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.
|Journal||IOP Conference Series: Earth and Environmental Science|
|Publication status||Published - 15 Apr 2016|
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)