulator. Describes an electronic circuit which can be used to demonstrate the stellar magnitude scale. Six rectangular light-emitting diodes with independently adjustable duty cycles represent stars of magnitudes 1 through 6. Experimentally verifies the logarithmic response of the eye. Full Text Available La investigación contable orientada al mercado de capitales ha vuelto a dirigir recientemente su interés hacia los modelos de valoración de acciones. Este cambio se ha venido produciendo de manera paralela a la constatación empírica de la existencia de numerosas anomalías en el comportamiento del mercado y la capacidad de las variables contables para explicar las diferencias en las rentabilidades obtenidas por los títulos en el mercado. Todo ello ha propiciado el diseño y desarrollo de estrategias de inversión que permitían obtener rentabilidades anormales positivas. La determinación del valor intrínseco pasa necesariamente por el establecimiento de un modelo de valoración. El objetivo de este trabajo es analizar los fundamentos conceptuales del MRR. Después de indicar sus ventajas en comparación con los modelos tradicionales de valoración, nos centramos en la descripción de sus limitaciones tanto desde un punto de vista teórico como empírico. Esta mudança tem ocorrida de forma. Full Text Available OBJECTIVE: The present study sought to: a categorize youths into groups based on their level of alcohol use and number of symptoms of alcohol abuse and dependence defined in the Diagnostic and Statistical Manual of Mental Disorders DSM-IV, and b examine whether these categories were associated with other problem behaviors in which youths engage marijuana use, sexual intercourse, and having been arrested or having trouble with the law. Youths were categorized based on their alcohol use and alcohol problems. These categories were then examined for associations with lifetime marijuana use, lifetime sexual intercourse, and having been arrested or having had trouble with the law in the past year. The original eight categories of alcohol use were collapsed into six categories based on the results. RESULTS: For virtually every group characterized by higher severity of alcohol use and alcohol problems, researchers found an increasing prevalence of marijuana use in their lifetimes, increasing odds of sexual intercourse in their lifetimes, and having had trouble with the law in the past year. Scaling relations of moment magnitude , local magnitude , and duration magnitude for earthquakes originated in northeast India. In this study, we aim to improve the scaling between the moment magnitude M W , local magnitude M L , and the duration magnitude M D for earthquakes in Shillong-Mikir plateau and its adjoining region of northeast India by extending the M W estimates to lower magnitude earthquakes using spectral analysis of P-waves from vertical component seismograms. The scaling relationships investigated comply well with similar relationships in other regions in the world and in other seismogenic areas in the northeast India region. National Oceanic and Atmospheric Administration, Department of Commerce — These data contain shipboard current magnitudes and directions collected in the Pacific, both pelagic and near shore environments. Data is collected using an RD Magnitude conversion to unified moment magnitude using orthogonal regression relation. Homogenization of earthquake catalog being a pre-requisite for seismic hazard assessment requires region based magnitude conversion relationships. Linear Standard Regression SR relations fail when both the magnitudes have measurement errors. In this paper a technique is proposed for using such OSR for preparation of homogenized earthquake catalog in moment magnitude Mw. For derivation of orthogonal regression relation between mb and Mw, a data set consisting of events with observed body wave magnitudes mb,obs and moment magnitude Mw,obs values has been taken from ISC and GCMT databases for Northeast India and adjoining region for the period Firstly, an OSR relation given below has been developed using mb,obs and Mw,obs values corresponding to events from this data set. A linear relation is then developed between these mb,obs values and corresponding mb,proxy values given by the OSR line using orthogonality criterion. The accuracy of the above procedure has been checked with the rest of the data i. The improvement in the correlation coefficient value between mb,obs and Mw estimated using the proposed procedure compared to the correlation coefficient value between mb,obs and Mw,obs shows the advantage of OSR relationship for homogenization. The OSR procedure developed in this study can be used to homogenize any catalog containing various magnitudes e. The proposed procedure also remains valid in case the magnitudes have measurement errors of different orders, i. Absolute magnitudes by statistical parallaxes. As additional output, the algorithm provides one also with the dispersion in magnitude of the sample sigmasub M , the mean solar motion U,V,W and the corresponding velocity ellipsoid sigmasub u , sigmasub v , sigmasub w. The use of this algorithm is illustrated. Understanding Magnitudes to Understand Fractions. Fractions are known to be difficult to learn and difficult to teach, yet they are vital for students to have access to further mathematical concepts. This article uses evidence to support teachers employing teaching methods that focus on the conceptual understanding of the magnitude of fractions. The authors report four clinical cases of congenital lobar emphysema in the newborn. The chest x-ray at admission was suggestive of CLE and the diagnosis was confirmed by computorized tomography. The CLE affected the right upper lobe in three cases and the medium lobe in one case. All patients were treated with lobectomy. Guerra , Acción , Drama , Romance. Chapitel FILM. UA Group. Y respon- irbol de Navidad. Nochebe- ovaco6n. Con siler. Silencio de ,sion. La conser- manigua. La e familiar al fifie, estrellas con suS colas lumI- n es temblor e nosas, se han convertido en ,efia con ella en palmas reales. El sol de me- Congas, rumbas. Comor para u- La vaca y la multl. Y [aria se palpa la bendita realidad pequehita. Incon- nso un rosal Y rebiblemente humana. Paz ria sofocada. Esta ira- sfuerzo sobrehu- se que Bernanos aeerte a po- iisculos tensos se ner en la boca moribunda de flor de piel' v su cure de Campagne, cae uvo sombra Mu- sobre las almas abiertas. En paza descansar y esta nocheblanca. Sociedad El fin de af4o en los clubs. Ia que en cads ry Vallhonrat y Pando, una club, tendri exceptional bri- aeiorita atractivisima. Prime- jnven Raoe1l Rodriguez Ca- ranente nos ieferiremosa a barrocas. Tulane, en Nueva Orleans. Este compromise se forma- Se desarrollara en la espa. En el Habana novia. Felici- la noche a cuatro de la ma- dades. Se' serviri un ex- quisito mend y se bailara con dos orquestas de primer orden debiendo asistir las seforas de traje corto y los caballeros de traje corriente. Grandiosa bajo todos sus as- pectos sera la fiesta del Ha- vana Biltmore Yacht and Country Club donde su di- rectiva viene hacienda puLl- tiple preparatives. Para la mejor organizacion del event se ruega iacar las reservacio- nes con Ia debida anticipa- tion. El ador- no estara a cargo del cono- i crdo decorador Cajaravilla y se extender. A medianoche -ie seavira una magnifica ce- na y el baile reinara dese l piimera hora con las orques- tas Kubavana v Sensaci6n '' debiendo asistir los caballe- ru- de eltoueta. El domingo diecisiete del enti ante mes de enero. Beatriz Solis e Hidal- ' go Gato, con e' joven Agus-. En la clinic del reparto Miramar ha da- do a luz una linda nifa Isa sefiora Margarita Gonmez t Diago. De acuerdo con la rostumbre los padres del novio. Muchos iexlos le deseasmos a tan important cargo. Ir fue rfrecido un animado "party" de tespedida al asiitnm ico t. ManIolo Mario Mori. Juan Manuel Tapia. Miguel Angel Pantagua. Hector Ro- driguez y Armando Codina. Curios G. En esos dias memor. Mendoza se complace en ofrecer una series de atractivos pars todos los gustos r oars to- dos loe olsitillos. El dia de Navidad estrenardn estos lindos models de FAYA Todo en illos es primoroso: los colors, los detalles, los bordados DiseAidos, confeccionados y adornados en nuestros propios talleres, constituven verdaderas creaciones. Son los tstidos de fiesta que used preferird para iodas sus nineas. Trdigalas a sriros. Jiias: Termr piew. D di Ialia Tamom fasn nw l a roes DJl 34 at Salomon Stenz n. Trtde el pas o dl fecmiento ee- a o y de rept e Yok or cdotraba yer. Ai paa aran una cart tcempo- La sooras de Fondon. En primer tdrmino. Otilla Castro. T ,2 no. Otilia Beoto vioda de lranco. Gea e i efdan urae dIsalogudos Sa e cubre de luin la Cronies qu Isa lies a a tumba OIedes a uest ,sigoddad svHabanera pare dar cuenta de Era oU alma sencilla iv buena re adan tabin uesrquisieas r otra oa la muy dol, rosa generosa, que dea de. Escoa uno deItntoe modelos Aentoa- goza gratos reeterdos. Maria An-I Luca beaos la rela W eiss. Francisco y' qua d Cheauviu. Lucia Fer- trajo hae tmoy poco Ia dolencia Para su alma una oracidn v a ojoreo brrel y -fa en p Ls Arh"rcu naindr de Castro. Siuen Ins felleita ion na oramable propelaria la Sra. Geor- perfumes. Lucrte Larrea. Tnbheii ha' atilivi p. Lucia Ara. Es hija del senor Manuel Leo. Zaldo y Llanso. Dsignadons bha sido padios ,tificaran per la no'ia, los sen- sa Ferrae en y bel se ora Isabet Waly Basulto y Sala a Pr. Lucia Sodcco do Agoamante. Llanso do Leom Bellot s dol es. Wal-yBato y sanaia. Lucia SOcurez de Agramonte. Miguela Msndessenmladeyuna i 'l. MOs Ie- iaIocs doctor Carl. Luua ArAmonte SuArez. Antonio ue. Prio Socdrra-. Jalme Cots. MantP grotios, Maria Antnna Rodri- posa. O stra con obrus quo sigue brindando I Iei Estela de h, Campa. Gis Ia Son- a y Espinosa. Confortada con los Santos Au. El sepelio se efectu6 ayer pnr oa tarde y constitul6 usna sentclda manifestacion de pesar. Alberto v Juan iGuttirrez de la Solana v Pdirz xlas casas amuebladas on exhibici6n.. Paza isuresits. Freddy Goudie. In;a J1r-. I lebiada a las once v media de la ge Silva. Pedro Pablo Pu,. Ing Juan Mariano Mora. Boda de alto rango social. Luis Pizarro, d' or i id uv esosa. SFrancisco R. Ins sen -o g"-b' s I ev6 a cahn ante familiares v, uOrstes Esten6z. Jons F- N: amist des muy altlcadas. Adolfo Albaisa. Joaquin Binsca. Alberto Fernandez Q Jnse Benito v Luis i tlbuyr tin acirertn ma de Pour- los nuevos es. Desde el onrtirn hasta el fores- a Mexicn. De blusa ajustada. Avalnribase el cnnjunin ode-' mas con aretes v brnche s e brij- llantes tambion de su familiar. Suscribiernn el acta. Inc M,- no Pedrosa. Guillermo Villalba. La boda, Garcerfin. Entre las amistadeg de In, cnn. Sancd i SMo riu.. Debido a su gran 6xito, repetimos nuestro anterior venta de modolos que son copies exoctas de vestido omer'canos que le costorian much m6s. Srr' models de ma de Ca doo nd'd l-4t. Santa Cara, Sonc. Piiamo, Tafrfs S. Tallta S M L. ChrdoisesVagaoo Sagui o IaGewade. Urbi et Orbi El Cong. Cat6lico Colombiano De la fi.. I ti4 lfr ein. Vida rural. NC Pero ms clu. Imblano de Vid Rural subrayt nuevas tierrat. Is necesidad de una reform ta las Inmensas oorciones del e- I g es y afilhadiqoo siOL e ns lot vastas regions africanas. Se afit qua Una politics di i. An tral" Stan, u eateler q6e1 4e 1e- SNumero cass omerciales exhiben en ]as pteenles hincapie en el evidencee d evelan Is deficiente explotacdcn ides. FIgura i la te. Misa solemne en la Ermita de Montserrat, Ante esta situaci6n de latifun- 'ra obtener un met o rendi- espoa del secretario de honor, Je a Dia Diat; Antomna Vade,. Filix Alluntia O. Jesus Vega Rodrigut. Fote Bauian. Lavin Soleanor har e antre. Los viernes de trbenoc pun rillo de Ena udAe. Sociales a n Miramar. Los vierne s tra laj ha de facilitar e la ai cunto i. Carva al Veras -ia de i ota a dfio e dc tir que Pgando s a o tt d e p t"o bisic del program i la uv. Cat61ica Cuban ha grabs- la Pjrroqua de Monserrate. Esta Coral, e-rtuar la Reserva del Santi realzare today clase de cultivo s aquillon que deberan lr i nor Jose Busamante Rod- oria son trabajadore, qu lab InsuAtuci6n musical que Ie- imo con el E. DEI irtn dade. D g uleJad. Jose gose M C.. Eltruch Ca EL S. Oa ACntoni. Coua s social. Ave d Prlmeraslc y Beltn"s dq La I cuerdan aistir a Ead ouard. Mania Minie. C ae ona del s F tra o illanuesa. G jln Morales. IVaias More soc ia B d r ndr 21M. Manue Alae Fe. Gal ia sen Jose ic nmins Curroas Fe. Jast Enoe Ioru. R Vnel t '. Pa a] inv en todas d ls l ases del erI. M ,p n Alh.. Manuel P reo Grafts, M -. Ivud de Catasus: Oailia Pern n r. M or dqinc aanc s ddn MasaR Cre a nias. C aTa d. Juan Coe Aba- driguez. Ig nal MartI ez MartlG nz. Oilia te las re de Jesus"n a la unas ie r deIarn ds lino t del mi r. Cues'a Igiesas. Lc ea Ba dsai es. Gulerrez Paula. A Aladr G ri. Man uencl ce l cu a ie spoa i ca hrgo n st e acn 'o acl e a la e l" on n iscq o LHbana ene adoradel mon el e s1 I aartMeue a quez alros e nires Aamr "rd re o P-, Festividad d-el lunes sido 1I mstma pues al cu- u a m vis. El peso, en kilogramos, fue evaluado en balanza digital con la participante descalza, con el mínimo de ropa y sin accesorios. Se tuvo como objetivo proporcionar nuevas orientaciones, reforzar contenidos correctos, revisar informaciones equivocadas, motivar la continuidad del tratamiento y aclarar dudas sobre el sobrepeso y las medias de control. También se incluyeron orientaciones sobre la hidratación adecuada y el riesgo de dietas y productos para perder peso sin indicación y supervisión de un profesional de la salud. Se permitió que los contenidos específicos relacionados por las mujeres fueran abordados, así como la expresión de dudas y comentarios. Debería haber flexibilidad en la secuencia de exposición de los contenidos si se percibía esa necesidad y se observó la comprensión de los contenidos enfocados pidiendo a las mujeres que informaran sobre la comprensión de los temas abordados. Para analizar las diferencias del peso intragrupo se utilizó el test t pareado, después de la evaluación de la normalidad de los datos por el test de Shapiro-Wilk. No hubo diferencia estadísticamente significativa entre los grupos GC y CC , haciendo la muestra homogénea. Salvador, BA, Brasil, En lo que se refiere a los datos antropométricos, los grupos control e intervención fueron homogéneos. La mediana fue de 90,7 Kg. En cuanto a la circunferencia de la cintura, en la comparación intragrupos, antes y después de la intervención, no se observaron alteraciones estadísticamente significativas. En la tabla 4, se presentan los resultados de la comparación intergrupos después de la intervención. Este ensayo controlado aleatorizado evaluó el efecto del monitoreo remoto de enfermería de mujeres con sobrepeso constatando beneficios en la mejora de las medidas antropométricas y ofrece evidencias para la utilización de esta herramienta terapéutica en el cuidado en salud y enfermería. Las condiciones de desigualdad social exigen enfoques sensibles del equipo de salud, en el sentido de comprender las dificultades de cada persona y adecuar las orientaciones a las mismas. Sin embargo, la mayoría realizaba el trabajo doméstico, confiriendo a ellas el nivel de actividad física activo o muy activo en el domicilio. Este panorama es preocupante, pues la actividad física regular por lo menos minutos por semana es uno de los pilares del tratamiento para reducción del peso El porcentaje de mujeres con obesidad fue superior al de sobrepeso y todas estaban con la circunferencia de la cintura aumentada representando un grupo poblacional con alto riesgo de morbimortalidad. Los datos del presente estudio mostraron que el monitoreo remoto de enfermería fue efectivo una vez que las medidas antropométricas de las mujeres del grupo intervención presentaron reducción con significancia estadística en comparación con el grupo control. Sin embargo, se destaca que el uso de estas tecnologías también logró resultados favorables en la pérdida de peso Se identificó sólo un estudio de intervención educativa que empleó encuentros presenciales y la tecnología del telemonitoreo. Escorts masculinos en Costa Rica. Encuentra hombres guapos en Costa Rica para disfrutar de un encuentro casual en tu ciudad. Clasificados de chico busca chico, escort gay y parejas gays que se anuncian en Skokka de forma totalmente gratuita. Hombres con pollones preparados para satisfacer todas las fantasías de hombres y mujeres. Genial la web! Cuanto os costó el tour por el desierto por persona? Y el albergue? Consejos para viajar por Marruecos. Parte III. Consejos para Viajar por Marruecos. 