Caracterización hidrogeológica de la Sierra de la Horna (Alicante)
In this paper we present the preliminary results ofthe'study of Sierra de Horna aquifer. There is a conection between Horna aquifer and the detritical aquifer of Rambla del Tarafa deduced from the piezometric data: The hydrochemistry results have shown .that most saline waters lie in the de...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1999 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9925 |
| Acceso en línea: | http://hdl.handle.net/10272/9925 |
| Access Level: | acceso abierto |
| Palabra clave: | Karstic aquifer Hydrogeochemistry Vertical zonation Horna Alicante |
| Sumario: | In this paper we present the preliminary results ofthe'study of Sierra de Horna aquifer. There is a conection between Horna aquifer and the detritical aquifer of Rambla del Tarafa deduced from the piezometric data: The hydrochemistry results have shown .that most saline waters lie in the deepest parts of the aquifer, while those of lowest mineralization occupy the area of the saturated zone closest to the surface |
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