CARACTERIZACION FISICOQUIMICA DE CUERPOS DE AGUA SUPERFICIAL Y SUBTERRANEA DE LA LOCALIDAD DE BELEN PITUTA "B", MUNICIPIO DE GUAQUI, BOLIVIA
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Rev. Bol. Quim
Abstract
La clasificación fisicoquímica de los tipos de agua superficial y subterránea estudiadas, según los diagramas Stiff y Piper-Hill-Langelier, es sulfatada-clorurada-cálcica, debido a las altas concentraciones de Ca2+, SO4(2-) y Cl-, predominantes entre los iones mayoritarios analizados. Se determinó la existencia de dos flujos de agua (diagramas de Superficie) en direcciones contrarias entre sí: uno subterráneo (prof.: 40 a 80m) de Sur-Oeste a Nor-Este y otro sub-superficial (prof.: 1 a 4m) de Sur-Este a Nor-Oeste, induciendo la existencia de dos acuíferos.
Stiff and Piper-Hill-Langelier diagrams give to us the classification of both superficial and groundwater resources as sulphated-chloride-calcic, due to the high concentration of Ca2+, SO4(2-) and Cl- among all the majorities ions. It was determine also the existence of two kind of water fluxes (according to Surfer diagrams) one direction from South-West to North-East (depth: 40-80m) and the other from South-East to North-West (depth: 1-4m), taking us to think on the existence of two aquifers inside our study area.
Stiff and Piper-Hill-Langelier diagrams give to us the classification of both superficial and groundwater resources as sulphated-chloride-calcic, due to the high concentration of Ca2+, SO4(2-) and Cl- among all the majorities ions. It was determine also the existence of two kind of water fluxes (according to Surfer diagrams) one direction from South-West to North-East (depth: 40-80m) and the other from South-East to North-West (depth: 1-4m), taking us to think on the existence of two aquifers inside our study area.
Description
Vol. 23, No. 1