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Depilacion rasurado masajes y mas. Mpga and Mpgv strongly correlate with the moment magnitude of the event, provided sufficient records for each event are available. The results show that Mpgv has a smaller standard deviation in comparison to Mpga when compared with the estimated magnitudes and provides a more accurate early assessment of earthquake magnitude. We test this new method to estimate the magnitude of the Tohoku earthquake and we present the results of this estimation. PGA and PGV from borehole recordings allow us to estimate the magnitude of this event s and s after the earthquake onset, respectively. We demonstrate that the incorporation of borehole strong ground-motion records immediately available after the occurrence of large earthquakes significantly increases the accuracy of earthquake magnitude estimation and the associated improvement in earthquake and tsunami early warning systems performance. Moment magnitude versus predicted magnitude Mpga and Mpgv. Numerous studies have tried to identify the core deficit of developmental dyscalculia DD , mainly by assessing a possible deficit of the mental representation of numerical magnitude. Research in healthy adults has shown that numerosity, duration, and space share a partly common system of magnitude processing and representation. However, in DD, numerosity processing has until now received much more attention than the processing of other non-numerical magnitudes. To assess whether or not the processing of non-numerical magnitudes is impaired in DD, the performance of 15 adults with DD and 15 control participants was compared in four categorization tasks using numerosities, lengths, durations, and faces as non- magnitude -based control stimuli. Results showed that adults with DD were impaired in processing numerosity and duration, while their performance in length and face categorization did not differ from controls' performance. Our findings support the idea of a nonsymbolic magnitude deficit in DD, affecting numerosity and duration processing but not length processing. Consideration of reinforcer magnitude may be important for maximizing the efficacy of treatment for problem behavior. Nonetheless, relatively little is known about children's preferences for different magnitudes of social reinforcement or the extent to which preference is related to differences in reinforcer efficacy. The purpose of the current study was to evaluate the relations among reinforcer magnitude , preference, and efficacy by drawing on the procedures and results of basic experimenta Integration and magnitude homogenization of the Egyptian earthquake catalogue. Hussein, H. The aim of the present work is to compile and update a catalogue of the instrumentally recorded earthquakes in Egypt, with uniform and homogeneous source parameters as required for the analysis of seismicity and seismic hazard assessment. This in turn requires a detailed analysis and comparison of the properties of different available sources, including the distribution of events with time, the magnitude completeness and the scaling relations between different kinds of magnitude reported by different agencies. The observational data cover the time interval and an area between The linear regressions between various magnitude types have been evaluated for different magnitude ranges. Using the best linear relationship determined for each available pair of magnitudes , as well as those identified between the magnitudes and the seismic moment, we convert the different magnitude types into moment magnitudes M W , through a multi-step conversion process. Analysis of the catalogue completeness, based on the MW thus estimated, allows us to identify two different time intervals with homogeneous properties. De esta manera los límites este y oeste quedaron establecidos por la confluencia de los ríos antes mencionados y la localidad de Bajada del Agrio, respectivamente. We illustrate two essential consequences of the systematic difference between moment magnitude and local magnitude for small earthquakes, illuminating the underlying earthquake physics. However, the relationship between local magnitude ML and moment is itself magnitude dependent. Just as importantly, if this relation is overlooked, prediction of large- magnitude ground motion from small earthquakes will be misguided. We also consider the effect of this magnitude scale difference on b-value. The oft-cited b-value of 1 should hold for small magnitudes , given M. This is of particular import when estimating the rate of large earthquakes when one has limited data on their recurrence, as is the case for induced earthquakes in the central US. The integrated theory of numerical development posits that a central theme of numerical development from infancy to adulthood is progressive broadening of the types and ranges of numbers whose magnitudes are accurately represented. The process includes four overlapping trends: 1 representing increasingly precisely the magnitudes of non-symbolic…. We investigated the relation between children's numerical- magnitude representations and their memory for numbers. Results of three experiments indicated that the more linear children's magnitude representations were, the more closely their memory of the numbers approximated the numbers presented. This relation was present for preschoolers and…. Non extensivity and frequency magnitude distribution of earthquakes. Starting from first principles in this case a non-extensive formulation of the maximum entropy principle and a phenomenological approach, an explicit formula for the magnitude distribution of earthquakes is derived, which describes earthquakes in the whole range of magnitudes. The Gutenberg-Richter law appears as a particular case of the obtained formula. Comparison with geophysical data gives a very good agreement. Trosclair-Lasserre, Nicole M. The purpose of the current…. The link between number and space has been discussed in the literature for some time, resulting in the theory that number, space and time might be part of a generalized magnitude system. To date, several behavioral and neuroimaging findings support the notion of a generalized magnitude system, although contradictory results showing a partial overlap or separate magnitude systems are also found. The possible existence of a generalized magnitude processing area leads to the question how individuals with developmental dyscalculia DD , known for deficits in numerical-arithmetical abilities, process magnitudes. By means of neuropsychological tests and functional magnetic resonance imaging fMRI we aimed to examine the relationship between number and space in typical and atypical development. Participants were 16 adolescents with DD In the fMRI paradigm participants had to perform discrete arrays of dots and continuous magnitude angles comparisons as well as a mental rotation task. In the neuropsychological tests, adolescents with dyscalculia performed significantly worse in numerical and complex visuo-spatial tasks. However, they showed similar results to TD peers when making discrete and continuous magnitude decisions during the neuropsychological tests and the fMRI paradigm. A conjunction analysis of the fMRI data revealed commonly activated higher order visual inferior and middle occipital gyrus and parietal inferior and superior parietal lobe magnitude areas for the discrete and continuous magnitude tasks. Moreover, no differences were found when contrasting both magnitude processing conditions, favoring the possibility of a generalized magnitude system. Group comparisons further revealed that dyscalculic subjects showed increased activation in domain general regions, whilst TD peers activate domain specific areas to a greater extent. In conclusion, our results point to the existence of a. The magnitude of an earthquake is one of its basic parameters and is a measure of its scale. It plays a significant role in seismology and earthquake engineering research, particularly in the calculations of the seismic rate and b value in earthquake prediction and seismic hazard analysis. However, several current types of magnitudes used in seismology research, such as local magnitude ML , surface wave magnitude MS , and body-wave magnitude MB , have a common limitation, which is the magnitude saturation phenomenon. Fortunately, the problem of magnitude saturation was solved by a formula for calculating the seismic moment magnitude MW based on the seismic moment, which describes the seismic source strength. Now the moment magnitude is very commonly used in seismology research. However, in China, the earthquake scale is primarily based on local and surface-wave magnitudes. In the present work, we studied the empirical relationships between moment magnitude MW and local magnitude ML as well as surface wave magnitude MS in the Chinese Mainland. Therefore, in China, if the moment magnitude of an earthquake is not reported by any agency in the world, we can use the equations mentioned above for converting ML to MW and MS to MW. These relationships are very important, because they will allow the China earthquake catalogs to be used more effectively for seismic hazard analysis, earthquake prediction, and other seismology research. We also computed the relationships of and where Mo is the seismic moment by linear regression using the Global Centroid Moment Tensor. The goal of tsunami forecast, as a system for predicting potential impact of a tsunami at coastlines, requires quick estimate of a tsunami magnitude. This goal has been recognized since the beginning of tsunami research. The work of Kajiura, Soloviev, Abe, Murty, and many others discussed several scales for tsunami magnitude based on estimates of tsunami energy. However, difficulties of estimating tsunami energy based on available tsunami measurements at coastal sea-level stations has carried significant uncertainties and has been virtually impossible in real time, before tsunami impacts coastlines. The slow process of tsunami magnitude estimates, including collection of vast amount of available coastal sea-level data from affected coastlines, made it impractical to use any tsunami magnitude scales in tsunami warning operations. Uncertainties of estimates made tsunami magnitudes difficult to use as universal scale for tsunami analysis. Historically, the earthquake magnitude has been used as a proxy of tsunami impact estimates, since real-time seismic data is available of real-time processing and ample amount of seismic data is available for an elaborate post event analysis. This measure of tsunami impact carries significant uncertainties in quantitative tsunami impact estimates, since the relation between the earthquake and generated tsunami energy varies from case to case. In this work, we argue that current tsunami measurement capabilities and real-time modeling tools allow for establishing robust tsunami magnitude that will be useful for tsunami warning as a quick estimate for tsunami impact and for post-event analysis as a universal scale for tsunamis inter-comparison. We present a method for estimating the tsunami magnitude based on tsunami energy and present application of the magnitude analysis for several historical events for inter-comparison with existing methods. New moment magnitude scale, evidence of stress drop magnitude scaling and stochastic ground motion model for the French West Indies. S-waves Fourier spectra are analysed to simultaneously determine source, path and site terms. The results show that the duration magnitude routinely estimated for the events that occurred in the region underestimate moment magnitude by 0. From the inverted seismic moments and corner frequencies, we compute Brune's stress drops. We show that stress drops increase with increasing magnitude. The same pattern is observed on apparent stresses i. However, the rate of increase diminishes at high magnitudes , which is consistent with a constant stress drop model for large events. Using the results of the inversions, we perform ground motion simulations for the entire data set using the SMSIM stochastic simulation tool. Although the magnitude -dependent stress drop model is giving better results than the constant stress drop model, the interevent variability remains high, which could suggest that stress drop depends on other parameters such as the depth of the hypocentre. In any case, the overall variability is of the same order of magnitude as usually observed in empirical ground motion prediction equations. This event is larger than previous one in terms of magnitude and showed that measured magnitude strongly depends on the frequency band of data. Relative spectral magnitude varies with frequencies and decreases as frequency increase. A methodology is presented for determining mb Pn magnitude of underground nuclear explosions from local Pn phase. The mb Pn estimates of regional events for Korean Peninsula are determined to be mb Pn? Systematic non-linearity does not observed at frequency band from 0. The magnitude of 6th event is mb Pn 6. Further research of applicable mb Pn magnitude scaling is required for all frequency band and. The bolometric, infrared and visual absolute magnitudes of Mira variables. Statistical parallaxes, as well as stars with individually known distances are used to derive bolometric and infrared absolute magnitudes of Mira Me variables. The derived bolometric magnitudes are in the mean about 0. The problem of determining the pulsation constant is discussed. Miras with periods greater than days probably pulsate in the first overtone. Those of shorter periods are anomalous and may be fundamental pulsators. It is shown that the absolute visual magnitudes at mean light of Miras with individually determined distances are consistent with values derived by Clayton and Feast from statistical parallaxes. Potencial del Agua del suelo. Full Text Available La energía potencial del agua presenta diferencias de un punto del suelo a otro; esas diferencias son las que originan el movimiento del agua de acuerdo a la tendencia universal de la materia en el sentido de moverse de donde la energía potencial es mayor a donde dicha energía es menor. En el suelo el agua en consecuencia se mueve hacia donde su energía decrece hasta lograr su estado de equilibrio. Se desprende entonces que la cantidad de energía potencial absoluta contenida en el agua, no es importante por sí misma, sino por su relación con la energía en diferentes lugares dentro del suelo. El concepto Potencial de agua del suelo es un criterio para esta energía. On the magnitude and recurence of Vrancea earthquakes. The moment- magnitude scale Msub W is proposed for the quantification of Vrancea earthquakes. The asperity model is found adequate to explain the observed quasi-cycles and super-cycles in the occurrence of large events. Disparities in the Magnitude of Human Immunodeficiency Virus HICs while tuberculosis, candidiasis, chronic diarrhea, and cryptococcosis were predominant Mohar A. Magnitude and factors associated with post-cesarean surgical site Magnitude and factors associated with post-cesarean surgical site infection at Hawassa University Teaching and referral hospital, southern Ethiopia: a Thus, it should be averted by implementing infection prevention techniques. Rapid earthquake magnitude determination for Vrancea early warning system. Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude from the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in order to avoid false alarms. A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into account that it is computed from only 3 stations in a very short time interval. Impact of magnitude uncertainties on seismic catalogue properties. Catalogue-based studies are of central importance in seismological research, to investigate the temporal, spatial and size distribution of earthquakes in specified study areas. Methods for estimating the fundamental catalogue parameters like the Gutenberg-Richter G-R b-value and the completeness magnitude Mc are well established and routinely applied. However, the magnitudes reported in seismicity catalogues contain measurement uncertainties which may significantly distort the estimation of the derived parameters. In this study, we use numerical simulations of synthetic data sets to assess the reliability of different methods for determining b-value and Mc, assuming the G-R law validity. After contaminating the synthetic catalogues with Gaussian noise with selected standard deviations , the analysis is performed for numerous data sets of different sample size N. The noise introduced to the data generally leads to a systematic overestimation of magnitudes close to and above Mc. This fact causes an increase of the average number of events above Mc, which in turn leads to an apparent decrease of the b-value. This may result to a significant overestimation of seismicity rate even well above the actual completeness level. The b-value can in general be reliably estimated even for relatively small data sets N magnitudes higher than the actual completeness level are used. Nevertheless, a correction of the total number of events belonging in each magnitude class i. Because magnitude uncertainties here with the form of Gaussian noise are inevitable in all instrumental catalogues, this finding is fundamental for seismicity rate and seismic hazard assessment analyses. Also important is that for some data analyses significant bias cannot necessarily be avoided by choosing a high Mc value for analysis. In such cases, there may be a risk of severe miscalculation of. The static surface deformation can be recovered from strong motion records. Compared to satellite-based measurements such as GPS or InSAR, the advantage of strong motion records is that they have the potential to provide real-time coseismic static displacements. The use of these valuable data was optimized for the moment magnitude estimation. A centroid grid search method was introduced to calculate the moment magnitude by using1 model. The method to data sets was applied of the The magnitude of innovation and its evolution in social animals. Innovative behaviour in animals, ranging from invertebrates to humans, is increasingly recognized as an important topic for investigation by behavioural researchers. However, what constitutes an innovation remains controversial, and difficult to quantify. Drawing on a broad definition whereby any behaviour with a new component to it is an innovation, we propose a quantitative measure, which we call the magnitude of innovation , to describe the extent to which an innovative behaviour is novel. This allows us to distinguish between innovations that are a slight change to existing behaviours low magnitude , and innovations that are substantially different high magnitude. Using mathematical modelling and evolutionary computer simulations, we explored how aspects of social interaction, cognition and natural selection affect the frequency and magnitude of innovation. We show that high- magnitude innovations are likely to arise regularly even if the frequency of innovation is low, as long as this frequency is relatively constant, and that the selectivity of social learning and the existence of social rewards, such as prestige and royalties, are crucial for innovative behaviour to evolve. We suggest that consideration of the magnitude of innovation may prove a useful tool in the study of the evolution of cognition and of culture. Iranian earthquakes, a uniform catalog with moment magnitudes. A uniform earthquake catalog is an essential tool in any seismic hazard analysis. In this study, an earthquake catalog of Iran and adjacent areas was compiled, using international and national databanks. The following priorities were applied in selecting magnitude and earthquake location: a local catalogs were given higher priority for establishing the location of an earthquake and b global catalogs were preferred for determining earthquake magnitudes. In an effort to avoid the "boundary effect," since the newly compiled catalog will be mainly used for seismic hazard assessment, the study area includes the areas adjacent to Iran. The standardization of the catalog in terms of magnitude was achieved by the conversion of all types of magnitude into moment magnitude , M W, by using the orthogonal regression technique. In the newly compiled catalog, all aftershocks were detected, based on the procedure described by Gardner and Knopoff Bull Seismol Soc Am , The seismicity parameters were calculated for the six main tectonic seismic zones of Iran, i. Changes in the timing and magnitude of floods in Canada. It is expected that the global climate change will have significant impacts on the regime of hydrologic extremes. An increase in both the frequency and magnitude of hydrologic extremes is anticipated in the near future. Sin duda represen- nacional. En estos dos periods del president ta el tipo de president lider. Eisenhower no ha habido nada semejante a sla gualmente el gobernador Rockefeller, en luche que dej6 invilido al president Wilson, aI banda republicans, cumple la figure de di- que elimin6 de la vida piblica a president namisma y progress augurada par Hyman. Su Hoover, quc acab6 con la vida del president a;rancada y su triunfo en Is e lecciones de i Franklin D. Roosevelt o que provoco imprope- Nueva York han side portentoso. En este sentido los comentaristas han co- Poe parte de os dem6cretas. Si triun- hombres ima im ir un e propia fan Ioi republicans con el vicepresidente Ni- a Ia presidencia de la nacidn. El ataque seri implacable para ;m- ma elecci6n presidential es interesante destacar pedi. En case de ser elec- el Ar.. Pero la agresion se iniciari opor- mente mis poderoso candidate demdcrata, el tunamenite para evilar na reelecci6n. Por su part, el senador Ke- En cuantc a un presidentie dem6crata, con- nnedy pod. Los politicos pro- Sin embargo, los viejos bonzos de ambos fesionales de ambos partidos lo ven como un partidos sue6an con dos tickets ideals: Nixon- intelectual contemplative que pudiera resultar Rockefeller por los republicans: Stevenson-. Las elecciones pri- querido de dristica accidn. Por otra parte, hay marias escalonadas de aqui alas fechas de las araa unanimidad en estimar que el senador Ke- convenclones en julio de , deberin influir nnedy seria el menos combatido de los presi- decisivamente en el alineamiento de los presi- dentes democratas. Primero los politicos del denciaies. Es el Dia del Antigua Alum- no. Deide temprano todo seri bullicio y jiblilo en la casa. Ninguna satisfacci6n mayoi para los actuales profesores que re- cibir a los que un tiempo pasaron por las aulas dcl plantel y muchos de Ins cuate, lueron sus compafieros de studios. Y nin- guna satisfacci6n mayor para todos que abrazar a sus condiscipulos y recorder de pasada las jornadas escolares vividas en comon. Ia quietud de las salas de studio. Un sentimiento de nostalgia se disol- iern en el ambiente. Que nada conmue- ve mas hondamente que recorder los dias de ]a adolescencia y de la nifiez y asociar. Belin no es s6lo un centro de saber. Es un hogar de formaci6n. Par no los 'que pasaron por sus aulas se sienten perenne- mente vinculados al colegio. Y vuelven skemprt a el como el que acude al pase de list en forma voluntaria. Nada mis hermoso que la ahanza del ayer y del hoy, de la experiencia y del entusiasmo, para emprender el. Esto es In que simboliza el Dia del Antigue Alumno. Un titulo que Unicamente no conquistan los que no perseveran. Un titular que honra cuando el punto de refe- rencia es Belen. Muchos anfermo Ms quajan de qua cuands acuden a I botica to demuanda d ciertos medicamentos que lea son indispen- sables parn conservar La salud aliviarsn de sum dolencias, el boticario Io itico que leis brinda Ison eicusaUs. ZO s usanto depends del Ministerio d, Co- - mercie7 Quienquiera que sea, debs tomar car. Per io mnese mientras el INRA no asuma I responsabilidad de fabricar an Cuba todas las vitamins, hor- moans y antibi6ticos y pildoras tranquiliza- doras que a s ecesitas e el mundo actual pain sobrevivir. El nuestro alude a "pueblos". El nor teamericano alude, tal vez, a "gobiernos". En cuyo caso habria que Ilegar a! Eso no eas nueo. Aqui s has exhibi. Como que algunos de los espectadores, en algunas ecenas, teulan qua taparse las narices. C ella nos trai ira el Ave-M la csperanrza aa. La ebt velas al vien anunclacion. Jose bra. Un peda Tan pequefi fiuelo lindo una guajip;ta Tan grande brir a Dios. Salrededores bra. Y no I el sol que tambien a M Una mata pequefilta cc al ver a Mar eho su peeh brazos en es mano, los m Sdibujaron a la Virgen tu cha sombra sonreir. Poroue Ventuia G a i ta Calderon rue. De Vcntuia me decta una vez Gabriela Mistral que ta tuno de los dos proisisa- hic- panoamenricanos el otro. Gomez Carrillo. Es decir. OS hechos recientes des- defando el paternalismm" de exportable e hunden cada uerias qu no prmanc, births an Expertos economists de una univer- n cas popular cas D tacan a. El importarse; [a inflaci6n, en Esta media nos parece may jusr-, xima generaci6n de los Estados Unidos pe- el ieruano de un modo suel- es el via e de Khrushchev a gobierno de Varsovia es vic- suma, se acentia. Los tra. Pere debe smr complementada con otra qua diri. Gomez ontar tiempo, va[ga Ia aclaracion- que impone Moscil-lo que. Y Ra do alaboraci6o axtranjera qua me Ahora faftadaber si se o darin. En nos hechos concretes nos to ci. De alguna manera-pa- iila. Campo de intervention Del C6digo Social de nal, expression de la organi- cmen uan dechado d ele-ic zacinpre nal, e per- n dachado de eli- lante subrayindose el resul- el desconocimiento de los en cambio. Lo Segundo ha per- Gomulka ha temido que caudal de mercaderia. Al volver al poder Este castigo es igualmen- duraci6n del trabajo diarno nimato se cometen los mias del Modernismo y acendrada en los iltimos mess. Pero se vi6 obligado a eevar lons te el que determine las dimi- la prohibition del trabajo graves abuses en perjuicio de Naclonalzacion de empress par largos aos de residencia lo primero, que podriamos tornales de nls trabajadores siones de personajes, do nocturne, el descanso domi- los socios o del pfiblico. Im- Razones particulars pue- enParis. Ocurria asi que llmar el castigo a Is "rev- de 1. Pero en corporaci6n de Gomulka. Esti en su derecho ai Proteeci6n contra la concn- econdmica. Debe pro. Pier en el fond. Esto, de otro lado, ha hay una ofensiva de casai- AI e loartieontdprine- pregitimamente,ya para pro- eagenti6ninete.. Debe re- dado alas a loa parlarios go" dirigida ot In. En todos eto c ason la AI igual que sus hermanos. La con- Parsego oblevitar pare los tra hibitivos , mpena ayudarl o- inici l ev onsvi ciso el pintor Jose mueFran- men itere polaco un cambio planificada. Los campesinos. Un large y-aimire- actual. Icu l asc to la. Lettres Francalses, si no re- cuerdo mal, desvel6 --con- Ia autoridad de buen juez sue a su author se e reco- nocia- las razones de aeuel Valard6n. Hasta entonces, abriela habia sido. Sabre nuestro patricio ha- bia escrito. Pe r o much mas. Sassone era otra cosa. Llego alia hlce mucoos arios, no se si ya con am7paro de di- plomatico menor. Como Ventura. Cultivo versos v diversiones. Escribl6 come- dias. Caso con la actnz Maria Palou y dirigio su compalfia. Gustaba de decir que se sentia espahel en el Peru y peruano en Espafia. 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El sol de me- Congas, rumbas. Comor para u- La vaca y la multl. Y [aria se palpa la bendita realidad pequehita. Incon- nso un rosal Y rebiblemente humana. Paz ria sofocada. Esta ira- sfuerzo sobrehu- se que Bernanos aeerte a po- iisculos tensos se ner en la boca moribunda de flor de piel' v su cure de Campagne, cae uvo sombra Mu- sobre las almas abiertas. En paza descansar y esta nocheblanca. Sociedad El fin de af4o en los clubs. Ia que en cads ry Vallhonrat y Pando, una club, tendri exceptional bri- aeiorita atractivisima. Prime- jnven Raoe1l Rodriguez Ca- ranente nos ieferiremosa a barrocas. Tulane, en Nueva Orleans. Este compromise se forma- Se desarrollara en la espa. En el Habana novia. Felici- la noche a cuatro de la ma- dades. Se' serviri un ex- quisito mend y se bailara con dos orquestas de primer orden debiendo asistir las seforas de traje corto y los caballeros de traje corriente. Grandiosa bajo todos sus as- pectos sera la fiesta del Ha- vana Biltmore Yacht and Country Club donde su di- rectiva viene hacienda puLl- tiple preparatives. Para la mejor organizacion del event se ruega iacar las reservacio- nes con Ia debida anticipa- tion. El ador- no estara a cargo del cono- i crdo decorador Cajaravilla y se extender. A medianoche -ie seavira una magnifica ce- na y el baile reinara dese l piimera hora con las orques- tas Kubavana v Sensaci6n '' debiendo asistir los caballe- ru- de eltoueta. El domingo diecisiete del enti ante mes de enero. Beatriz Solis e Hidal- ' go Gato, con e' joven Agus-. En la clinic del reparto Miramar ha da- do a luz una linda nifa Isa sefiora Margarita Gonmez t Diago. De acuerdo con la rostumbre los padres del novio. Muchos iexlos le deseasmos a tan important cargo. Ir fue rfrecido un animado "party" de tespedida al asiitnm ico t. ManIolo Mario Mori. Juan Manuel Tapia. Miguel Angel Pantagua. Hector Ro- driguez y Armando Codina. Curios G. En esos dias memor. Mendoza se complace en ofrecer una series de atractivos pars todos los gustos r oars to- dos loe olsitillos. El dia de Navidad estrenardn estos lindos models de FAYA Todo en illos es primoroso: los colors, los detalles, los bordados DiseAidos, confeccionados y adornados en nuestros propios talleres, constituven verdaderas creaciones. Son los tstidos de fiesta que used preferird para iodas sus nineas. Trdigalas a sriros. Jiias: Termr piew. D di Ialia Tamom fasn nw l a roes DJl 34 at Salomon Stenz n. Trtde el pas o dl fecmiento ee- a o y de rept e Yok or cdotraba yer. Ai paa aran una cart tcempo- La sooras de Fondon. En primer tdrmino. Otilla Castro. T ,2 no. Otilia Beoto vioda de lranco. Gea e i efdan urae dIsalogudos Sa e cubre de luin la Cronies qu Isa lies a a tumba OIedes a uest ,sigoddad svHabanera pare dar cuenta de Era oU alma sencilla iv buena re adan tabin uesrquisieas r otra oa la muy dol, rosa generosa, que dea de. Escoa uno deItntoe modelos Aentoa- goza gratos reeterdos. Maria An-I Luca beaos la rela W eiss. Francisco y' qua d Cheauviu. Lucia Fer- trajo hae tmoy poco Ia dolencia Para su alma una oracidn v a ojoreo brrel y -fa en p Ls Arh"rcu naindr de Castro. Siuen Ins felleita ion na oramable propelaria la Sra. Geor- perfumes. Lucrte Larrea. Tnbheii ha' atilivi p. Lucia Ara. Es hija del senor Manuel Leo. Zaldo y Llanso. Dsignadons bha sido padios ,tificaran per la no'ia, los sen- sa Ferrae en y bel se ora Isabet Waly Basulto y Sala a Pr. Lucia Sodcco do Agoamante. Llanso do Leom Bellot s dol es. Wal-yBato y sanaia. Lucia SOcurez de Agramonte. Miguela Msndessenmladeyuna i 'l. MOs Ie- iaIocs doctor Carl. Luua ArAmonte SuArez. Antonio ue. Prio Socdrra-. Jalme Cots. MantP grotios, Maria Antnna Rodri- posa. O stra con obrus quo sigue brindando I Iei Estela de h, Campa. Gis Ia Son- a y Espinosa. Confortada con los Santos Au. El sepelio se efectu6 ayer pnr oa tarde y constitul6 usna sentclda manifestacion de pesar. Alberto v Juan iGuttirrez de la Solana v Pdirz xlas casas amuebladas on exhibici6n.. Paza isuresits. Freddy Goudie. In;a J1r-. I lebiada a las once v media de la ge Silva. Pedro Pablo Pu,. Ing Juan Mariano Mora. Boda de alto rango social. Luis Pizarro, d' or i id uv esosa. SFrancisco R. Ins sen -o g"-b' s I ev6 a cahn ante familiares v, uOrstes Esten6z. Jons F- N: amist des muy altlcadas. Adolfo Albaisa. Joaquin Binsca. Alberto Fernandez Q Jnse Benito v Luis i tlbuyr tin acirertn ma de Pour- los nuevos es. Desde el onrtirn hasta el fores- a Mexicn. Vitaliy Vorobyov. Ver todos los créditos IMDb. Rusia Ucrania. Guerra , Acción , Drama , Romance..

