987 resultados para Clemente Quaglio
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El objeto de este proyecto es definir las obras e instalaciones necesarias para depurar las aguas residuales de la localidad de San Clemente (Cuenca) hasta los límites de la Legislación vigente, y su posterior vertido al cauce del río Rus.
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Próximo a cumplirse el primer aniversario del fallecimiento de Clemente Saénz Ridruejo, el pasado 14 de febrero de 2007 se celebró en la sede de la Real Academia de Bellas Artes un emotivo homenaje a quien había sido maestro de ingenieros a lo largo de una vida en la que la práctica profesional, intensamente ejercida había sido complementada con singular brillantez por otras actividades que hicieron de Clemente un personaje excepcional.
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Segunda obra con port. propia, en p. 133
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Sign. : A-I 8
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Sign.: A-C4
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Sign. : [ ]2, *4
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Los tres textos están fechados al final en 1732
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Plancha de acero
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Segundo imp. tomado de colofón
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Texto dado en Valencia el día 19 de enero de 1726
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Sign.: A12
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Apéndices en español
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The chemical and mineralogical composition of pelagic sediments from the East Pacific Ocean has been determined with the aim of defining the ultimate sources and the mechanisms of formation of the solid phases. The distribution of elements between sea-water, the pore solution and the various solid components of the sediments permits interpretations of the variations in time and space of the gross chemical composition of pelagic clays. For example, manganese, present in sea-water in a divalent form, is apparently oxidized at the sediment-water interface to tetravalent species which subsequently become a part of the group of ferromanganese oxide minerals which are found in the marine environment. It is suggested the rate of manganese accumulation in sediments is some function of the length of time the sediment surface is in contact with sea-water. The contribution of chemical species from the different geospheres is considered. The quantitative importance of pelagic clays in the major sedimentary cycle is studied on the basis of the distribution of the weathered igneous rock products between continental and pelagic deposits and sea-water. These analyses of a wide variety of pelagic clays allow a reformulation of the geochemical balance and it is concluded that pelagic clays account for approximately 13 per cent of the total mass of sediments produced over geologic time.