Consideraciones sobre la hidroquímica de las aguas termales de «los Baños de Sierra Elvira» (Granada)
The principal physico-chemical characteristics of thermomineral waters of Banos de Sierra Elvira are studied (Middle Subbetic, Granada). The waters are calcium-sulphate type, with salinity around 2,5 g/ I and temperature of 32 °C. By SOLMINEQ.88 program the thermodinamic equilibrium conditions in su...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1995 |
| 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:10272/13373 |
| Acceso en línea: | http://hdl.handle.net/10272/13373 |
| Access Level: | acceso abierto |
| Palabra clave: | Hydrochemistry Thermomineral waters Carbonatic aquifer |
| Sumario: | The principal physico-chemical characteristics of thermomineral waters of Banos de Sierra Elvira are studied (Middle Subbetic, Granada). The waters are calcium-sulphate type, with salinity around 2,5 g/ I and temperature of 32 °C. By SOLMINEQ.88 program the thermodinamic equilibrium conditions in surface are studied. The waters are saturated in most of mineral studied and have a base temperature of 63 °C (silica-quartz themometry). The results obtained show a long-term residence of waters, affected with mixing processes of shallow fresch-waters with low nitrate values |
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