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Bbw pornt 6 minWTF Wild oral stimulation with hot beauty. Sexdate utrecht. A parte de típicos puestos de todos los colores, fuimos a ver el mercado de animales domésticos y parking de burros! El hit de nuestra visita fue encargar la pizza bereber leímos sobre esta pizza en una de las guías. Para pedirla, hay un cierto ritual que hay que seguir: hay que comprar la carne que quieras al carnicero, y el se encarga de mandar a un niño al de la verdura y luego a la paderia y traerla de vuelta al carnicero en unos 40 min. Pagamos 10o Dhs entre 6, pero era tan grande que nos costó acabarla!!! Sobre las Bueno, si no os da cosa dormir en la cama donde duermen todos, ni hace falta el saco. Hola, dromedario! Depende del dromedario y de donde esté en fila… si es un adulto y va primero, no pasa nada, pero si te toca, como a mí, un jovencito al final de la fila, … es divertido!!! El campamento, por lo visto, es de varias empresas. Child prostitution: magnitude and related problems. In Ethiopia, very little is known about prostitution in general and about child prostitution in particular. The objective of this study was to determine the magnitude of child prostitution and to identify problems associated with it. A cross-sectional study design was utilized. Data were collected using structured questionnaire. A total of commercial sex workers were interviewed. Eighty eight At the time of joining prostitution Poverty, disagreement with family, and peer influence were the major reasons leading to prostitution. Strategies need to be developed to rescue child prostitutes from on-job violence, and to establish a rehabilitation program for those interested to discontinue prostitution along with efforts to minimize entry into prostitution. Full Text Available The prevalence of blindness among children in different regions varies from 0. This means that there are an estimated 1. Children who are blind have to overcome a lifetime of emotional, social and economic difficulties which affect the child, the family and society. The numbers blind with cataract do not reflect the years of disability and lost quality of life. Childhood blindness is second only to adult cataract as a cause of blind-person years. Timely recognition and intervention can eliminate blind-years due to childhood cataract, as the condition is treatable. How fault geometry controls earthquake magnitude. Recent large megathrust earthquakes, such as the Mw9. The first event occurred in a relatively low-convergence-rate subduction zone where events of its size were unexpected. The second event involved 60 m of shallow slip in a region thought to be aseismicaly creeping and hence incapable of hosting very large magnitude earthquakes. These earthquakes highlight gaps in our understanding of mega-earthquake rupture processes and the factors controlling their global distribution. Here we show that gradients in dip angle exert a primary control on mega-earthquake occurrence. We calculate the curvature along the major subduction zones of the world and show that past mega-earthquakes occurred on flat low-curvature interfaces. A simplified analytic model demonstrates that shear strength heterogeneity increases with curvature. Stress loading on flat megathrusts is more homogeneous and hence more likely to be released simultaneously over large areas than on highly-curved faults. Therefore, the absence of asperities on large faults might counter-intuitively be a source of higher hazard. Dessokey, M. The measurements, derived by the simulated Wood Anderson seismograms, are analysed and discussed. Historical revision of the exposure magnitude and the dosimetric magnitudes used in radiological protection. The moment magnitude M w and the energy magnitude M e: common roots and differences. Starting from the classical empirical magnitude -energy relationships, in this article, the derivation of the modern scales for moment magnitude M w and energy magnitude M e is outlined and critically discussed. The formulas for M w and M e calculation are presented in a way that reveals, besides the contributions of the physically defined measurement parameters seismic moment M 0 and radiated seismic energy E S, the role of the constants in the classical Gutenberg-Richter magnitude -energy relationship. This relationship directly links M e with M w via their common scaling to classical magnitudes and, at the same time, highlights the reason why M w and M e can significantly differ. As a result, for the same earthquake, M e may sometimes differ by more than one magnitude unit from M w. Such a difference is highly relevant when assessing the actual damage potential associated with a given earthquake, because it expresses rather different static and dynamic source properties. While M w is most appropriate for estimating the earthquake size i. Therefore, whenever possible, these two magnitudes should be both independently determined and jointly considered. Usually, only M w is taken as a unified magnitude in many. Automatic computation of moment magnitudes for small earthquakes and the scaling of local to moment magnitude. Moment magnitudes MW are computed for small and moderate earthquakes using a spectral fitting method. A combined bootstrap and orthogonal L1 minimization is then used to produce a scaling relation between ML and MW. The scaling relation has a polynomial form and is shown to reduce the dependence of the predicted MW residual on magnitude relative to an existing linear scaling relation. The scaling between ML and MW is explored using synthetic data computed with a stochastic simulation method. It is shown that the scaling relation can be explained by the interaction of attenuation, the stress-drop and the Wood-Anderson filter. For instance, it is shown that the stress-drop controls the saturation of the ML scale, with low-stress drops e. An attempt has been made to examine an empirical relationship between moment magnitude M W and local magnitude M L for the earthquakes in the northeast Indian region. Some earthquakes that were recorded during are used in this study. The M W- M L relationships in seven selected zones of the region are determined by linear regression analysis. A significant variation in the M W- M L relationship and its zone specific dependence are reported here. It is found that M W is equivalent to M L with an average uncertainty of about 0. A single relationship is, however, not adequate to scale the entire northeast Indian region because of heterogeneous geologic and geotectonic environments where earthquakes occur due to collisions, subduction and complex intra-plate tectonics. Temporal and spatial variations in the magnitude of completeness Temporal and spatial variations in the magnitude of completeness for homogenized moment magnitude catalogue for northeast India. Ranjit Das H R Orthogonal regression relations for conversion of body and surface wave magnitudes to w,HRVD based on events data for the period — have been derived. A combined bootstrap and orthogonal L1 minimization is then used to produce a scaling relation bet Magnitudes and frequencies of earthquakes in relation to seismic risk. Estimating the frequencies of occurrence of earthquakes of different magnitudes on a regional basis is an important task in estimating seismic risk at a construction site. Analysis of global earthquake data provides an insight into the magnitudes frequency relationship in a statistical manner. It turns out that, whereas a linear relationship between the logarithm of earthquake occurrence rates and the corresponding earthquake magnitudes fits well in the magnitude range between 5 and 7, a second degree polynomial in M, the earthquake magnitude provides a better description of the frequencies of earthquakes in a much wider range of magnitudes. It may be possible to adopt magnitude frequency relation for regions, for which adequate earthquake data are not available, to carry out seismic risk calculations. We present a simple and fast method for magnitude determination technique for earthquake and tsunami early warning systems based on strong ground motion prediction equations GMPEs in Japan. This method incorporates borehole strong motion records provided by the Kiban Kyoshin network KiK-net stations. We analyzed strong ground motion data from large magnitude earthquakes 5. Mpga and Mpgv strongly correlate with the moment magnitude of the event, provided sufficient records for each event are available. The results show that Mpgv has a smaller standard deviation in comparison to Mpga when compared with the estimated magnitudes and provides a more accurate early assessment of earthquake magnitude. We test this new method to estimate the magnitude of the Tohoku earthquake and we present the results of this estimation. PGA and PGV from borehole recordings allow us to estimate the magnitude of this event s and s after the earthquake onset, respectively. We demonstrate that the incorporation of borehole strong ground-motion records immediately available after the occurrence of large earthquakes significantly increases the accuracy of earthquake magnitude estimation and the associated improvement in earthquake and tsunami early warning systems performance. Moment magnitude versus predicted magnitude Mpga and Mpgv. Numerous studies have tried to identify the core deficit of developmental dyscalculia DD , mainly by assessing a possible deficit of the mental representation of numerical magnitude. Research in healthy adults has shown that numerosity, duration, and space share a partly common system of magnitude processing and representation. However, in DD, numerosity processing has until now received much more attention than the processing of other non-numerical magnitudes. To assess whether or not the processing of non-numerical magnitudes is impaired in DD, the performance of 15 adults with DD and 15 control participants was compared in four categorization tasks using numerosities, lengths, durations, and faces as non- magnitude -based control stimuli. Results showed that adults with DD were impaired in processing numerosity and duration, while their performance in length and face categorization did not differ from controls' performance. Our findings support the idea of a nonsymbolic magnitude deficit in DD, affecting numerosity and duration processing but not length processing. Consideration of reinforcer magnitude may be important for maximizing the efficacy of treatment for problem behavior. Nonetheless, relatively little is known about children's preferences for different magnitudes of social reinforcement or the extent to which preference is related to differences in reinforcer efficacy. The purpose of the current study was to evaluate the relations among reinforcer magnitude , preference, and efficacy by drawing on the procedures and results of basic experimenta Integration and magnitude homogenization of the Egyptian earthquake catalogue. Hussein, H. The aim of the present work is to compile and update a catalogue of the instrumentally recorded earthquakes in Egypt, with uniform and homogeneous source parameters as required for the analysis of seismicity and seismic hazard assessment. This in turn requires a detailed analysis and comparison of the properties of different available sources, including the distribution of events with time, the magnitude completeness and the scaling relations between different kinds of magnitude reported by different agencies. The observational data cover the time interval and an area between The linear regressions between various magnitude types have been evaluated for different magnitude ranges. Using the best linear relationship determined for each available pair of magnitudes , as well as those identified between the magnitudes and the seismic moment, we convert the different magnitude types into moment magnitudes M W , through a multi-step conversion process. Analysis of the catalogue completeness, based on the MW thus estimated, allows us to identify two different time intervals with homogeneous properties. De esta manera los límites este y oeste quedaron establecidos por la confluencia de los ríos antes mencionados y la localidad de Bajada del Agrio, respectivamente. We illustrate two essential consequences of the systematic difference between moment magnitude and local magnitude for small earthquakes, illuminating the underlying earthquake physics. However, the relationship between local magnitude ML and moment is itself magnitude dependent. Just as importantly, if this relation is overlooked, prediction of large- magnitude ground motion from small earthquakes will be misguided. We also consider the effect of this magnitude scale difference on b-value. The oft-cited b-value of 1 should hold for small magnitudes , given M. This is of particular import when estimating the rate of large earthquakes when one has limited data on their recurrence, as is the case for induced earthquakes in the central US. The integrated theory of numerical development posits that a central theme of numerical development from infancy to adulthood is progressive broadening of the types and ranges of numbers whose magnitudes are accurately represented. The process includes four overlapping trends: 1 representing increasingly precisely the magnitudes of non-symbolic…. We investigated the relation between children's numerical- magnitude representations and their memory for numbers. Results of three experiments indicated that the more linear children's magnitude representations were, the more closely their memory of the numbers approximated the numbers presented. This relation was present for preschoolers and…. Non extensivity and frequency magnitude distribution of earthquakes. Starting from first principles in this case a non-extensive formulation of the maximum entropy principle and a phenomenological approach, an explicit formula for the magnitude distribution of earthquakes is derived, which describes earthquakes in the whole range of magnitudes. The Gutenberg-Richter law appears as a particular case of the obtained formula. Comparison with geophysical data gives a very good agreement. Trosclair-Lasserre, Nicole M. The purpose of the current…. The link between number and space has been discussed in the literature for some time, resulting in the theory that number, space and time might be part of a generalized magnitude system. To date, several behavioral and neuroimaging findings support the notion of a generalized magnitude system, although contradictory results showing a partial overlap or separate magnitude systems are also found. The possible existence of a generalized magnitude processing area leads to the question how individuals with developmental dyscalculia DD , known for deficits in numerical-arithmetical abilities, process magnitudes. By means of neuropsychological tests and functional magnetic resonance imaging fMRI we aimed to examine the relationship between number and space in typical and atypical development. Participants were 16 adolescents with DD In the fMRI paradigm participants had to perform discrete arrays of dots and continuous magnitude angles comparisons as well as a mental rotation task. In the neuropsychological tests, adolescents with dyscalculia performed significantly worse in numerical and complex visuo-spatial tasks. However, they showed similar results to TD peers when making discrete and continuous magnitude decisions during the neuropsychological tests and the fMRI paradigm. A conjunction analysis of the fMRI data revealed commonly activated higher order visual inferior and middle occipital gyrus and parietal inferior and superior parietal lobe magnitude areas for the discrete and continuous magnitude tasks. Moreover, no differences were found when contrasting both magnitude processing conditions, favoring the possibility of a generalized magnitude system. Group comparisons further revealed that dyscalculic subjects showed increased activation in domain general regions, whilst TD peers activate domain specific areas to a greater extent. In conclusion, our results point to the existence of a. The magnitude of an earthquake is one of its basic parameters and is a measure of its scale. It plays a significant role in seismology and earthquake engineering research, particularly in the calculations of the seismic rate and b value in earthquake prediction and seismic hazard analysis. However, several current types of magnitudes used in seismology research, such as local magnitude ML , surface wave magnitude MS , and body-wave magnitude MB , have a common limitation, which is the magnitude saturation phenomenon. Fortunately, the problem of magnitude saturation was solved by a formula for calculating the seismic moment magnitude MW based on the seismic moment, which describes the seismic source strength. Now the moment magnitude is very commonly used in seismology research. However, in China, the earthquake scale is primarily based on local and surface-wave magnitudes. In the present work, we studied the empirical relationships between moment magnitude MW and local magnitude ML as well as surface wave magnitude MS in the Chinese Mainland. Therefore, in China, if the moment magnitude of an earthquake is not reported by any agency in the world, we can use the equations mentioned above for converting ML to MW and MS to MW. These relationships are very important, because they will allow the China earthquake catalogs to be used more effectively for seismic hazard analysis, earthquake prediction, and other seismology research. We also computed the relationships of and where Mo is the seismic moment by linear regression using the Global Centroid Moment Tensor. The goal of tsunami forecast, as a system for predicting potential impact of a tsunami at coastlines, requires quick estimate of a tsunami magnitude. Renuncio Aceptar. San José. Trans Y Travestis. Encuentros Casuales. Dsignadons bha sido padios ,tificaran per la no'ia, los sen- sa Ferrae en y bel se ora Isabet Waly Basulto y Sala a Pr. Lucia Sodcco do Agoamante. Llanso do Leom Bellot s dol es. Wal-yBato y sanaia. Lucia SOcurez de Agramonte. Miguela Msndessenmladeyuna i 'l. MOs Ie- iaIocs doctor Carl. Luua ArAmonte SuArez. Antonio ue. Prio Socdrra-. Jalme Cots. MantP grotios, Maria Antnna Rodri- posa. O stra con obrus quo sigue brindando I Iei Estela de h, Campa. Gis Ia Son- a y Espinosa. Confortada con los Santos Au. El sepelio se efectu6 ayer pnr oa tarde y constitul6 usna sentclda manifestacion de pesar. Alberto v Juan iGuttirrez de la Solana v Pdirz xlas casas amuebladas on exhibici6n.. Paza isuresits. Freddy Goudie. In;a J1r-. I lebiada a las once v media de la ge Silva. Pedro Pablo Pu,. Ing Juan Mariano Mora. Boda de alto rango social. Luis Pizarro, d' or i id uv esosa. SFrancisco R. Ins sen -o g"-b' s I ev6 a cahn ante familiares v, uOrstes Esten6z. Jons F- N: amist des muy altlcadas. Adolfo Albaisa. Joaquin Binsca. Alberto Fernandez Q Jnse Benito v Luis i tlbuyr tin acirertn ma de Pour- los nuevos es. Desde el onrtirn hasta el fores- a Mexicn. De blusa ajustada. Avalnribase el cnnjunin ode-' mas con aretes v brnche s e brij- llantes tambion de su familiar. Suscribiernn el acta. Inc M,- no Pedrosa. Guillermo Villalba. La boda, Garcerfin. Entre las amistadeg de In, cnn. Sancd i SMo riu.. Debido a su gran 6xito, repetimos nuestro anterior venta de modolos que son copies exoctas de vestido omer'canos que le costorian much m6s. Srr' models de ma de Ca doo nd'd l-4t. Santa Cara, Sonc. Piiamo, Tafrfs S. Tallta S M L. ChrdoisesVagaoo Sagui o IaGewade. Urbi et Orbi El Cong. Cat6lico Colombiano De la fi.. I ti4 lfr ein. Vida rural. NC Pero ms clu. Imblano de Vid Rural subrayt nuevas tierrat. Is necesidad de una reform ta las Inmensas oorciones del e- I g es y afilhadiqoo siOL e ns lot vastas regions africanas. Se afit qua Una politics di i. An tral" Stan, u eateler q6e1 4e 1e- SNumero cass omerciales exhiben en ]as pteenles hincapie en el evidencee d evelan Is deficiente explotacdcn ides. FIgura i la te. Misa solemne en la Ermita de Montserrat, Ante esta situaci6n de latifun- 'ra obtener un met o rendi- espoa del secretario de honor, Je a Dia Diat; Antomna Vade,. Filix Alluntia O. Jesus Vega Rodrigut. Fote Bauian. Lavin Soleanor har e antre. Los viernes de trbenoc pun rillo de Ena udAe. Sociales a n Miramar. Los vierne s tra laj ha de facilitar e la ai cunto i. Carva al Veras -ia de i ota a dfio e dc tir que Pgando s a o tt d e p t"o bisic del program i la uv. Cat61ica Cuban ha grabs- la Pjrroqua de Monserrate. Esta Coral, e-rtuar la Reserva del Santi realzare today clase de cultivo s aquillon que deberan lr i nor Jose Busamante Rod- oria son trabajadore, qu lab InsuAtuci6n musical que Ie- imo con el E. DEI irtn dade. D g uleJad. Jose gose M C.. Eltruch Ca EL S. Oa ACntoni. Coua s social. Ave d Prlmeraslc y Beltn"s dq La I cuerdan aistir a Ead ouard. Mania Minie. C ae ona del s F tra o illanuesa. G jln Morales. IVaias More soc ia B d r ndr 21M. Manue Alae Fe. Gal ia sen Jose ic nmins Curroas Fe. Jast Enoe Ioru. R Vnel t '. Pa a] inv en todas d ls l ases del erI. M ,p n Alh.. Manuel P reo Grafts, M -. Ivud de Catasus: Oailia Pern n r. M or dqinc aanc s ddn MasaR Cre a nias. C aTa d. Juan Coe Aba- driguez. Ig nal MartI ez MartlG nz. Oilia te las re de Jesus"n a la unas ie r deIarn ds lino t del mi r. Cues'a Igiesas. Lc ea Ba dsai es. Gulerrez Paula. A Aladr G ri. Man uencl ce l cu a ie spoa i ca hrgo n st e acn 'o acl e a la e l" on n iscq o LHbana ene adoradel mon el e s1 I aartMeue a quez alros e nires Aamr "rd re o P-, Festividad d-el lunes sido 1I mstma pues al cu- u a m vis. Is te a d0irectila e Is Bensfi- man e sea e fav el. I Maina. Ca ta D ren. Ua cicia ls iL"ed P ad re. Ifee eu pSractia viaml. Snzcez ie ilan ui n d ale a eC lu alesp e. C r rse dat ie u e r nlnA p r - An inesueeoee pelai as rn- v h l. Sc n ea ntua r el en-si e re VaIa en el que n ha de ul. Vineleene Cn Mon' d I.. A thos -, Uni tin e atanes dc u t nopme. An el Cuba de su s tro am e. Ae C i 'itd1 Hur0s pun Melosi mPetiene. La c si. ZulaI- D s. Eu-Iui dea u i s elebi i manana ho- Is SM. Pc B di c sedel1 M. Bs otia. I Avenuds 20a ilacs 2re delo ut 1Fvern ld is uer: el Iranr- La. A-i i el. A l GeIs le-. A A ndia Pasad Rr ip n uevr b inn mmxlma. Nuestro labor pro. I drt ls sedran Gra e tL a PBah- agi.. Manuel Verga- Is "ad st lanes -- vte -. Saris r-0 e. Iso preIirss out conoe- o prapuesti pan el schism Re- te. Patron y Assieve". Gerveiao e altos ]a Se i t d Is pnd id. D esu Frnnde z sp re dis tin- Club G. Ra n drow. MS tiesals u-lda. Contindan los preparativos on los predios de Tarara Yacht CiuU para festejar alegremente la oes. Con gran animaci6n han re- cibido los socios la noticia de este magnifico belle de Ao. El Comitd de Casa, es el organism encargado de I organized6n. A media noche seri servida Isl tradicional cena de San Siles. Foto DM: Karrefio. Cualquier lnformaci6n adicio- I ra J " tal ser ofrecida por el teliefo- lebrada en jeis de Miraim no de Is secretariat del Club. Anis ve calda y de un blanco purisi- acreditado jardin "Le Prin- bal Duarte Jr. Inclin Villadi. Ernesto P. Smith te cuadrado,. Padre Manuel CoucTeiro. I peados y to folds, con vors y Mendiolia. Armando Cuervo Fer. Despusdde I bobs. Argue-- de re. XNotor XNbe. Carks Arteg. En calidad de testigoa firma- do Garcia Comeaihas. Raul Hermida. ArtWo do b To- de oro con brillantes, que tueron Or. Jos6 A. Casabuena Miranda. GonzAlez Rebull. Hector E. El ramo. Morquez de to Hermmso Cuervo Cuevas. I ibio, u bo ar Para estrenarlos ahora y despedir el aho B 4W f- Q cuan- 'da. Rpuide alivie parn fa de Jesus de Miramar para Entre ]as grandca bodas que una boda de las mayores simpa- se han celebrado duranie la tem- tias. Ia Iiq. Lo pal r sfeeto. Ins mismons qu se repe- te e n a socledad habanera por Ian do trecho en trecho. Conchita Fernandez Ro- El altar mayor resaltaba be- gcr de Cuervo Rubino, cuya re- liamenic sobre el rojn cortina. Do te enlace, sino verbales y pt con l ui tnllette elln que humaa- plmstdo; aprobo deo a; la I prensa. Tara s. Taobis hb. Para analizar las diferencias del peso intragrupo se utilizó el test t pareado, después de la evaluación de la normalidad de los datos por el test de Shapiro-Wilk. No hubo diferencia estadísticamente significativa entre los grupos GC y CC , haciendo la muestra homogénea. Salvador, BA, Brasil, En lo que se refiere a los datos antropométricos, los grupos control e intervención fueron homogéneos. La mediana fue de 90,7 Kg. En cuanto a la circunferencia de la cintura, en la comparación intragrupos, antes y después de la intervención, no se observaron alteraciones estadísticamente significativas. En la tabla 4, se presentan los resultados de la comparación intergrupos después de la intervención. Este ensayo controlado aleatorizado evaluó el efecto del monitoreo remoto de enfermería de mujeres con sobrepeso constatando beneficios en la mejora de las medidas antropométricas y ofrece evidencias para la utilización de esta herramienta terapéutica en el cuidado en salud y enfermería. Las condiciones de desigualdad social exigen enfoques sensibles del equipo de salud, en el sentido de comprender las dificultades de cada persona y adecuar las orientaciones a las mismas. Sin embargo, la mayoría realizaba el trabajo doméstico, confiriendo a ellas el nivel de actividad física activo o muy activo en el domicilio. Este panorama es preocupante, pues la actividad física regular por lo menos minutos por semana es uno de los pilares del tratamiento para reducción del peso El porcentaje de mujeres con obesidad fue superior al de sobrepeso y todas estaban con la circunferencia de la cintura aumentada representando un grupo poblacional con alto riesgo de morbimortalidad. Los datos del presente estudio mostraron que el monitoreo remoto de enfermería fue efectivo una vez que las medidas antropométricas de las mujeres del grupo intervención presentaron reducción con significancia estadística en comparación con el grupo control. Sin embargo, se destaca que el uso de estas tecnologías también logró resultados favorables en la pérdida de peso Se identificó sólo un estudio de intervención educativa que empleó encuentros presenciales y la tecnología del telemonitoreo. En este sentido, el monitoreo remoto es una de las herramientas terapéuticas efectivas para la educación en salud e incentivo al autocuidado. En cuanto a la obesidad, esta estrategia debe considerarse como una opción adicional al tratamiento convencional En condiciones crónicas de salud, a ejemplo de la insuficiencia cardíaca, del infarto agudo de miocardio, de las enfermedades respiratorias y renales crónicas, se ha demostrado que el telemonitoreo proporciona efectos benéficos. Estos beneficios generalmente se refieren al empoderamiento de los usuarios para desempeñar un papel activo en el propio cuidado de la salud, la influencia en sus actitudes y comportamientos y en la mejora de las condiciones clínicas Los resultados de esta investigación pueden contribuir con una visión innovadora para los profesionales de la salud, especialmente de enfermería, que trabajan con personas con sobrepeso. Control de autoridades Proyectos Wikimedia Datos: Q Datos: Q Categorías ocultas: Wikipedia:Artículos que necesitan referencias Wikipedia:Referenciar cine Wikipedia:Artículos con identificadores diferentes en Wikidata..

