Underground water in Sukhodol Bay area (South Primorye)

All-Russian Scientific Conference with International Participation on Contemporary Issues of Hydrogeology, Engineering Geology and Hydrogeoecology in Eurasia

Chelnokov, G.^1 ; Kolubaeva, Yu.^2

Far East Geological Institute, Far Eastern Branch, RAS, Vladivostok, Russia^1

Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, RAS, Tomsk Division, Tomsk, Russia^2

关键词: Aluminosilicate minerals;    Bay areas;    Groundwater composition;    Non equilibrium;    Water-bearing rocks;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/33/1/012001/pdf
DOI  :  10.1088/1755-1315/33/1/012001

来源: IOP

【 摘 要 】

The paper describes the specific chemical groundwater composition in Sukhodol Bay (eastern Ussuri Bay). The equilibrium between groundwater and carbonate-aluminosilicate minerals in water-bearing rocks was calculated. It was established that a fraction of the studied water was calcite saturated. However, dolomite and magnesium undersaturated groundwater is non-equilibrium with primary aluminosilicates.