4 resultados para Alumbrado eléctrico

em Universitat de Girona, Spain


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La Encuesta de Infraestructura y Equipamientos Locales (EIEL) es un inventario periódico demandado por el Ministerio de Política Territorial (MPT) español a las Diputaciones Provinciales. El objetivo inicial de la EIEL es el análisis y valoración de las necesidades de las entidades locales en cuanto a dotaciones de infraestructuras y equipamientos se refiere. La EIEL recoge un amplio rango de información territorial que se agrupa en torno a varios bloques: red viaria, abastecimiento de agua, saneamiento, servicio de recogida y tratamiento de residuos, alumbrado, acceso a redes de telecomunicaciones, equipamientos y planes de ordenación urbanística

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Increase of the metropolitan area of cities provoking a progressive settlement of zones that previously had a different territorial use. These zones are usually located within city houndaries and for many years have been affected hy the waste of many kinds of residues. Qualitative analysis of the electrical behaviour of soil, based on maps and cross sections of apparent conductivity, allows us to locate anomalies generated by the wastes. Moreover, the electrornagnetic techniques (EM-31 and EM-34 Geonics devices) are cheaper than other survey methods. Two examples in the campus of the University of Girona, in the southern area of Girona city, illustrate the environmental problem and the applicability of the geophysical method

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The geometry of Riera de Tossa (Costa Brava, Catalonia) Pleistocene paleovalley has been studied by two geophysical prospecting methods: vertical electric sounding (VES-DC) and seismic refraction. The results show the existence of a sudden slope change of the thalweg that permits to differentiate two sections where erosion processes operated in unequal intensity. Based on geological and geomorphological available data, it can be inferred that this slope rupture is caused by the litological control imposed by the alineation of resistant materials, which limited the headward erosion extend of the creek during the Upper Pleistocene