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{INSERTKEYS} On the magnitude and recurence of Vrancea earthquakes. The moment- magnitude scale Msub W is proposed for the quantification of Vrancea earthquakes. The asperity model is found adequate to explain the observed quasi-cycles and super-cycles in the occurrence of large events.

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Disparities in the Magnitude of Human Immunodeficiency Virus HICs while tuberculosis, candidiasis, chronic diarrhea, and cryptococcosis were predominant Mohar A.

Magnitude and factors associated with post-cesarean surgical site Magnitude and factors associated with post-cesarean surgical site infection Casado pero buscando en Kolka Hawassa University Teaching and referral hospital, southern Ethiopia: a Thus, it should be averted by implementing infection prevention techniques.

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Rapid earthquake magnitude determination for Vrancea early warning system. Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude continue reading the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in Casado pero buscando en Kolka to avoid false alarms.

A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into Casado pero buscando en Kolka that it is computed from only 3 stations in a very short time interval. Impact of magnitude uncertainties on seismic catalogue properties.

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Catalogue-based studies are of central importance in seismological research, to investigate the temporal, spatial and size distribution of earthquakes in specified study areas. Methods for estimating the fundamental catalogue parameters like the Gutenberg-Richter G-R b-value and the completeness magnitude Mc are well established and routinely applied.

However, the magnitudes reported in seismicity catalogues contain measurement uncertainties which may significantly source the estimation of the derived parameters.

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In this study, we use numerical simulations of synthetic data sets to assess the reliability of different methods for determining b-value and Mc, assuming the G-R law validity. After contaminating the synthetic catalogues with Gaussian noise with selected standard deviationsthe analysis is performed for numerous data sets Casado pero buscando en Kolka different sample size N.

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The noise introduced to the data generally leads to a systematic overestimation of magnitudes close to and above Mc. This fact causes an increase of the average number of events above Mc, which in turn leads to an apparent decrease of the b-value.

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This Casado pero buscando en Kolka result to a significant overestimation of seismicity rate even well above the actual completeness level. The b-value can in general be reliably estimated even for relatively small data sets N magnitudes higher than the actual completeness level are used. Nevertheless, a correction of the total number of events belonging in each magnitude class i.

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Because magnitude uncertainties here with the form of Gaussian noise are inevitable in all instrumental catalogues, this finding is fundamental for seismicity rate and seismic Casado pero buscando en Kolka assessment analyses. Also important is that for some data analyses significant bias cannot necessarily be avoided by choosing a high Mc value for analysis.

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In such cases, there may be a risk of severe miscalculation of. The static surface deformation can be recovered Casado pero buscando en Kolka strong motion records. Compared to satellite-based measurements such as GPS or InSAR, the advantage of strong motion records is that they have the potential to provide real-time coseismic static displacements.

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The use of these valuable data was optimized for the moment magnitude estimation. A centroid grid search method was introduced to calculate the moment magnitude by using1 model.

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The method to data sets was applied of the The magnitude of innovation and its evolution in social animals. Innovative behaviour in animals, ranging from invertebrates to humans, is increasingly recognized as an important topic for investigation by behavioural researchers. However, what constitutes an innovation remains controversial, and difficult to quantify.

Ajale Xxxmcom 2 girls 1 pole Two girls posing in a pole dance studio. Allvideo Xxx. A conjunction analysis of the fMRI data revealed commonly activated higher order visual inferior and middle occipital gyrus and parietal inferior and superior parietal lobe magnitude areas for the discrete and continuous magnitude tasks. Moreover, no differences were found when contrasting both magnitude processing conditions, favoring the possibility of a generalized magnitude system. Group comparisons further revealed that dyscalculic subjects showed increased activation in domain general regions, whilst TD peers activate domain specific areas to a greater extent. In conclusion, our results point to the existence of a. The magnitude of an earthquake is one of its basic parameters and is a measure of its scale. It plays a significant role in seismology and earthquake engineering research, particularly in the calculations of the seismic rate and b value in earthquake prediction and seismic hazard analysis. However, several current types of magnitudes used in seismology research, such as local magnitude ML , surface wave magnitude MS , and body-wave magnitude MB , have a common limitation, which is the magnitude saturation phenomenon. Fortunately, the problem of magnitude saturation was solved by a formula for calculating the seismic moment magnitude MW based on the seismic moment, which describes the seismic source strength. Now the moment magnitude is very commonly used in seismology research. However, in China, the earthquake scale is primarily based on local and surface-wave magnitudes. In the present work, we studied the empirical relationships between moment magnitude MW and local magnitude ML as well as surface wave magnitude MS in the Chinese Mainland. Therefore, in China, if the moment magnitude of an earthquake is not reported by any agency in the world, we can use the equations mentioned above for converting ML to MW and MS to MW. These relationships are very important, because they will allow the China earthquake catalogs to be used more effectively for seismic hazard analysis, earthquake prediction, and other seismology research. We also computed the relationships of and where Mo is the seismic moment by linear regression using the Global Centroid Moment Tensor. The goal of tsunami forecast, as a system for predicting potential impact of a tsunami at coastlines, requires quick estimate of a tsunami magnitude. This goal has been recognized since the beginning of tsunami research. The work of Kajiura, Soloviev, Abe, Murty, and many others discussed several scales for tsunami magnitude based on estimates of tsunami energy. However, difficulties of estimating tsunami energy based on available tsunami measurements at coastal sea-level stations has carried significant uncertainties and has been virtually impossible in real time, before tsunami impacts coastlines. The slow process of tsunami magnitude estimates, including collection of vast amount of available coastal sea-level data from affected coastlines, made it impractical to use any tsunami magnitude scales in tsunami warning operations. Uncertainties of estimates made tsunami magnitudes difficult to use as universal scale for tsunami analysis. Historically, the earthquake magnitude has been used as a proxy of tsunami impact estimates, since real-time seismic data is available of real-time processing and ample amount of seismic data is available for an elaborate post event analysis. This measure of tsunami impact carries significant uncertainties in quantitative tsunami impact estimates, since the relation between the earthquake and generated tsunami energy varies from case to case. In this work, we argue that current tsunami measurement capabilities and real-time modeling tools allow for establishing robust tsunami magnitude that will be useful for tsunami warning as a quick estimate for tsunami impact and for post-event analysis as a universal scale for tsunamis inter-comparison. We present a method for estimating the tsunami magnitude based on tsunami energy and present application of the magnitude analysis for several historical events for inter-comparison with existing methods. New moment magnitude scale, evidence of stress drop magnitude scaling and stochastic ground motion model for the French West Indies. S-waves Fourier spectra are analysed to simultaneously determine source, path and site terms. The results show that the duration magnitude routinely estimated for the events that occurred in the region underestimate moment magnitude by 0. From the inverted seismic moments and corner frequencies, we compute Brune's stress drops. We show that stress drops increase with increasing magnitude. The same pattern is observed on apparent stresses i. However, the rate of increase diminishes at high magnitudes , which is consistent with a constant stress drop model for large events. Using the results of the inversions, we perform ground motion simulations for the entire data set using the SMSIM stochastic simulation tool. Although the magnitude -dependent stress drop model is giving better results than the constant stress drop model, the interevent variability remains high, which could suggest that stress drop depends on other parameters such as the depth of the hypocentre. In any case, the overall variability is of the same order of magnitude as usually observed in empirical ground motion prediction equations. This event is larger than previous one in terms of magnitude and showed that measured magnitude strongly depends on the frequency band of data. Relative spectral magnitude varies with frequencies and decreases as frequency increase. A methodology is presented for determining mb Pn magnitude of underground nuclear explosions from local Pn phase. The mb Pn estimates of regional events for Korean Peninsula are determined to be mb Pn? Systematic non-linearity does not observed at frequency band from 0. The magnitude of 6th event is mb Pn 6. Further research of applicable mb Pn magnitude scaling is required for all frequency band and. The bolometric, infrared and visual absolute magnitudes of Mira variables. Statistical parallaxes, as well as stars with individually known distances are used to derive bolometric and infrared absolute magnitudes of Mira Me variables. The derived bolometric magnitudes are in the mean about 0. The problem of determining the pulsation constant is discussed. Miras with periods greater than days probably pulsate in the first overtone. Those of shorter periods are anomalous and may be fundamental pulsators. It is shown that the absolute visual magnitudes at mean light of Miras with individually determined distances are consistent with values derived by Clayton and Feast from statistical parallaxes. Potencial del Agua del suelo. Full Text Available La energía potencial del agua presenta diferencias de un punto del suelo a otro; esas diferencias son las que originan el movimiento del agua de acuerdo a la tendencia universal de la materia en el sentido de moverse de donde la energía potencial es mayor a donde dicha energía es menor. En el suelo el agua en consecuencia se mueve hacia donde su energía decrece hasta lograr su estado de equilibrio. Se desprende entonces que la cantidad de energía potencial absoluta contenida en el agua, no es importante por sí misma, sino por su relación con la energía en diferentes lugares dentro del suelo. El concepto Potencial de agua del suelo es un criterio para esta energía. On the magnitude and recurence of Vrancea earthquakes. The moment- magnitude scale Msub W is proposed for the quantification of Vrancea earthquakes. The asperity model is found adequate to explain the observed quasi-cycles and super-cycles in the occurrence of large events. Disparities in the Magnitude of Human Immunodeficiency Virus HICs while tuberculosis, candidiasis, chronic diarrhea, and cryptococcosis were predominant Mohar A. Magnitude and factors associated with post-cesarean surgical site Magnitude and factors associated with post-cesarean surgical site infection at Hawassa University Teaching and referral hospital, southern Ethiopia: a Thus, it should be averted by implementing infection prevention techniques. Rapid earthquake magnitude determination for Vrancea early warning system. Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude from the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in order to avoid false alarms. A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into account that it is computed from only 3 stations in a very short time interval. Impact of magnitude uncertainties on seismic catalogue properties. Catalogue-based studies are of central importance in seismological research, to investigate the temporal, spatial and size distribution of earthquakes in specified study areas. Methods for estimating the fundamental catalogue parameters like the Gutenberg-Richter G-R b-value and the completeness magnitude Mc are well established and routinely applied. However, the magnitudes reported in seismicity catalogues contain measurement uncertainties which may significantly distort the estimation of the derived parameters. In this study, we use numerical simulations of synthetic data sets to assess the reliability of different methods for determining b-value and Mc, assuming the G-R law validity. After contaminating the synthetic catalogues with Gaussian noise with selected standard deviations , the analysis is performed for numerous data sets of different sample size N. The noise introduced to the data generally leads to a systematic overestimation of magnitudes close to and above Mc. This fact causes an increase of the average number of events above Mc, which in turn leads to an apparent decrease of the b-value. This may result to a significant overestimation of seismicity rate even well above the actual completeness level. The b-value can in general be reliably estimated even for relatively small data sets N magnitudes higher than the actual completeness level are used. Nevertheless, a correction of the total number of events belonging in each magnitude class i. Because magnitude uncertainties here with the form of Gaussian noise are inevitable in all instrumental catalogues, this finding is fundamental for seismicity rate and seismic hazard assessment analyses. Also important is that for some data analyses significant bias cannot necessarily be avoided by choosing a high Mc value for analysis. In such cases, there may be a risk of severe miscalculation of. The static surface deformation can be recovered from strong motion records. Compared to satellite-based measurements such as GPS or InSAR, the advantage of strong motion records is that they have the potential to provide real-time coseismic static displacements. The use of these valuable data was optimized for the moment magnitude estimation. A centroid grid search method was introduced to calculate the moment magnitude by using1 model. The method to data sets was applied of the The magnitude of innovation and its evolution in social animals. Innovative behaviour in animals, ranging from invertebrates to humans, is increasingly recognized as an important topic for investigation by behavioural researchers. However, what constitutes an innovation remains controversial, and difficult to quantify. Drawing on a broad definition whereby any behaviour with a new component to it is an innovation, we propose a quantitative measure, which we call the magnitude of innovation , to describe the extent to which an innovative behaviour is novel. This allows us to distinguish between innovations that are a slight change to existing behaviours low magnitude , and innovations that are substantially different high magnitude. Using mathematical modelling and evolutionary computer simulations, we explored how aspects of social interaction, cognition and natural selection affect the frequency and magnitude of innovation. We show that high- magnitude innovations are likely to arise regularly even if the frequency of innovation is low, as long as this frequency is relatively constant, and that the selectivity of social learning and the existence of social rewards, such as prestige and royalties, are crucial for innovative behaviour to evolve. We suggest that consideration of the magnitude of innovation may prove a useful tool in the study of the evolution of cognition and of culture. Iranian earthquakes, a uniform catalog with moment magnitudes. A uniform earthquake catalog is an essential tool in any seismic hazard analysis. In this study, an earthquake catalog of Iran and adjacent areas was compiled, using international and national databanks. The following priorities were applied in selecting magnitude and earthquake location: a local catalogs were given higher priority for establishing the location of an earthquake and b global catalogs were preferred for determining earthquake magnitudes. In an effort to avoid the "boundary effect," since the newly compiled catalog will be mainly used for seismic hazard assessment, the study area includes the areas adjacent to Iran. The standardization of the catalog in terms of magnitude was achieved by the conversion of all types of magnitude into moment magnitude , M W, by using the orthogonal regression technique. In the newly compiled catalog, all aftershocks were detected, based on the procedure described by Gardner and Knopoff Bull Seismol Soc Am , The seismicity parameters were calculated for the six main tectonic seismic zones of Iran, i. Changes in the timing and magnitude of floods in Canada. It is expected that the global climate change will have significant impacts on the regime of hydrologic extremes. An increase in both the frequency and magnitude of hydrologic extremes is anticipated in the near future. As a consequence, the design and operation of water resource systems will have to adapt to the changing regime of hydrologic extremes. This study explores trends in the timing and magnitude of floods in natural streamflow gauging stations in Canada. The seasonality of floods is analyzed and the selected streamflow stations grouped into five flood seasonality regions. A common year long observation period from to is used in the analysis to eliminate the effect of hydro-climatic variability in the timing and magnitude of floods resulting from different observation periods. The timing of floods is described in terms of directional statistics. A method is developed for analyzing trends in directional dates of flood occurrence that is not affected by the choice of zero direction. The magnitude of floods is analyzed by the annual maximum and peak-over-threshold methods. Trends in the timing and magnitude of floods are identified in each flood seasonality region using the Mann-Kendall nonparametric test, with a modification for auto-correlated data. The results show a good correspondence between the identified flood seasonality regions and the main terrestrial zones in Canada. Significant changes in the timing and magnitude of floods are found in the flood seasonality regions. In the EDZ, the permeability of the rock increases. The annular EDZ surrounding the tunnel may act as a continuous and high-permeable pathway for the groundwater flow, which accelerates the intrusion of groundwater into the repository and increases the release of radionuclide into the biosphere from the repository. Therefore an investigation on the magnitude of the EDZ has been important from the viewpoint of mechanical stability and radiological safety for a geological repository. The magnitude of EDZ was estimated to be 0. The magnitude of EDZ can be estimated to be about 2 m from the viewpoint of permeability, and the permeabilities in the EDZ seem to be increased at up to 2 orders of magnitude compared with those in the intact rock. The magnitude of EDZ estimated based on the permeability is larger than that from the Goodman jack test. The concept of maximum earthquake magnitude mx is widely used in seismic hazard and risk analysis. However, absolute mx lacks a precise definition and cannot be determined from a finite earthquake history. The surprising magnitudes of the Sumatra and the Tohoku earthquakes showed that most methods for estimating mx underestimate the true maximum if it exists. Thus, we introduced the alternate concept of mp T , probable maximum magnitude within a time interval T. Here, we integrate the paleoseismic data in the Cascadia subduction zone to estimate mp. The Cascadia subduction zone has been seismically quiescent since at least Fortunately, turbidite studies have unearthed a 10, year record of great earthquakes along the subduction zone. We thoroughly investigate the earthquake magnitude -frequency distribution of the region by combining instrumental and paleoseismic data, and using the tectonic moment rate information. To use the paleoseismic data, we first estimate event magnitudes , which we achieve by using the time interval between events, rupture extent of the events, and turbidite thickness. We estimate three sets of TGR parameters: for the first two sets, we consider a geographically large Cascadia region that includes the subduction zone, and the Explorer, Juan de Fuca, and Gorda plates; for the third set, we consider a narrow geographic region straddling the subduction zone. Next, we calculate the corresponding mc. Salvador Allende. Medición cuantitativa de la velocidad del habla. La magnitud velocidad del habla no tiene una definición precisa, si bien es ampliamente utilizada tanto en actividades diarias como en tareas específicas como lo son la dactilografía, estenografía y taquigrafía, entre otras. No existe información precisa para el castellano y What controls the maximum magnitude of injection-induced earthquakes? Three different approaches for estimation of maximum magnitude are considered here, along with their implications for managing risk. The first approach is based on a deterministic limit for seismic moment proposed by McGarr , which was originally designed for application to mining-induced seismicity. This approach has since been reformulated for earthquakes induced by fluid injection McGarr, In essence, this method assumes that the upper limit for seismic moment release is constrained by the pressure-induced stress change. A deterministic limit is given by the product of shear modulus and the net injected fluid volume. This method is based on the assumptions that the medium is fully saturated and in a state of incipient failure. An alternative geometrical approach was proposed by Shapiro et al. This assumption reduces the maximum- magnitude problem to one of estimating the largest potential slip surface area within a given stimulated volume. Finally, van der Elst et al. These three models imply different approaches for risk management. The deterministic method proposed by McGarr implies that a ceiling on the maximum magnitude can be imposed by limiting the net injected volume, whereas the approach developed by Shapiro et al. Finally, the sample-size hypothesis of Van der Elst et al. The latter two approaches suggest that real-time monitoring is essential for effective management of risk. A reliable estimate of maximum. The strain energy Est, as potential energy, released by an earthquake and the seismic moment Mo are two fundamental physical earthquake parameters. The moment Mo, first obtained in by Aki, revolutioned the quantification of earthquake size and led to the elimination of the limitations of the conventional magnitudes originally ML, Richter, mb, Ms, m, MGR. Both Mo and Est, not in a 1-to-1 correspondence, are uniform measures of the size, although Est is presently less accurate than Mo. Encuentros Casuales. Sex Cam. Escorts masculinos en Costa Rica. Encuentra hombres guapos en Costa Rica para disfrutar de un encuentro casual en tu ciudad. Clasificados de chico busca chico, escort gay y parejas gays que se anuncian en Skokka de forma totalmente gratuita. Datos: Q Categorías ocultas: Wikipedia:Artículos que necesitan referencias Wikipedia:Referenciar cine Wikipedia:Artículos con identificadores diferentes en Wikidata. Espacios de nombres Artículo Discusión. Vistas Leer Editar Ver historial. Lo hizo o p. E:cUeSIc U e-. Anu:-regavtria par su carel ]. O 1,jes cubanos. Pree Stable: Dr. I eho Boyersd. 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Aquí acaba el desierto y empezamos a andar por Rodra y Dades, zonas de montaña y escalada. Hola Pedro, gracias por tu comentario. Nos a gustado mucho, felicitaciones por el post, hemos tomado nota sera nuestro destino para Diciembre. Un saludo…..

