Hidrogeoquímica y microbiología en los Hervideros del Campo de Calatrava (Ciudad Real).

• Autores: Javier G. Yélamos, Ramón Redondo Ortega, Fernando de Castro San Miguel, María Angeles Galván Tamame, Juan Martínez Rubio, Luis F. Rebollo Ferreiro, Pedro Ruano Magán, Agustín Senderos Domínguez, Fermín Villarroya Gil
• Localización: Geogaceta, ISSN 0213-683X, Nº. 26, 1999, págs. 115-118
• Idioma: español
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• Resumen

  • CÓZ-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 15years. The hydrochemical facies is miked-catipn bicarbonate and is related to the extinct yolcanism 6f the area. It is a possibility that not all the Hervideros are originated from volcapic 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