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

  1. Yélamos, Javier G.
  2. Redondo Ortega, Ramón
  3. Castro San Miguel, Fernando de
  4. Galván Tamame, María Angeles
  5. Martínez Rubio, Juan
  6. Rebollo Ferreiro, Luis F.
  7. Ruano Magán, Pedro
  8. Senderos Domínguez, Agustín
  9. Villarroya Gil, Fermín
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1999

Número: 26

Páginas: 115-118

Tipo: Artículo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

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

Fuente de los datos: Dialnet