Drawing on a broad definition whereby any behaviour with a new component to it is an innovation, we propose a quantitative measure, which we call the magnitude of innovationto describe the extent to which Casado pero buscando en Kolka innovative behaviour is novel. This allows us to distinguish between innovations that are a slight change to existing behaviours low magnitudeand innovations that are substantially different high magnitude.

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Using mathematical modelling and evolutionary computer simulations, we explored how aspects of social interaction, cognition and natural selection affect the frequency and magnitude of innovation. We show that high- magnitude innovations are likely to arise regularly even if the frequency of innovation is low, as long as this frequency is relatively constant, and that the selectivity of social learning and the existence of social rewards, such as prestige and royalties, are crucial for innovative behaviour to evolve.

We suggest that consideration of the magnitude of innovation may Casado pero buscando en Kolka a useful tool in the study of the evolution of cognition and of culture.

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Iranian earthquakes, a uniform catalog with moment magnitudes. A uniform earthquake catalog is an essential tool in any seismic hazard analysis. In this study, an earthquake catalog of Iran and adjacent areas was compiled, using international and national databanks.

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The following priorities were applied in selecting magnitude and earthquake location: a local catalogs were given higher priority for establishing the location of an earthquake and b global catalogs were preferred for determining earthquake magnitudes.

In an effort to avoid the "boundary effect," since the newly compiled catalog will be mainly used for seismic hazard assessment, the study area includes the areas adjacent to Iran. The standardization of the catalog in terms Casado pero buscando en Kolka magnitude was achieved by the conversion of all types of magnitude into moment magnitudeM W, by using the orthogonal Casado pero buscando en Kolka technique.

In the newly compiled catalog, all aftershocks were detected, based on the procedure described by Gardner and Knopoff Bull Seismol Soc Am The seismicity parameters were calculated for the six main tectonic seismic zones of Iran, i. Changes in the timing and magnitude of floods in Canada.

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It is expected that the global climate change will have significant impacts on the regime of hydrologic extremes. An increase in both the frequency and magnitude of hydrologic extremes is anticipated in the near future.

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As a consequence, the design and operation of water resource systems will have to adapt to the changing regime of hydrologic extremes.

This study explores trends in the timing and magnitude of floods in Casado pero buscando en Kolka streamflow gauging stations in Canada. The seasonality of floods is analyzed and the selected streamflow stations grouped into five flood seasonality regions.

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A common year long observation period from to is used in the analysis to eliminate the effect of hydro-climatic variability in the timing and magnitude of floods resulting from different observation periods. The timing of floods is described in terms of directional statistics. A method is developed for analyzing trends in directional dates of flood occurrence that is not affected by the choice of zero Casado pero buscando en Kolka.

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The magnitude of floods is analyzed by the annual maximum and peak-over-threshold methods. Casado pero buscando en Kolka in the timing and magnitude of floods are identified in each flood seasonality region using the Mann-Kendall nonparametric test, with a modification for auto-correlated data. The results show a good correspondence between the identified flood seasonality regions and the main terrestrial zones in Canada. Significant changes in the timing and magnitude of floods are found in the flood seasonality regions.

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Ayetarin IMui Tel. Fredrih March y Klin' lotet. Nottceror na lonRlo El on. Balcony 30 Dttan Video lepn. InO - a. IE L Lm. The Gutenberg-Richter nomograph is applied to the peak amplitudes for 24 large underground nuclear explosions that took place in Nevada. The amplitudes were measured at 18 California Wood-Anderson stations located km from the explosion epicenter. The variation of the individual station magnitudes and magnitude corrections and the variation of the average and rms error estimates in the magnitude determinations are examined with respect to distance, azimuth, and event location. The magnitude prediction capability of the Gutenberg-Richter nomograph is examined on the basis of these two criteria, and certain corrections are suggested. The azimuthal dependence of the individual station magnitudes is investigated, and corrections for the California stations are calculated. Statistical weighting schemes for two-component data are employed, and the assumptions and limitations in the use of peak amplitudes are discussed. Extreme value distribution of earthquake magnitude. Probability distribution of maximum earthquake magnitude is first derived for an unspecified probability distribution of earthquake magnitude. A model for energy release of large earthquakes, similar to that of Adler-Lomnitz and Lomnitz, is introduced from which the probability distribution of earthquake magnitude is obtained. An extensive set of world data for shallow earthquakes, covering the period from to , is used to determine the parameters of the probability distribution of maximum earthquake magnitude. Because of the special form of probability distribution of earthquake magnitude , a simple iterative scheme is devised to facilitate the estimation of these parameters by the method of least-squares. The agreement between the empirical and derived probability distributions of maximum earthquake magnitude is excellent. The children's pretest numerical magnitude representations were found to be correlated with their pretest arithmetic knowledge and to be…. Representations of the Magnitudes of Fractions. We tested whether adults can use integrated, analog, magnitude representations to compare the values of fractions. The only previous study on this question concluded that even college students cannot form such representations and instead compare fraction magnitudes by representing numerators and denominators as separate whole numbers. Magnitude of localized magnetic moments in metals. The magnitude of the localized magnetic moment of a transition or rare earth element impurity in a metal is evaluated within the framework of the Anderson model. Rotational invariance is preserved throughout. Graphs of the magnitude of the magnetization as a function of the relevant parameters of the model are provided and discussed. Local magnitudes of small contained explosions. The relationship between explosive yield and seismic magnitude has been extensively studied for underground nuclear tests larger than about 1 kt. For monitoring smaller tests over local ranges within km , we need to know whether the available formulas can be extrapolated to much lower yields. Here, we review published information on amplitude decay with distance, and on the seismic magnitudes of industrial blasts and refraction explosions in the western U. Next we measure the magnitudes of some similar shots in the northeast. We find that local magnitudes ML of small, contained explosions are reasonably consistent with the magnitude -yield formulas developed for nuclear tests. These results are useful for estimating the detection performance of proposed local seismic networks. Discounting Behaviour and the Magnitude Effect. We evaluate the claim that individuals exhibit a magnitude effect in their discounting behaviour, where higher discount rates are inferred from choices made with lower principals, all else being equal. If the magnitude effect is quantitatively significant, it is not appropriate to use one discount Using data from a field experiment in Denmark, we find statistically significant evidence of a magnitude effect that is much smaller than is claimed. This evidence surfaces only if one controls Determination of the Meteor Limiting Magnitude. The limiting meteor magnitude of a meteor camera system will depend on the camera hardware and software, sky conditions, and the location of the meteor radiant. Some of these factors are constants for a given meteor camera system, but many change between meteor shower or sporadic source and on both long and short timescales. Since the limiting meteor magnitude ultimately gets used to calculate the limiting meteor mass for a given data set, it is important to have an understanding of these factors and to monitor how they change throughout the night, as a 0. The Magnitude of Atherogenic Dyslipidaemia among Geriatric June on consecutive geriatric patients with systemic hypertension Measuring radon source magnitude in residential buildings. A description is given of procedures used in residences for rapid grab-sample and time-dependent measurements of the air-exchange rate and radon concentration. The radon source magnitude is calculated from the results of simultaneous measurements of these parameters. Grab-sample measurements in three survey groups comprising US houses showed the radon source magnitude to vary approximately log-normally with a geometric mean of 0. Successive measurements in six houses in the northeastern United States showed considerable variability in source magnitude within a given house. In two of these houses the source magnitude showed a strong correlation with the air-exchange rate, suggesting that soil gas influx can be an important transport process for indoor radon. Comparar esse sistema a um sistema computacional de acesso livre. Time series of increments can be created in a number of different ways from a variety of physical phenomena. For example, in the phenomenon of volatility clustering-well-known in finance- magnitudes of adjacent increments are correlated. Here we define a model-independent test to measure the statistical significance of any observed asymmetry. We propose a simple stochastic process characterized by a an asymmetry parameter lambda and a method for estimating lambda. We illustrate both the test and process by analyzing physiological data. Local magnitude , duration magnitude and seismic moment of Dahshour earthquakes. Full Text Available Local magnitudes ML have been calculated for 56 earthquakes of the Dahshour sequence using simulated records of the KEG broadband station and the estimated calibration function of the Dahshour area. These were compared with their corresponding values of duration magnitudes obtained from the analog short period seismograms of the HLW station. Seismic moment has also been estimated for these events using simple measurements from the time domain records. These measurements based on the simulated Wood Anderson seismograms are used for the local magnitude ML estimation. The moment magnitude Mw and the energy magnitude Me: common roots and differences. Abstract Starting from the classical empirical magnitude -energy relationships, in this article, the derivation of the modern scales for moment magnitude Mw and energy magnitude Me is outlined and critically discussed. The formulas for Mw and Me calculation are presented in a way that reveals, besides the contributions of the physically defined measurement parameters seismic moment M0 and radiated seismic energy ES, the role of the constants in the classical Gutenberg? Richter magnit Colour- magnitude diagram of NGC The electronographic observations were obtained with an experimental Spectracon image-converter, having photocathode and exit window dimensions of 20 x 30 mm, mounted at the prime-focus of the in. Lick reflector. The photographic observations were obtained with the in. Carnegie astrograph and the in. Crossley reflector. The colour- magnitude diagram resembles that of M92, with the difference that a red horizontal branch is more pronounced than the asymptotic branch in NGC The topology of the horizontal branch is that of clusters with an intermediate metal content and is thus at variance with the mean period of the RR Lyr stars and the unreddened colour of the subgiant branch read at the magnitude level of the horizontal branch, both of which would indicate an extremely low metal content. Historical revision of the exposure magnitude and the dosimetric magnitudes used in radiological protection; Revision historica de la magnitud exposicion y las magnitudes dosimetricas empleadas en proteccion radiologica. Gonzalez J, F. Mexico ; Alvarez R, J. In this work a historical revision of the exposure magnitude development and their roentgen unit - is made, noting that it had their origin in the electric methods for the detection of the ionizing radiation in the period of at However, the ionization is not who better characterizes the physical, chemical and biological effects of the ionizing radiations, but is the energy deposited by this radiation in the interest bodies, which led historically to the development of dosimetric magnitudes in energy terms like they are: the absorbed dose D , the kerma K and the equivalent dose H Interaction of Number Magnitude and Auditory Localization. The interplay of perception and memory is very evident when we perceive and then recognize familiar stimuli. Conversely, information in long-term memory may also influence how a stimulus is perceived. Prior work on number cognition in the visual modality has shown that in Western number systems long-term memory for the magnitude of smaller numbers can influence performance involving the left side of space, while larger numbers have an influence toward the right. Here, we investigated in the auditory modality whether a related effect may bias the perception of sound location. The noise bursts were preceded by a spoken number or, as a nonsemantic control condition, numbers that were played in reverse. The relative constant error in noise localization forward minus reversed speech indicated a systematic shift in localization toward more central locations when the number was smaller and toward more peripheral positions when the preceding number magnitude was larger. These findings do not support the traditional left-right number mapping. Instead, the results may reflect an overlap between codes for number magnitude and codes for sound location as implemented by two channel models of sound localization, or possibly a categorical mapping stage of small versus large magnitudes. Incentive theory: IV. Magnitude of reward. Incentive theory is successfully applied to data from experiments in which the amount of food reward is varied. This is accomplished by assuming that incentive value is a negatively accelerated function of reward duration. The interaction of the magnitude of a reward with its delay is confirmed, and the causes and implications of this interaction are discussed. Local magnitudes ML have been calculated for 56 earthquakes of the Dahshour sequence using simulated records of the KEG broadband station and the estimated calibration function of the Dahshour area. Absolute- magnitude distributions of supernovae. The absolute- magnitude distributions of seven supernova SN types are presented. The data used here were primarily taken from the Asiago Supernova Catalogue, but were supplemented with additional data. We accounted for both foreground and host-galaxy extinction. A bootstrap method is used to correct the samples for Malmquist bias. Separately, we generate volume-limited samples, restricted to events within Mpc. The normal Ia distribution was the brightest with a mean absolute blue magnitude of — The IIP distribution was the dimmest at — Magnitudes and units in radiation protection. This sheet provides definition and information on the ionizing radiations, the measurement of a ionizing radiation magnitude by a radioactive source the becquerel , the measurement of the ionizing radiation energy absorbed by the organism the gray , the biological impact evaluation of ionizing radiations in function of their nature the sievert and the evaluation and comparison of biological risks bond to little doses dose efficiency. Improving Children's Knowledge of Fraction Magnitudes. Full Text Available We examined whether playing a computerized fraction game, based on the integrated theory of numerical development and on the Common Core State Standards' suggestions for teaching fractions, would improve children's fraction magnitude understanding. Fourth and fifth-graders were given brief instruction about unit fractions and played Catch the Monster with Fractions, a game in which they estimated fraction locations on a number line and received feedback on the accuracy of their estimates. In our initial study, children showed large gains from pretest to posttest in their fraction number line estimates, magnitude comparisons, and recall accuracy. In a more rigorous second study, the experimental group showed similarly large improvements, whereas a control group showed no improvement from practicing fraction number line estimates without feedback. The results provide evidence for the effectiveness of interventions emphasizing fraction magnitudes and indicate how psychological theories and research can be used to evaluate specific recommendations of the Common Core State Standards. However, the scatter between ML and Mw at small magnitudes is usually large and the resulting scaling relations are therefore uncertain. In an attempt to reduce these uncertainties, we first analyze the ML versus Mw relation based on events, induced by the stimulation of a geothermal reservoir below the city of Basel, Switzerland. Values of ML range from 0. Because effects due to the radiation pattern and to the propagation path between source and receiver are nearly identical at a particular station for all events in a given sequence, the scatter in the data is substantially reduced. Based on simulations using synthetic source time functions for different magnitudes and Q values estimated from spectral ratios between downhole and surface recordings, we conclude that the observed scaling can be explained by attenuation and scattering along the path. Other effects that could explain the observed magnitude scaling, such as a possible systematic increase of stress drop or rupture velocity with moment magnitude , are masked by attenuation along the path. Strong motion duration and earthquake magnitude relationships. Earthquake duration is the total time of ground shaking from the arrival of seismic waves until the return to ambient conditions. Much of this time is at relatively low shaking levels which have little effect on seismic structural response and on earthquake damage potential. As a result, a parameter termed ''strong motion duration'' has been defined by a number of investigators to be used for the purpose of evaluating seismic response and assessing the potential for structural damage due to earthquakes. This report presents methods for determining strong motion duration and a time history envelope function appropriate for various evaluation purposes, for earthquake magnitude and distance, and for site soil properties. There are numerous definitions of strong motion duration. For most of these definitions, empirical studies have been completed which relate duration to earthquake magnitude and distance and to site soil properties. Each of these definitions recognizes that only the portion of an earthquake record which has sufficiently high acceleration amplitude, energy content, or some other parameters significantly affects seismic response. Studies have been performed which indicate that the portion of an earthquake record in which the power average rate of energy input is maximum correlates most closely with potential damage to stiff nuclear power plant structures. Hence, this report will concentrate on energy based strong motion duration definitions. Sequential dependencies in magnitude scaling of loudness. Ten normally hearing listeners used a programmable sone-potentiometer knob to adjust the level of a Hz sinusoid to match the loudness of numbers presented to them in a magnitude production task. Three different power-law exponents 0. B were used to program the sone-potentiometer. The knob settings systematically influenced the form of the loudness function. Time series analysis was used to assess the sequential dependencies in the data, which increased with increasing exponent and were greatest for the log-law. 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Gender-specific demographic factors and lifestyle habits related to physical inactivity. Rev Nutr. Physical exercises as a strategy to prevent and to treat obesity: physiological and methodological aspects. Women's meal frequency and nutritional and health profiles. Rev Esp Cardiol. Obesity, insulin resistance and comorbidities? Mechanisms of association. Arq Bras Endocrinol Metab. J Am Diet Assoc..

