Estimación de parámetros hidrogeológicos en los acuíferos costeros del Bajo Guadalhorce (Málaga) mediante el análisis de la influencia de las mareas
By the use of continuous data recording on two points of the Bajo Guadalhorce coastal sector (Malaga province, southern Spain), located at 626 m and 985 m inland, it has been possible to verify a clear influence of tidal oscillations on the water table of the unconfined and the confined aquifers. Va...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 2016 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13560 |
| Acesso em linha: | http://hdl.handle.net/10272/13560 |
| Access Level: | acceso abierto |
| Palavra-chave: | Tidal influence Time lag Transmissivity Coastal aquifer Guadalhorce Influencia de marea Retraso de marea Transmisividad Acuífero costero |
| Resumo: | By the use of continuous data recording on two points of the Bajo Guadalhorce coastal sector (Malaga province, southern Spain), located at 626 m and 985 m inland, it has been possible to verify a clear influence of tidal oscillations on the water table of the unconfined and the confined aquifers. Various methods to estimate aquifer transmissivity have been applied. The results depends on the method and, more important, on the storage coefficient (S) values. After the calculations it is possible to confirm that the time lag and tidal efficiency factor methods give coherent results with previous data, although with the time lag method the transmissivity values are an order of magnitude higher |
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