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Explotación hidrogeológica en la cuenca del Río Miraflores Pcia. de Jujuy. Argentina.
Tipo de material:
ArtículoIdioma: Español; Castellano Tema(s): Género/Forma:
En: Revista del Instituto de Geología y Minería no.6, p.211-255Resumen: An unconfined aquifer has been developed in flood sediments of Miraflores River vasin in the Abra Pampa graben (Jujuy province: 22º 15' - 23º 17' lat. south; 65º 32'- 66º 15'long. West). Its hydraulc characterists have been determined through two mechanical sounding which had shown a base of a white cemented, compacted sandstone at 35 meters of depth (mensured in de middle of de valley). -It was found that the volumen "Q" varies from 900 to 1600m3 day, with a depression lower than 13(tanto/ciento) The coefficient of transmisibility goes from 600 to 2500 m2 / day with a quick recuperation and ono excellent qualitu water.
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Artículo
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Biblioteca Instituto de Geología y Mineria "Ing. Carlos F. Stubbe" | Revista del Instituto de Geología y Minería, no.6 (Navegar estantería(Abre debajo)) | Disponible |
Relevamiento: 1986.
An unconfined aquifer has been developed in flood sediments of Miraflores River vasin in the Abra Pampa graben (Jujuy province: 22º 15' - 23º 17' lat. south; 65º 32'- 66º 15'long. West). Its hydraulc characterists have been determined through two mechanical sounding which had shown a base of a white cemented, compacted sandstone at 35 meters of depth (mensured in de middle of de valley). -It was found that the volumen "Q" varies from 900 to 1600m3 day, with a depression lower than 13(tanto/ciento) The coefficient of transmisibility goes from 600 to 2500 m2 / day with a quick recuperation and ono excellent qualitu water.
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