In the EDZ, the permeability of the rock increases. The annular EDZ surrounding the tunnel may act as a Casado pero buscando en Kolka and high-permeable pathway for the groundwater flow, which accelerates the intrusion of groundwater into the repository and increases the release of radionuclide into the biosphere from the repository. Therefore an investigation on the magnitude of the EDZ has been important from the viewpoint of mechanical stability and radiological safety for a geological repository.

The magnitude of EDZ was estimated to be 0.

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The magnitude of EDZ can be estimated to be about 2 m from the Casado pero buscando en Kolka of permeability, and the permeabilities in the EDZ seem to be increased https://blog-4.frugalphotographer.store/tag-21-08-2020.php up to 2 orders of magnitude compared with those in the intact rock. The magnitude of EDZ estimated based on the permeability is larger than that from the Goodman jack test.

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The concept of maximum earthquake magnitude mx is widely used in seismic hazard and risk analysis. However, absolute mx lacks a precise definition and cannot be determined from a finite earthquake history. The surprising magnitudes of the Sumatra and the Tohoku earthquakes showed that most methods for Casado pero buscando en Kolka mx underestimate the true maximum if it exists.

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Thus, we introduced the alternate concept of mp Tprobable maximum magnitude within a time interval T. Here, we integrate the paleoseismic Casado pero buscando en Kolka in the Cascadia subduction zone to estimate mp. The Cascadia subduction zone has been seismically quiescent since at least Fortunately, turbidite studies have unearthed a 10, year record of great earthquakes along the subduction zone.

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We thoroughly investigate the earthquake magnitude -frequency distribution of the region by combining instrumental and paleoseismic data, and using the tectonic moment rate information. To use the paleoseismic data, we Casado pero buscando en Kolka estimate event magnitudeswhich we achieve by using the time interval between events, rupture extent of the events, and turbidite thickness.

We estimate three sets of TGR parameters: for the first two Casado pero buscando en Kolka, we consider a geographically large Cascadia region that includes the subduction zone, and the Explorer, Juan de Fuca, and Gorda plates; for the third set, we consider a narrow geographic region straddling the subduction zone.

Next, we calculate the corresponding mc.

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La magnitud velocidad del habla no tiene una definición precisa, si bien es ampliamente utilizada tanto en actividades diarias como en tareas específicas como lo son la dactilografía, estenografía y taquigrafía, entre otras. No existe información precisa para el castellano y What controls the maximum magnitude of injection-induced earthquakes?

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Three different approaches for estimation of maximum magnitude are considered here, along with their implications for managing risk. The first approach is based on a deterministic limit for seismic moment proposed by McGarrwhich was originally designed for application to mining-induced seismicity.

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This approach has since been reformulated for earthquakes induced by fluid injection McGarr, In essence, this method assumes Casado pero buscando en Kolka the upper limit for seismic moment release is constrained by the pressure-induced stress change. A deterministic limit is given by the product of shear modulus and the net injected fluid volume. This method is based on the assumptions that the medium is fully saturated and in a state of incipient failure.

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An alternative geometrical approach was proposed by Shapiro et al. This assumption reduces the maximum- magnitude problem to one of estimating the largest potential slip surface area within a given stimulated volume.

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Finally, van der Elst et al. These three models imply different approaches for risk management. The deterministic method proposed by McGarr implies that a ceiling on the maximum magnitude can be imposed by limiting the net injected volume, whereas the approach developed by Shapiro et al.

Finally, the sample-size hypothesis of Van der Elst et al.

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The latter two approaches suggest that real-time monitoring is essential for effective management of risk. A reliable estimate of maximum.

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The strain energy Est, as potential energy, released by an earthquake and the seismic moment Mo are two fundamental physical earthquake parameters. The moment Mo, first obtained in by Aki, revolutioned the quantification of earthquake size and led to the Casado pero buscando en Kolka of the limitations of the conventional magnitudes originally ML, Richter, mb, Ms, m, MGR. Both Mo and Est, not in a 1-to-1 correspondence, are uniform measures of the size, although Est is presently less accurate than Mo.

Casado pero buscando en Kolka

Est is partitioned in seismic- Esfracture- Eg and frictional-energy Ef, and Ef is lost as frictional heat energy.

Related to Mo, Est and Es, several modern magnitudes were defined under various assumptions: the moment magnitude Mw Kanamori,strain energy magnitude ME Purcaru and Berckhemer,tsunami magnitude Mt Abe,mantle magnitude Mm Okal and Talandier,seismic energy magnitude Me Choy and Boatright,Yanovskaya et al,body-wave magnitude Mpw Tsuboi et Casado pero buscando en Kolka, Results for some.

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Magnitude corrections for attenuation in the upper mantle. Sincea consistent discrepancy in seismic magnitudes of nuclear detonations at NTS compared with Casado pero buscando en Kolka of detonations elsewhere in the world has been observed. This discrepancy can be explained in terms of a relatively high seismic attenuation for compressional waves in the upper mantle beneath the NTS and in certain other locations. A correction has been developed for this attenuation based on a relationship between the velocity of compressional waves at the top of the earth's mantle just beneath the Mohorovicic discontinuity and the seismic attenuation further down in the upper mantle.

Our new definition of body-wave magnitude includes corrections for attenuation in the upper mantle at both ends of the teleseismic Casado pero buscando en Kolka path. These corrections bring the NTS oservations into line with measurements of foreign events, and enable one to make more reliable estimates of yields of underground nuclear explosions, wherever see more explosion occurs.

Magnitude and duration of stretch modulate fibroblast remodeling. Mechanical cues modulate fibroblast tractional forces and remodeling of extracellular matrix in healthy tissue, healing wounds, and engineered matrices.

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The goal of the present study is to establish dose-response relationships between stretch parameters magnitude and duration per day and matrix remodeling metrics compaction, strength, extensibility, collagen content, contraction, and cellularity. Trends in matrix remodeling metrics as a Casado pero buscando en Kolka of stretch magnitude and duration were analyzed using regression analysis. Collagen density increased exponentially as a function of both the magnitude and duration of https://map-i.frugalphotographer.store/blog-2020-04-17.php, with samples stretched for the reduced duration per day having the highest levels of collagen accumulation.

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Our results indicate that both the magnitude and the duration per day of stretch are critical Casado pero buscando en Kolka in modulating fibroblast remodeling of the extracellular matrix, and that these two factors regulate different aspects of this remodeling.

These findings move us one step closer to fully characterizing culture conditions for tissue equivalents, developing improved Casado pero buscando en Kolka healing treatments and understanding tissue responses to changes in mechanical environments during growth, repair, and disease states.

Color- magnitude relations in nearby galaxy clusters. We show that the color- magnitude relation parameters slope, zero-point, and scatter do not exhibit significant evolution within this low-redshift range. High- magnitude head impact exposure in youth football. OBJECTIVE Even in the absence of a clinically diagnosed concussion, research suggests that neurocognitive changes may develop in football players as a result of frequent head impacts that occur during football games and practices.

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The objectives of this study were to determine the specific situations in which high- magnitude impacts accelerations exceeding 40g occur in youth football games and practices and to assess how representative practice activities are of games with regard to high- magnitude head impact exposure. Video recordings from practices and games were used to verify all high- magnitude head impacts, identify specific impact characteristics, and determine the amount of time Casado pero buscando en Kolka in each activity.

Impacts were characterized based on the position played by the team member who received the Casado pero buscando en Kolka, the part of the field where the impact occurred, whether the impact occurred during a game or practice play, and the cause of the impact.

High- magnitude impacts occurred most frequently in the open field in both games Aunque varios de los continue reading del avión mueren Grivtsov y Katya se salvan milagrosamente, mientras que Linko también sobrevive luego de saltar en paracaídas del avión.

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The IG received remote monitoring through telephone calls and conventional monitoring, and the CG received conventional monitoring. Women were assessed at the baseline and after three months of intervention. Eighty one women completed the study.

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Casado pero buscando en Kolka En Brasil, el sobrepeso viene aumentando en todas las edades, en ambos sexos, en todos los niveles de ingreso y de escolaridad 5. Las causas del Casado pero buscando en Kolka son complejas y multifactoriales, incluyen factores biológicos, ambientales, sociales y psicológicos, haciendo el control un desafío, principalmente el mantenimiento de la pérdida de peso a largo plazo 6 - 7.

Asociado a pocas opciones de tratamiento con eficacia comprobada para el control del peso, la insuficiencia de servicio de referencia con personal capacitado y una aparente falta de tiempo y de motivación de los clientes parecen componer el problema 9 - En las sociedades modernas, el aumento del consumo de alimentos ricos en grasas y carbohidratos con alta densidad energética y reducción de los niveles de actividad física ha favorecido la ganancia de peso 3.

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Como el exceso de tejido adiposo visceral se ha Casado pero buscando en Kolka con el síndrome metabólico y otras enfermedades crónicas, la evaluación de la grasa visceral es indicada como importante marcador. Para esta evaluación se ha recomendado la medida de la cintura asociada al IMC 6 Todavia, pouco se conhece seus benefícios no manejo do controle do peso.

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El monitoreo remoto es una tecnología innovadora que puede ayudar a las personas en situación crónica Casado pero buscando en Kolka la salud resultando en una mayor sensación de empoderamiento, mejor gestión de la enfermedad y en la adhesión al tratamiento. Sin embargo, poco se conocen sus beneficios en el manejo del control del peso. Las investigaciones que usaron esta tecnología en su mayoría se realizaron con personas con otros problemas crónicos de salud como enfermedad pulmonar obstructiva crónica, insuficiencia cardíaca congestiva y diabetes mellitus 16 - En este contexto, el presente estudio tuvo el objetivo de evaluar el efecto del monitoreo remoto de enfermería en la mejora de las medidas antropométricas de mujeres con sobrepeso.

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Se trata de un Casado pero buscando en Kolka clínico aleatorio y controlado, realizado en un servicio de ambulatorio de referencia para obesidad en la ciudad de Salvador, Bahia, Brasil. Todas las participantes firmaron el término de consentimiento libre y esclarecido.

Para todas aquellas que atendieron a los criterios de inclusión y exclusión se hizo la invitación para click de la investigación y se programaron fechas Casado pero buscando en Kolka para la recolección de los datos iniciales, con cerca de 20 participantes por día. De estas, asistieron y constituyeron el baseline. Pareja Busca Chica.

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Casado pero buscando en Kolka

