Hydrochemical evolution and environmental features of Salso River catchment, central Sicily (Italy)

6533b824fe1ef96bd1281268

RESEARCH PRODUCT

Hydrochemical evolution and environmental features of Salso River catchment, central Sicily (Italy)

Mariano Valenza Rocco Favara F. Grassa

subject

Hydrology Pollution geography geography.geographical_feature_category media_common.quotation_subject General Engineering Drainage basin Structural basin Water balance Facies Earth and Planetary Sciences (miscellaneous)General Earth and Planetary Sciences Environmental Chemistry Environmental science Water quality Surface water Groundwater General Environmental Science Water Science and Technology media_common

description

A hydrogeochemical study of the Salso River highlighted the chemical and isotopic space-time evolution along its flow path and the main contamination processes. Within the basin, three different hydrogeochemical facies have been individuated: (1) Ca-Mg-HCO3, (2) Ca-Mg-SO4 and (3) Na-Cl. The first facies reflects the chemical composition of the groundwaters hosted in the carbonate reliefs that belong to the Madonie Mountains. The second and the third facies are the result of the interaction processes between surface waters and the gypsum and salty clays, respectively. Two pollution sources have been also located in the basin downstream from the salt mine and downstream from a discharge area of wastewater from the town of Gangi. On the basis of the location of natural and anthropogenic pollution sources, the waters available for drinking and irrigation use are also indicated.

year	journal	country	edition	language
2000-10-13	Environmental Geology

https://doi.org/10.1007/s002540000116

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