Consideraciones sobre el contenido isotópico de las aguas subterráneas en el Bajo Andarax (Almería)
The isotopic content of the groundwaters of the Lower Andarax was used as the basis for differentiating two subterranean flow systems. The more superficial system is represented by less impoverished waters with temperatures of less than 24 °C. The deeper system corresponds to lighter waters and temp...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2001 |
| 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:10272/9461 |
| Acceso en línea: | http://hdl.handle.net/10272/9461 |
| Access Level: | acceso abierto |
| Palabra clave: | Geothermal waters Oxygen-18 Deuterium |
| Sumario: | The isotopic content of the groundwaters of the Lower Andarax was used as the basis for differentiating two subterranean flow systems. The more superficial system is represented by less impoverished waters with temperatures of less than 24 °C. The deeper system corresponds to lighter waters and temperatures exceeding 24.5 °C. Using these data one can consider the hydraulic connection between the carbonate aquifer and the deep aquifer, and the possible recharge at depth between the carbonate and detritic aquifers in the Cádor area |
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