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Facefuck cartoon p Dani daniels i have a wife. Chubby Milf. Iranians Porn. Un saludo…. Sitio Web dato opcional. Este sitio usa Akismet para reducir el spam. Aprende cómo se procesan los datos de tus comentarios. Blog de viajes para exploradores, aventureros y ahorradores. Etiquetas: desierto , Marruecos , merzouga , rissani. Genial la web! Cuanto os costó el tour por el desierto por persona? Y el albergue? Temporal and spatial variations in the magnitude of completeness for homogenized moment magnitude catalogue for northeast India. Ranjit Das H R Orthogonal regression relations for conversion of body and surface wave magnitudes to w,HRVD based on events data for the period — have been derived. A combined bootstrap and orthogonal L1 minimization is then used to produce a scaling relation bet Magnitudes and frequencies of earthquakes in relation to seismic risk. Estimating the frequencies of occurrence of earthquakes of different magnitudes on a regional basis is an important task in estimating seismic risk at a construction site. Analysis of global earthquake data provides an insight into the magnitudes frequency relationship in a statistical manner. It turns out that, whereas a linear relationship between the logarithm of earthquake occurrence rates and the corresponding earthquake magnitudes fits well in the magnitude range between 5 and 7, a second degree polynomial in M, the earthquake magnitude provides a better description of the frequencies of earthquakes in a much wider range of magnitudes. It may be possible to adopt magnitude frequency relation for regions, for which adequate earthquake data are not available, to carry out seismic risk calculations. We present a simple and fast method for magnitude determination technique for earthquake and tsunami early warning systems based on strong ground motion prediction equations GMPEs in Japan. This method incorporates borehole strong motion records provided by the Kiban Kyoshin network KiK-net stations. We analyzed strong ground motion data from large magnitude earthquakes 5. Mpga and Mpgv strongly correlate with the moment magnitude of the event, provided sufficient records for each event are available. The results show that Mpgv has a smaller standard deviation in comparison to Mpga when compared with the estimated magnitudes and provides a more accurate early assessment of earthquake magnitude. We test this new method to estimate the magnitude of the Tohoku earthquake and we present the results of this estimation. PGA and PGV from borehole recordings allow us to estimate the magnitude of this event s and s after the earthquake onset, respectively. We demonstrate that the incorporation of borehole strong ground-motion records immediately available after the occurrence of large earthquakes significantly increases the accuracy of earthquake magnitude estimation and the associated improvement in earthquake and tsunami early warning systems performance. Moment magnitude versus predicted magnitude Mpga and Mpgv. Numerous studies have tried to identify the core deficit of developmental dyscalculia DD , mainly by assessing a possible deficit of the mental representation of numerical magnitude. Research in healthy adults has shown that numerosity, duration, and space share a partly common system of magnitude processing and representation. However, in DD, numerosity processing has until now received much more attention than the processing of other non-numerical magnitudes. To assess whether or not the processing of non-numerical magnitudes is impaired in DD, the performance of 15 adults with DD and 15 control participants was compared in four categorization tasks using numerosities, lengths, durations, and faces as non- magnitude -based control stimuli. Results showed that adults with DD were impaired in processing numerosity and duration, while their performance in length and face categorization did not differ from controls' performance. Our findings support the idea of a nonsymbolic magnitude deficit in DD, affecting numerosity and duration processing but not length processing. Consideration of reinforcer magnitude may be important for maximizing the efficacy of treatment for problem behavior. Nonetheless, relatively little is known about children's preferences for different magnitudes of social reinforcement or the extent to which preference is related to differences in reinforcer efficacy. The purpose of the current study was to evaluate the relations among reinforcer magnitude , preference, and efficacy by drawing on the procedures and results of basic experimenta Integration and magnitude homogenization of the Egyptian earthquake catalogue. Hussein, H. The aim of the present work is to compile and update a catalogue of the instrumentally recorded earthquakes in Egypt, with uniform and homogeneous source parameters as required for the analysis of seismicity and seismic hazard assessment. This in turn requires a detailed analysis and comparison of the properties of different available sources, including the distribution of events with time, the magnitude completeness and the scaling relations between different kinds of magnitude reported by different agencies. The observational data cover the time interval and an area between The linear regressions between various magnitude types have been evaluated for different magnitude ranges. Using the best linear relationship determined for each available pair of magnitudes , as well as those identified between the magnitudes and the seismic moment, we convert the different magnitude types into moment magnitudes M W , through a multi-step conversion process. Analysis of the catalogue completeness, based on the MW thus estimated, allows us to identify two different time intervals with homogeneous properties. De esta manera los límites este y oeste quedaron establecidos por la confluencia de los ríos antes mencionados y la localidad de Bajada del Agrio, respectivamente. We illustrate two essential consequences of the systematic difference between moment magnitude and local magnitude for small earthquakes, illuminating the underlying earthquake physics. However, the relationship between local magnitude ML and moment is itself magnitude dependent. Just as importantly, if this relation is overlooked, prediction of large- magnitude ground motion from small earthquakes will be misguided. We also consider the effect of this magnitude scale difference on b-value. The oft-cited b-value of 1 should hold for small magnitudes , given M. This is of particular import when estimating the rate of large earthquakes when one has limited data on their recurrence, as is the case for induced earthquakes in the central US. The integrated theory of numerical development posits that a central theme of numerical development from infancy to adulthood is progressive broadening of the types and ranges of numbers whose magnitudes are accurately represented. The process includes four overlapping trends: 1 representing increasingly precisely the magnitudes of non-symbolic…. We investigated the relation between children's numerical- magnitude representations and their memory for numbers. Results of three experiments indicated that the more linear children's magnitude representations were, the more closely their memory of the numbers approximated the numbers presented. This relation was present for preschoolers and…. Non extensivity and frequency magnitude distribution of earthquakes. Starting from first principles in this case a non-extensive formulation of the maximum entropy principle and a phenomenological approach, an explicit formula for the magnitude distribution of earthquakes is derived, which describes earthquakes in the whole range of magnitudes. The Gutenberg-Richter law appears as a particular case of the obtained formula. Comparison with geophysical data gives a very good agreement. Trosclair-Lasserre, Nicole M. The purpose of the current…. The link between number and space has been discussed in the literature for some time, resulting in the theory that number, space and time might be part of a generalized magnitude system. To date, several behavioral and neuroimaging findings support the notion of a generalized magnitude system, although contradictory results showing a partial overlap or separate magnitude systems are also found. The possible existence of a generalized magnitude processing area leads to the question how individuals with developmental dyscalculia DD , known for deficits in numerical-arithmetical abilities, process magnitudes. By means of neuropsychological tests and functional magnetic resonance imaging fMRI we aimed to examine the relationship between number and space in typical and atypical development. Participants were 16 adolescents with DD In the fMRI paradigm participants had to perform discrete arrays of dots and continuous magnitude angles comparisons as well as a mental rotation task. In the neuropsychological tests, adolescents with dyscalculia performed significantly worse in numerical and complex visuo-spatial tasks. However, they showed similar results to TD peers when making discrete and continuous magnitude decisions during the neuropsychological tests and the fMRI paradigm. A conjunction analysis of the fMRI data revealed commonly activated higher order visual inferior and middle occipital gyrus and parietal inferior and superior parietal lobe magnitude areas for the discrete and continuous magnitude tasks. Moreover, no differences were found when contrasting both magnitude processing conditions, favoring the possibility of a generalized magnitude system. Group comparisons further revealed that dyscalculic subjects showed increased activation in domain general regions, whilst TD peers activate domain specific areas to a greater extent. In conclusion, our results point to the existence of a. The magnitude of an earthquake is one of its basic parameters and is a measure of its scale. It plays a significant role in seismology and earthquake engineering research, particularly in the calculations of the seismic rate and b value in earthquake prediction and seismic hazard analysis. However, several current types of magnitudes used in seismology research, such as local magnitude ML , surface wave magnitude MS , and body-wave magnitude MB , have a common limitation, which is the magnitude saturation phenomenon. Fortunately, the problem of magnitude saturation was solved by a formula for calculating the seismic moment magnitude MW based on the seismic moment, which describes the seismic source strength. Now the moment magnitude is very commonly used in seismology research. However, in China, the earthquake scale is primarily based on local and surface-wave magnitudes. In the present work, we studied the empirical relationships between moment magnitude MW and local magnitude ML as well as surface wave magnitude MS in the Chinese Mainland. Therefore, in China, if the moment magnitude of an earthquake is not reported by any agency in the world, we can use the equations mentioned above for converting ML to MW and MS to MW. These relationships are very important, because they will allow the China earthquake catalogs to be used more effectively for seismic hazard analysis, earthquake prediction, and other seismology research. We also computed the relationships of and where Mo is the seismic moment by linear regression using the Global Centroid Moment Tensor. The goal of tsunami forecast, as a system for predicting potential impact of a tsunami at coastlines, requires quick estimate of a tsunami magnitude. This goal has been recognized since the beginning of tsunami research. The work of Kajiura, Soloviev, Abe, Murty, and many others discussed several scales for tsunami magnitude based on estimates of tsunami energy. However, difficulties of estimating tsunami energy based on available tsunami measurements at coastal sea-level stations has carried significant uncertainties and has been virtually impossible in real time, before tsunami impacts coastlines. The slow process of tsunami magnitude estimates, including collection of vast amount of available coastal sea-level data from affected coastlines, made it impractical to use any tsunami magnitude scales in tsunami warning operations. Uncertainties of estimates made tsunami magnitudes difficult to use as universal scale for tsunami analysis. Historically, the earthquake magnitude has been used as a proxy of tsunami impact estimates, since real-time seismic data is available of real-time processing and ample amount of seismic data is available for an elaborate post event analysis. This measure of tsunami impact carries significant uncertainties in quantitative tsunami impact estimates, since the relation between the earthquake and generated tsunami energy varies from case to case. In this work, we argue that current tsunami measurement capabilities and real-time modeling tools allow for establishing robust tsunami magnitude that will be useful for tsunami warning as a quick estimate for tsunami impact and for post-event analysis as a universal scale for tsunamis inter-comparison. We present a method for estimating the tsunami magnitude based on tsunami energy and present application of the magnitude analysis for several historical events for inter-comparison with existing methods. New moment magnitude scale, evidence of stress drop magnitude scaling and stochastic ground motion model for the French West Indies. S-waves Fourier spectra are analysed to simultaneously determine source, path and site terms. The results show that the duration magnitude routinely estimated for the events that occurred in the region underestimate moment magnitude by 0. From the inverted seismic moments and corner frequencies, we compute Brune's stress drops. We show that stress drops increase with increasing magnitude. The same pattern is observed on apparent stresses i. However, the rate of increase diminishes at high magnitudes , which is consistent with a constant stress drop model for large events. Using the results of the inversions, we perform ground motion simulations for the entire data set using the SMSIM stochastic simulation tool. Although the magnitude -dependent stress drop model is giving better results than the constant stress drop model, the interevent variability remains high, which could suggest that stress drop depends on other parameters such as the depth of the hypocentre. In any case, the overall variability is of the same order of magnitude as usually observed in empirical ground motion prediction equations. This event is larger than previous one in terms of magnitude and showed that measured magnitude strongly depends on the frequency band of data. Relative spectral magnitude varies with frequencies and decreases as frequency increase. A methodology is presented for determining mb Pn magnitude of underground nuclear explosions from local Pn phase. The mb Pn estimates of regional events for Korean Peninsula are determined to be mb Pn? Systematic non-linearity does not observed at frequency band from 0. The magnitude of 6th event is mb Pn 6. Further research of applicable mb Pn magnitude scaling is required for all frequency band and. The bolometric, infrared and visual absolute magnitudes of Mira variables. Statistical parallaxes, as well as stars with individually known distances are used to derive bolometric and infrared absolute magnitudes of Mira Me variables. The derived bolometric magnitudes are in the mean about 0. The problem of determining the pulsation constant is discussed. Miras with periods greater than days probably pulsate in the first overtone. Those of shorter periods are anomalous and may be fundamental pulsators. It is shown that the absolute visual magnitudes at mean light of Miras with individually determined distances are consistent with values derived by Clayton and Feast from statistical parallaxes. Potencial del Agua del suelo. Full Text Available La energía potencial del agua presenta diferencias de un punto del suelo a otro; esas diferencias son las que originan el movimiento del agua de acuerdo a la tendencia universal de la materia en el sentido de moverse de donde la energía potencial es mayor a donde dicha energía es menor. En el suelo el agua en consecuencia se mueve hacia donde su energía decrece hasta lograr su estado de equilibrio. Se desprende entonces que la cantidad de energía potencial absoluta contenida en el agua, no es importante por sí misma, sino por su relación con la energía en diferentes lugares dentro del suelo. El concepto Potencial de agua del suelo es un criterio para esta energía. On the magnitude and recurence of Vrancea earthquakes. The moment- magnitude scale Msub W is proposed for the quantification of Vrancea earthquakes. The asperity model is found adequate to explain the observed quasi-cycles and super-cycles in the occurrence of large events. Disparities in the Magnitude of Human Immunodeficiency Virus HICs while tuberculosis, candidiasis, chronic diarrhea, and cryptococcosis were predominant Mohar A. Magnitude and factors associated with post-cesarean surgical site Magnitude and factors associated with post-cesarean surgical site infection at Hawassa University Teaching and referral hospital, southern Ethiopia: a Thus, it should be averted by implementing infection prevention techniques. Rapid earthquake magnitude determination for Vrancea early warning system. Due to the huge amount of recorded data, an automatic procedure was developed and used to test different methods to rapidly evaluate earthquake magnitude from the first seconds of the P wave. In order to test all the algorithms involved in detection and rapid earthquake magnitude estimation, several tests were performed, in order to avoid false alarms. A method to rapidly estimate magnitude in 4 seconds from detection of P wave in the epicenter is proposed. The method was tested on al recorded data, and the magnitude error determination is acceptable taking into account that it is computed from only 3 stations in a very short time interval. Tengo 22 años soy pasivo quisiera conocer chicos y hombres maduros activos o heteros curiosos para amistad y sexo. Depilacion rasurado masajes y mas. Chico nuevo ofrece servicios sexuales en el departamento. Templado 22cm. Char- les AflotL Susana Soler. Auro- ra A Betancourt. Bernardino Dommguez. Zunmda Santana. Marnme Gajcia. Felipe SitIa Cardenas. Philip Rosenbers. Eu- genio Soler Alonso. UMri, A Alonso. Saaerem hala t. La Habana. Moeaical: aoUla Brav. Elpidl SIuncer y Mrandels; vdo. Padre Bastarrica. Ernestina Garcia Lebredo aVd. LeSic sU e' ::e [ c z ":". Iavor que ogradeceran. Ln :Doba-. Josi Maria. Constantino y Joaquin farbajossa Mnendrn. Gloria rata de Carba. Apar- tamentc "F", tercer pisao, en 23 y M Vedado. 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Ei doctor Santiago Roig Gar- gcia, el renombrado especialista, Muy felices se muestran eniatendid a Il sefhora de Chediak est. L Enlace Telefono ceptL, o y. San cu l icoCiA Ej pr6ximo abbado, dia dieci. Para las side de la noche se - nuete, en la iglesia del Carme-. Rina Casadevall Sern, con iorita Casadevall tir precedida. Seria durante veinte dias El dia 16 comienzan Muy buenos dial, estlmados ue ustedes pasaron y han e ch SSalud, y el Padre San. A Cn que le mu ch s graacia y que D no n nde s: a quvanzada edad, y el Papa para los qudice cpresenan sia l. En usa reu nioin celebrad a par de rea. F cto, ue promoverI a propo rTotminc en erl o ni s valnl se nCt o de r p. Revolucionari r- a J a da re m c str to l e nH iiate dIaA d eno period a cicl, final de Is vi- tempo dicho, so mantienen hs l. MararMrnta Lo- is Mara D iaz. La aom srega bisa qu cinsto- vosaca n final modic6 el y del propio patron, para ir- Matanza. Sr Antonio Bechy o alenci6n a alas necesidades Gonzal c, sale a buscar los me- os an de oa idon que el dd ear a edad hd o sld us aoiasc resuliado de la ltolimo votacion p redar a competencia desleal". Cs enauegos Sr. Luts M ro. Gonzalez Prdyle, y le Pforma e r lamondo e en Ia cudad N eW Yrke dad t poder encauzar haca lo aporte sincro y roeal d la cn- ,absncin a "no u dEmcos v docentes del candieda n. Lane vueIs n 26r W dia 23 para ha. Y nt a mas delrpaE a c1tendrnas usi b Yv En una declara'cio n antes de avioan en que vaja Christian A caedra rup corresponde-1barque dc nnas paCO Or una f. L al e dn a d giltClaetoa. I- aide to un aqudnqinoteracty Pue iden iOadextra eartO o-pe. A Honta cnde r mLorOd. P A ocdente de Chicago qu dce to pasado. Nacn Unidas. LEn I e e a la terminal I 21iestas pasuntaenend n. Ramiro S anchez do selecciasn runica. Aldentoie se mosr6 vi- S e adm iran no s61a los titun An Ca ae-. Relos aodod. S do tod el tinadl o a delt ali cloedo 45 aSminut ticndol. Dwcht D. Menoam de 1a RaOatdo orariice ouan a8i da P3ttara na. La"e-ud c nnncara de oaa c e- arosrboriz6suer d lyelo 1aStela. Lso N En una de]as"acn antesen do vin en qune vlal. Mrs Roy Alger-. F A l r'oespaia nterpoantari par. Aun dle. S o-n r. Buca v Amo cua cuantia sn fd a arbitraria. MnonCoa o Zbnea. Antoni o SegDi V Oquands. Giuneo n polls. MaIrlve rnI Va--an o I s ad. Co nrh. Pedro PeraC. L Alger. Is ha d Is mucharha do 0. O --GoioroF NaOl,. J be Aulores de C obs. Se dice uonuShadros erdnd o. Sa n r easoia y Part, do autor pa n l ulala mentode ts los u- ente do Ni.. L Omenlo. Quadros ha comeincado bn --Cala 1 m a. Lime ofrecerra a tns ataon Ia bter- o e"d S -A. C nidea t dimbln las oneiaduros. Antoi, P. G ofra n ca ls -oPoreunidad do ex aa. Nancy Torres. Vie- Ramos de Avila. Nora Macau de A de Fonseca. Garci, Ints Grca de Cabaiio. Elisa Vidaurrizaga. Angela Emilia Muooz de Aguilera, Yo- ax:to paia v. Ofehlia Rodriguez. Rosita M Torres de Forno. Elsa Sotelo. Matilde Monter de Garcia Remus. GOlda M. Joseina les. Ana Lilia Rodrigue. Gutirre de uintans. Ana Maria Coscullue- Guerra. Patria Flores de Diaz. Elena Ptrez Narbona. Elsa Pestla. L y 23, en el Vedado, desarro- de Goicoechea. Emilia Goicoe- ra H. I -l MartinezR rbzl1 Yo. Gloria Q. AcoodornE Tt O Ite. Martha Goe- -4 saeioritas Mercedes Zamorano,. Chary y Lotty Rangel. Caridad de Ia Cruz. Ledia Pimienta de Fuentes y las de Figueroa. Estrella Ptrez. Ana1 Alicia del Pico de Mufiiz. Alicia York. Rosy Rodriguesz Gaby Vives. Edna Ambioso de. Con ella. Ro- Losada. Catalina A. Gulirrez, Pilar del Hierro. Delia]Edelmira Cano de Mora. Amalia Valdds de del Pino, Ale-. Bertha del Pino de Alonso, Mag- -- eau mnrne D. Leiva de Roiz. AN I El rame de mano de Ia flancke' lievaria la etiqueta de "Milagros" 1 el afamado edin del Paseo del Prado y Col6n. A Funsirin de padrinos el padre de ella, seifor Arturn Chebau. Ia gentle sehora Rosmits Dirube viuda de Garcia Bango. A las once 7 media de la me- liana. Balboa y L6pez. La deenracs6n floral de la her- mosa basilica correri par cuenta de "La Dalia". Y serAn padrmnos. Pars ests bode luciri aquel sa- grado recinto lan galas de un de-. Colores oeC eld T a oroiwarmenze cominads. Con rerra- male. Fano cure cramisa- cocoa. Ha seflorita Hump Careas y Mar Verde, beige, rajo y rosa. A yue pdrne de st es er Patine de corduroy. En fron. Dulce Maria Mar. Pasianistas, en 1a Vibora, on 3 5 '. Avicultura Millones de pesos se pierden por fungus, Conciencia Agricola Noticiario Ganadero Mundial hongos, insects, roedores y mala semnilla I o i PrO plSOres de la avicultura que Un punto que debe de resol- ta con granos almacenados le Docinas de miles de guajiros y ,t. Los gorgojos en el Costo del muelle La produccJon de car 9ende sotitut. El doctor Per Miguel geaabad Frsoas 40 adts m dos. Lt e del erebsagno dr. H ay qu t vigilar Is pure s; B runer, prepare hace aclos an do- 40,9W0, e ttadas Um i doC- btene d cl cue roe b o gu, eo g6t Nel ao ae producasn almentos par aves. Hay una cantldad enor- mania OccidentaL h1. Bo; Alt-'di 21 prentZ Qu si. En Sanldad Vegetal hay menic las mercancias imports- que, por su salud o edad, no 5. Tuvieron el aclero de co L funos. Pars a Imentator a esos nectrse con genies que lenin sectos y unsa eni oe eme an- agrico en o mca ,os e e ao no d acen coca. D Ee lGo bies o a poracioest ha sun- 80 os ie dtnts obricans dee aot po. En lo que se refiere a los datos antropométricos, los grupos control e intervención fueron homogéneos. La mediana fue de 90,7 Kg. En cuanto a la circunferencia de la cintura, en la comparación intragrupos, antes y después de la intervención, no se observaron alteraciones estadísticamente significativas. En la tabla 4, se presentan los resultados de la comparación intergrupos después de la intervención. Este ensayo controlado aleatorizado evaluó el efecto del monitoreo remoto de enfermería de mujeres con sobrepeso constatando beneficios en la mejora de las medidas antropométricas y ofrece evidencias para la utilización de esta herramienta terapéutica en el cuidado en salud y enfermería. Las condiciones de desigualdad social exigen enfoques sensibles del equipo de salud, en el sentido de comprender las dificultades de cada persona y adecuar las orientaciones a las mismas. Sin embargo, la mayoría realizaba el trabajo doméstico, confiriendo a ellas el nivel de actividad física activo o muy activo en el domicilio. Este panorama es preocupante, pues la actividad física regular por lo menos minutos por semana es uno de los pilares del tratamiento para reducción del peso El porcentaje de mujeres con obesidad fue superior al de sobrepeso y todas estaban con la circunferencia de la cintura aumentada representando un grupo poblacional con alto riesgo de morbimortalidad. Los datos del presente estudio mostraron que el monitoreo remoto de enfermería fue efectivo una vez que las medidas antropométricas de las mujeres del grupo intervención presentaron reducción con significancia estadística en comparación con el grupo control. Sin embargo, se destaca que el uso de estas tecnologías también logró resultados favorables en la pérdida de peso Se identificó sólo un estudio de intervención educativa que empleó encuentros presenciales y la tecnología del telemonitoreo. En este sentido, el monitoreo remoto es una de las herramientas terapéuticas efectivas para la educación en salud e incentivo al autocuidado. En cuanto a la obesidad, esta estrategia debe considerarse como una opción adicional al tratamiento convencional En condiciones crónicas de salud, a ejemplo de la insuficiencia cardíaca, del infarto agudo de miocardio, de las enfermedades respiratorias y renales crónicas, se ha demostrado que el telemonitoreo proporciona efectos benéficos. Estos beneficios generalmente se refieren al empoderamiento de los usuarios para desempeñar un papel activo en el propio cuidado de la salud, la influencia en sus actitudes y comportamientos y en la mejora de las condiciones clínicas Los resultados de esta investigación pueden contribuir con una visión innovadora para los profesionales de la salud, especialmente de enfermería, que trabajan con personas con sobrepeso. Por lo tanto, se sugiere la evaluación del efecto del monitoreo remoto de enfermería con mujeres con sobrepeso con mayor tiempo de seguimiento. Los resultados demostraron que el monitoreo remoto presentó un efecto benéfico en cuanto a la reducción de las medidas antropométricas de las mujeres del grupo de intervención en comparación con el grupo control. Pharmacol Econ. Rusia Ucrania. Guerra , Acción , Drama , Romance. Chapitel FILM..

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