RT Journal Article
T1 Hidrogeoquímica y microbiología en Los Hervideros del Campo de Calatrava (Ciudad Real)
A1 Yélamos, Javier G.
A1 Redondo Ortega, Ramón
A1 Castro San Miguel, Fernando De
A1 Galván Tamame, Ángeles
A1 Martínez Rubio, Juan
A1 Rebollo Ferreiro, Luis F.
A1 Ruano Magán, Pedro
A1 Senderos Domínguez, Agustín Jesús
A1 Villarroya Gil, Fermín
AB 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
PB Sociedad Geológica de España
SN 0213-683X
YR 1999
FD 1999
LK https://hdl.handle.net/20.500.14352/112433
UL https://hdl.handle.net/20.500.14352/112433
LA spa
NO Yélamos, J.G. et al. (1999) «Hidrogeoquímica y microbiología en Los Hervideros del Campo de Calatrava (Ciudad Real).», Geogaceta, 26, pp. 115-118.
NO Comisión Interministerial de Ciencia y Tecnología (España)
DS Docta Complutense
RD 18 abr 2025