Hydrochemical characterization of shallow groundwater from the Mesta River basin | Zendy

Tanya Vasileva | Zendy; Aglaida Toteva | Zendy

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Hydrochemical characterization of shallow groundwater from the Mesta River basin

Author(s) -

Tanya Vasileva,

Aglaida Toteva

Publication year - 2019

Publication title -

engineering geology and hydrogeology

Language(s) - English

Resource type - Journals

eISSN - 2738-6996

pISSN - 0204-7934

DOI - 10.52321/igh.33.1.15

Subject(s) - groundwater , geology , geochemistry , gneiss , precambrian , marl , drainage basin , hydrology (agriculture) , structural basin , metamorphic rock , geomorphology , geotechnical engineering , cartography , geography

Groundwater is a valuable natural resource and an important source of drinking and domestic water supply. There are two types of groundwater in the Mesta River Basin: HCO3- > Ca2++Mg2+ (1st type waters) and HCO3- SO42-> Cl-. The cations are arranged in the order: Ca2++Mg2+ > (Na++K+) or Ca2+ > (Na++K+) > Mg2+. Groundwater is very soft to moderately hard, fresh, with TDS content up to 0.5 g/l and chloride content below 10 mg/l.

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