Geochemistry of Soda-Type Groundwater in the Torey Lakes Region (Russia): Differences between Catchment Area and Beyond; NSG2020 26th European Meeting of Environmental and Engineering Geophysics

Detalhes bibliográficos
Parent link:NSG2020 26th European Meeting of Environmental and Engineering Geophysics.— 2020.— [5 p.]
Autor principal: Drebot V. V. Valeriya Vitaljevna
Autor Corporativo: Национальный исследовательский Томский политехнический университет Инженерная школа природных ресурсов Отделение геологии
Resumo:Title screen
Chemical groundwater composition analyses in the Torey Lakes case study area allowed identification of the difference between the chemical composition of groundwaters in the Torey Lakes catchment area and groundwaters beyond. Waters differed with respect to TDS content, pH, sodium, sulfate ion and chloride ion. The thermodynamic equilibrium of waters with calcite was calculated and analyzed. The study showed that the chemical composition formation of Na-HCO₃ (soda) waters in the area of the Torey lakes is due to a combination of factors: climatological conditions, hydrogeological conditions (catchment area and type of circulation) and time of interaction in the water-rock system.
Idioma:inglês
Publicado em: 2020
Assuntos:
Acesso em linha:https://doi.org/10.3997/2214-4609.202020025
Formato: Recurso Electrónico Capítulo de Livro
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=665626
Descrição
Resumo:Title screen
Chemical groundwater composition analyses in the Torey Lakes case study area allowed identification of the difference between the chemical composition of groundwaters in the Torey Lakes catchment area and groundwaters beyond. Waters differed with respect to TDS content, pH, sodium, sulfate ion and chloride ion. The thermodynamic equilibrium of waters with calcite was calculated and analyzed. The study showed that the chemical composition formation of Na-HCO₃ (soda) waters in the area of the Torey lakes is due to a combination of factors: climatological conditions, hydrogeological conditions (catchment area and type of circulation) and time of interaction in the water-rock system.
DOI:10.3997/2214-4609.202020025