997 resultados para Guillermo II, 1056-1100.
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En una carta fechada en Buenos Aires en 1962, Guillermo de Torre invita a Max Aub, exiliado en México, a formar parte de un proyecto editorial, una serie titulada 'El Puente' que haría de enlace entre autores españoles del exilio y del interior disidentes, en torno a temas hispánicos e hispanoamericanos, que sería editada por Sudamericana. Aunque el emprendimiento no carece de novedad, existe, diez años antes, un antecedente particularmente relevante ya que involucra a los mismos corresponsales, en una iniciativa coincidente en el empeño fundamental. Por medio de una carta fechada en México en 1952, era Aub quien escribía a De Torre participándolo de un proyecto de colección que bajo el nombre de ?Patria y Ausencia? agruparía a escritores españoles exiliados, cuya edición correría por cuenta del Fondo de Cultura Económica. La ponencia analiza la relación entre las dos colecciones, a partir de la lectura del diálogo epistolar entre Max Aub y Guillermo de Torre
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En una carta fechada en Buenos Aires en 1962, Guillermo de Torre invita a Max Aub, exiliado en México, a formar parte de un proyecto editorial, una serie titulada 'El Puente' que haría de enlace entre autores españoles del exilio y del interior disidentes, en torno a temas hispánicos e hispanoamericanos, que sería editada por Sudamericana. Aunque el emprendimiento no carece de novedad, existe, diez años antes, un antecedente particularmente relevante ya que involucra a los mismos corresponsales, en una iniciativa coincidente en el empeño fundamental. Por medio de una carta fechada en México en 1952, era Aub quien escribía a De Torre participándolo de un proyecto de colección que bajo el nombre de ?Patria y Ausencia? agruparía a escritores españoles exiliados, cuya edición correría por cuenta del Fondo de Cultura Económica. La ponencia analiza la relación entre las dos colecciones, a partir de la lectura del diálogo epistolar entre Max Aub y Guillermo de Torre
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Antonio Sánchez Barbudo y Guillermo de Torre mantuvieron durante 1937 una polémica en torno al arte y a la función social del intelectual y el artista. La misma se suscitó a partir de un artículo publicado por Guillermo de Torre en la revista Sur, que mereció la inmediata respuesta de Sánchez Barbudo en su condición de secretario de la revista Hora de España; y luego un segundo artículo del teórico de las vanguardias. La controversia, al igual que la que mantuvieron los artistas Ramón Gaya y José Renau, es ejemplar en tanto permite leer las condiciones de creación y el lugar del compromiso del artista e intelectual, durante los últimos momentos de la II República y en medio de la Guerra Civil. Este trabajo es parte de un artículo en curso que analiza el debate entre destacados intelectuales en la revista Sur, en donde se explicitan dos posiciones bien precisas y diferenciadas que trascienden el contexto del conflicto español.
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Tabla de contenidos: La Sociedad Rural Argentina : Masa societaria, composición e interés / Marta E. Valencia. La ocupación de la tierra en la frontera bonaerense : El caso de Chascomús 1779-1821 / Guillermo Banzato, Guillermo Quinteros. El caso de las fuentes judiciales en los estudios de historia rural / María Angélica Corva.
