Caracterización hidrogeológica de las salinas de Saelices de la Sal (Guadalajara, España)
The salt evaporation ponds in Saelices are a site of Cultural and Ecological Interest Site inside the Alto Tajo Natural Park. Time ago the salty groundwater was pumped out from two wells. It has been proved that this salinity is due to the discharge of groundwater from Keuper facies. This salty wate...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2013 |
| 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:10272/8780 |
| Acceso en línea: | http://hdl.handle.net/10272/8780 |
| Access Level: | acceso abierto |
| Palabra clave: | Salt pond Groundwater Saelices Discharge zone Salina Agua subterránea Zona de descarga |
| Sumario: | The salt evaporation ponds in Saelices are a site of Cultural and Ecological Interest Site inside the Alto Tajo Natural Park. Time ago the salty groundwater was pumped out from two wells. It has been proved that this salinity is due to the discharge of groundwater from Keuper facies. This salty water flows up into the alluvial sediments of the Arroyo de la Vega. It is a Na- Cl type water with a high electric conductivity (higher than 25 mS/cm). This salty water gets mixed with fresh water (coming from rain and from adjacent quaternary sediments) inside the alluvial sediments and flows into the Arroyo de la Vega channel |
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