Hidrogeoquímica y microbiología en Los Hervideros del Campo de Calatrava (Ciudad Real)
CO2-rich springs and wells in the Campo de Calatrava commonly are named Hervideros. This ground water is originated by deep circulation along the fractures of the paleozoic rocks of the area, with residence times longer than 15 years. The hydrochemical facies is mixed-cation bicarbonate and is relat...
| Autores: | , , , , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1999 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/112433 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/112433 |
| Access Level: | acceso abierto |
| Palabra clave: | 556+550.4(460.287) 579 CO2-rich water Hydrogeochemistry Groundwater microbiology Campo de Calatrava Hidrología Geoquímica Microbiología (Biología) 2508 Hidrología 2503 Geoquímica |
| Sumario: | CO2-rich springs and wells in the Campo de Calatrava commonly are named Hervideros. This ground water is originated by deep circulation along the fractures of the paleozoic rocks of the area, with residence times longer than 15 years. The hydrochemical facies is mixed-cation bicarbonate and is related to the extinct volcanism of the area. It is a possibility that not all the Hervideros are originated from volcanic or magmatic C02. Bacterial evaluation indicates high values, but probably it is representative of the biomass presence in the proper sampling point instead of the groundwater-microbiology |
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