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Introduction: Chemical composition of water determines its physical properties and character of processes proceeding in it: freezing temperature, volume of evaporation, density, color, transparency, filtration capacity, etc. Presence of chemical elements in water solution confers waters special physical properties exerting significant influence on their circulation, creates necessary conditions for development and inhabitance of flora and fauna, and imparts to the ocean waters some chemical features that radically differ them from the land waters (Alekin & Liakhin, 1984). Hydrochemical information helps to determine elements of water circulation, convection depth, makes it easier to distinguish water masses and gives additional knowledge of climatic variability of ocean conditions. Hydrochemical information is a necessary part of biological research. Water chemical composition can be the governing characteristics determining possibility and limits of use of marine objects, both stationary and moving in sea water. Subject of investigation of hydrochemistry is study of dynamics of chemical composition, i.e. processes of its formation and hydrochemical conditions of water bodies (Alekin & Liakhin 1984). The hydrochemical processes in the Arctic Ocean are the least known. Some information on these processes can be obtained in odd publications. A generalizing study of hydrochemical conditions in the Arctic Ocean based on expeditions conducted in the years 1948-1975 has been carried out by Rusanov et al. (1979). The "Atlas of the World Ocean: the Arctic Ocean" contains a special section "Hydrochemistry" (Gorshkov, 1980). Typical vertical profiles, transects and maps for different depths - 0, 100, 300, 500, 1000, 2000, 3000 m are given in this section for the following parameters: dissolved oxygen, phosphate, silicate, pH and alkaline-chlorine coefficient. The maps were constructed using the data of expeditions conducted in the years 1948-1975. The illustrations reflect main features of distribution of the hydrochemical elements for multi-year period and represent a static image of hydrochemical conditions. Distribution of the hydrochemical elements on the ocean surface is given for two seasons - winter and summer, for the other depths are given mean annual fields. Aim of the present Atlas is description of hydrochemical conditions in the Arctic Ocean on the basis of a greater body of hydrochemical information for the years 1948-2000 and using the up-to-date methods of analysis and electronic forms of presentation of hydrochemical information. The most wide-spread characteristics determined in water samples were used as hydrochemical indices. They are: dissolved oxygen, phosphate, silicate, pH, total alkalinity, nitrite and nitrate. An important characteristics of water salt composition - "salinity" has been considered in the Oceanographic Atlas of the Arctic Ocean (1997, 1998). Presentation of the hydrochemical characteristics in this Hydrochemical Atlas is wider if compared with that of the former Atlas (Gorshkov, 1980). Maps of climatic distribution of the hydrochemical elements were constructed for all the standard depths, and seasonal variability of the hydrochemical parameters is given not only for the surface, but also for the underlying standard depths up to 400 m and including. Statistical characteristics of the hydrochemical elements are given for the first time. Detailed accuracy estimates of initial data and map construction are also given in the Atlas. Calculated values of mean-root deviations, maximum and minimum values of the parameters demonstrate limits of their variability for the analyzed period of observations. Therefore, not only investigations of chemical statics are summarized in the Atlas, but also some elements of chemical dynamics are demonstrated. Digital arrays of the hydrochemical elements obtained in nodes of a regular grid are the new form of characteristics presentation in the Atlas. It should be mentioned that the same grid and the same boxes were used in the Atlas, as those that had been used by creation of the US-Russian climatic Oceanographic Atlas. It allows to combine hydrochemical and oceanographic information of these Atlases. The first block of the digital arrays contains climatic characteristics calculated using direct observational data. These climatic characteristics were not calculated in the regions without observations, and the information arrays for these regions have gaps. The other block of climatic information in a gridded form was obtained with the help of objective analysis of observational data. Procedure of the objective analysis allowed us to obtain climatic estimates of the hydrochemical characteristics for the whole water area of the Arctic Ocean including the regions not covered by observations. Data of the objective analysis can be widely used, in particular, in hydrobiological investigations and in modeling of hydrochemical conditions of the Arctic Ocean. Array of initial measurements is a separate block. It includes all the available materials of hydrochemical observations in the form, as they were presented in different sources. While keeping in mind that this array contains some amount of perverted information, the authors of the Atlas assumed it necessary to store this information in its primary form. Methods of data quality control can be developed in future in the process of hydrochemical information accumulation. It can be supposed that attitude can vary in future to the data that were rejected according to the procedure accepted in the Atlas. The hydrochemical Atlas of the Arctic Ocean is the first specialized and electronic generalization of hydrochemical observations in the Arctic Ocean and finishes the program of joint efforts of Russian and US specialists in preparation of a number of atlases for the Arctic. The published Oceanographic Atlas (1997, 1998), Atlas of Arctic Meteorology and Climate (2000), Ice Atlas of the Arctic Ocean prepared for publication and Hydrochemical Atlas of the Arctic Ocean represent a united series of fundamental generalizations of empirical knowledge of Arctic Ocean nature at climatic level. The Hydrochemical Atlas of the Arctic Ocean was elaborated in the result of joint efforts of the SRC of the RF AARI and IARC. Dr. Ye. Nikiforov was scientific supervisor of the Atlas, Dr. R. Colony was manager on behalf of the USA and Dr. L. Timokhov - on behalf of Russia.
