Sobre la hidroquímica de la cuenca del río Almanzora (Almería)
The waters of the Almanzora basin have very different chemistry according to the hydrogeological context; the mineralization is between 0,4 and more than 6 g/i; the hydrochemical facies is usually . calcic, bicarbonated in the carbonated aquifers, of lower salinity, and sulphated for the detritic aq...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1993 |
| 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:10272/14061 |
| Acceso en línea: | http://hdl.handle.net/10272/14061 |
| Access Level: | acceso abierto |
| Palabra clave: | Hydrochemistry Thermalism Almanzora basin |
| Sumario: | The waters of the Almanzora basin have very different chemistry according to the hydrogeological context; the mineralization is between 0,4 and more than 6 g/i; the hydrochemical facies is usually . calcic, bicarbonated in the carbonated aquifers, of lower salinity, and sulphated for the detritic aquifers and surface waters. Mild regional thermal ism also occurs with emergence temperatures usually ranging between 20 and 28º C |
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