Ground water regimes containing country rock minerals in Southern Kuzbass (case study: Narysk-Ostashkin)

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

Domrocheva, E.^1 ; Lepokurova, O.^2

A.A. Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, RAS, Tomsk, Russia^1

National Research Tomsk Polytechnic University, Tomsk, Russia^2

关键词: Aluminosilicate minerals;    Calculation results;    Groundwater composition;    Kuzbass;    Non equilibrium;    Water regime;   

Others  :  https://iopscience.iop.org/article/10.1088/1755-1315/33/1/012003/pdf
DOI  :  10.1088/1755-1315/33/1/012003

来源: IOP

【 摘 要 】

The paper describes the calculation results revealing groundwater in equilibrium to carbonates and aluminosilicate minerals of country rocks in Narysk-Ostashkinsk area. It was proved that groundwater is in nonequilibrium to primary (endogenous) minerals in which they dissolve, however are in equilibrium to clays and carbonates which precipitate in the groundwater. The groundwater composition varies.