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We present Submillimeter Array [C II] 158 μm and Karl G. Jansky Very Large Array 12^CO(1-0) line emission maps for the bright, lensed, submillimeter source at z = 5.2430 behind A 773: HLSJ091828.6+514223 (HLS0918). We combine these measurements with previously reported line profiles, including multiple 12^CO rotational transitions, [C I], water, and [N II], providing some of the best constraints on the properties of the interstellar medium in a galaxy at z > 5. HLS0918 has a total far-infrared (FIR) luminosity L_FIR(8–1000 μm) = (1.6 ± 0.1) × 10^14 L_☉ μ^–1, where the total magnification μ_total = 8.9 ± 1.9, via a new lens model from the [C II] and continuum maps. Despite a HyLIRG luminosity, the FIR continuum shape resembles that of a local LIRG. We simultaneously fit all of the observed spectral line profiles, finding four components that correspond cleanly to discrete spatial structures identified in the maps. The two most redshifted spectral components occupy the nucleus of a massive galaxy, with a source-plane separation <1 kpc. The reddest dominates the continuum map (demagnified L_FIR, component = (1.1 ± 0.2) × 10^13 L_☉) and excites strong water emission in both nuclear components via a powerful FIR radiation field from the intense star formation. A third star-forming component is most likely a region of a merging companion (ΔV ~ 500 km s^–1) exhibiting generally similar gas properties. The bluest component originates from a spatially distinct region and photodissociation region analysis suggests that it is lower density, cooler, and forming stars less vigorously than the other components. Strikingly, it has very strong [N II] emission, which may suggest an ionized, molecular outflow. This comprehensive view of gas properties and morphology in HLS0918 previews the science possible for a large sample of high-redshift galaxies once ALMA attains full sensitivity.
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Includes index.
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CCBE s. XVI
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Mode of access: Internet.
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Mercury (II)measurementswereperformedthankstoanewlydevelopedelectrochemicalmethodusinga disposablegoldmodified screenprintedcarbonelectrode.Themethodhasawidedynamicrange(1–100 mg/L), agoodaccuracyandalimitofdetectionincompliancewithWHOstandards.Theapplicationofthe methodtoseveralgroundwatersamplesmadeitpossibletoidentify,forthe first time,mercurycontent higherthantherecommendedWHOstandardvalueinagoldminingactivityareainthenorthern partofBurkinaFaso.TheaccuracyoftheassaywascheckedbyICP/MS.
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La obra que se entrega hoy es un gran ejemplo de la riqueza académica con la que todos cuentan en Iberoamérica, motor de una nueva integración, que mueve y motiva por encima de intereses políticos y partidarios. Para una mejor lectura de las evoluciones y las expectativas en derecho público en Iberoamérica, así como del balance del derecho administrativo colombiano, en sus primeros cien años de justicia contencioso-administrativa, en este orden de ideas se ha dividido la publicación en dos tomos. El primero de ellos se divide en tres partes: derecho constitucional, teoría general del derecho administrativo, y acto y procedimiento administrativo. El segundo tomo viene distribuido en cinco partes: la primera parte se ha denominado contratos administrativos, la segunda parte régimen local, la tercera parte, denominada bienes del Estado, la cuarta parte, contencioso-administrativo y la última parte, se ha descrito como temas varios. En ella se encuentran reflexiones sobre la evolución de la teoría del daño especial en Colombia. Con lo anterior, se espera haber cumplido con un buen balance bicentenario del derecho público en Iberoamérica y del derecho administrativo colombiano en estos cien primeros años de justicia contencioso-administrativa, en homenaje al maestro Jaime Vidal Perdomo, eximio jurista colombiano consagrado al estudio y análisis del derecho público y exponente calificado y reconocido de la academia en Colombia y en los países iberoamericanos.