@article{10272/8821,
year = {2004},
url = {http://hdl.handle.net/10272/8821},
abstract = {The Andarax river is characterized by the variability of its flow, which is dependent upon the rainfall regime
of the area. This work presents a study of the chemical composition of the surface waters of the Andarax
river over an annual cycle. It analyses the relationship between ground water and surface waters using a
hydrogeochemical methodology. The ground water-surface water interactions was found to be more intense
in two areas: the north of Almócita and north of Santa Fe. North of Almócita local discharges of good
quality water arise, which leads to the chemical stabilization of the surface water. In this stretch, electrical
conductivity, temperature and ion concentrations are constant, and lower than at adjacent sampling
points. At north of Santa Fe, in the mid-section of the river, a contrasting effect is observed with an
increase in salinity and seasonal variability. Concentrations of Cl- and SO4
2- become elevated, and there is
a marked increase in salinity – especially during low flow periods when the majority of the surface flow
derives from groundwater drainage},
publisher = {Sociedad Geológica de España},
keywords = {Ground water/surface water interactions},
keywords = {Hydrochemistry},
keywords = {Andarax},
title = {Aspectos hidrogeoquímicos sobre la relación aguas subterráneas-aguas superficiales en el río Andarax (Almería)},
title = {Hydrogeochemical aspects about the interaction groundwater-surface water in the Andarax river (Almería)},
author = {Sánchez Martos, Francisco and Pulido Bosch, Antonio and Vallejos, Ángela and Gisbert, Josep and Molina, Luis},
}