RT Journal Article
T1 Modelización hidrogeoquímica del agua de infiltración en la Cueva de Nerja (Málaga)
T1 Hydrogeochemical modeling of the drip water in the Nerja cave (Málaga)
A1 Cardenal Escarcena, J.
A1 Benavente Herrera, José
A1 Andreo Navarro, Bartolomé
A1 Carrasco Cantos, Francisco
AB A hydrochemical study of the drip water in the Nerja Cave has been carried out using geochemical modeling. Results indicate that major ions in the infiltration water are meteoric in origin (évapotranspiration of rain water plus equilibrium with a soil Pc02 of TO 25 atm) but sequential dissolution of calcite and dolomite also occurs in an open system to C02. Moreover, because the low discharge rate of the drip water points, this water maintains long contact with the cave atmosphere before enough volume can be sampled for a complete analysis. Thus measured pH are strongly affected, so modeled pH are lower (even 0.3-0.6 pH-units) than those measured ones
PB Sociedad Geológica de España
YR 1998
FD 1998
LK http://hdl.handle.net/10272/10185
UL http://hdl.handle.net/10272/10185
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026