@article{10272/9878,
year = {1999},
url = {http://hdl.handle.net/10272/9878},
abstract = {Conventional and isotopic hydrogeochemical techniques have been applied to a study of CO2-rich waters in the northeast of Catalonia. Two hydrogeochemical facies, a calcium-bicarbonate and another sodium-bicarbonate are clearly distinguished. The second one seems to be the result of evolution from the calcium facies. The tritium-ages support the previous division in two hydrogeochemical facies. Measurements of ,sO and deuterium ratio indicate that the carbonic waters have a meteoric origin. The i3C/12C ratio varied from -5,0 to -0,64 6°/œ showing a deep origin of CO},
publisher = {Sociedad Geológica de España},
keywords = {Ground water},
keywords = {CO2-rich waters},
keywords = {Hydrogeochemistry},
keywords = {Environmental isotopes},
keywords = {Catalonia},
title = {Hidrogeoquímica convencional e isotópica de las aguas carbónicas de Cataluña},
title = {Conventional and isotopic hydrogeochemistry of CO2-rich waters of Catalonia},
author = {Redondo, R. and Yélamos, J. G.},
}