Características hidroquímicas de las aguas termominerales de los Baños de Alhama de Murcia (Murcia)
The Baños de Alhama de Murcia waters are calcium-sodium-magnesium sulfhate types and have a high temperature (44-45 °C) and conductivity (3.800-4.000mhosfcm); with cluster and factorial analysis of variables the study is complemented. The fluoride, boron and lithium ions have a high concentration an...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1992 |
| 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:10272/16324 |
| Acceso en línea: | http://hdl.handle.net/10272/16324 |
| Access Level: | acceso abierto |
| Palabra clave: | Hydrogeochemistry Termomineral waters Cluster and factorial analysis Neotectonic |
| Sumario: | The Baños de Alhama de Murcia waters are calcium-sodium-magnesium sulfhate types and have a high temperature (44-45 °C) and conductivity (3.800-4.000mhosfcm); with cluster and factorial analysis of variables the study is complemented. The fluoride, boron and lithium ions have a high concentration and the base temperatures range from 66 and 245 centlgrades. The tempera¬ture and chemical composition of the water shows a thermic anomaly directly related with the tec¬tonic activity in the area |
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