Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование
Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia). / Novikov, D. A.; Dultsev, F. F.; Chernykh, A. V.
в: Journal of Physics: Conference Series, Том 1451, № 1, 012007, 09.09.2020.Результаты исследований: Научные публикации в периодических изданиях › статья по материалам конференции › Рецензирование
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TY - JOUR
T1 - Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia)
AU - Novikov, D. A.
AU - Dultsev, F. F.
AU - Chernykh, A. V.
PY - 2020/9/9
Y1 - 2020/9/9
N2 - Results of thermodynamic calculations of the interactions of radon waters from the Zaeltsovsky field with the minerals of host rocks are presented for the first time. It was established that waters under study are supersaturated with respect to calcite and siderite, and to a smaller extent with respect to magnesite and dolomite. No saturation of radon waters with respect to primary aluminosilicate minerals (albite, anortite, microcline, ferrosilite) is observed. The points are located in the fields of stability of clayey minerals (kaolinite, Ca- and Mg-montmorillonite, Fe-sepiolite), gibbsite and leptochlorite. In the evolution of the water-rock system, they correspond to the siallite type of interaction with rocks.
AB - Results of thermodynamic calculations of the interactions of radon waters from the Zaeltsovsky field with the minerals of host rocks are presented for the first time. It was established that waters under study are supersaturated with respect to calcite and siderite, and to a smaller extent with respect to magnesite and dolomite. No saturation of radon waters with respect to primary aluminosilicate minerals (albite, anortite, microcline, ferrosilite) is observed. The points are located in the fields of stability of clayey minerals (kaolinite, Ca- and Mg-montmorillonite, Fe-sepiolite), gibbsite and leptochlorite. In the evolution of the water-rock system, they correspond to the siallite type of interaction with rocks.
KW - equilibrium
KW - hydrogeochemistry
KW - Novosibirsk
KW - radon waters
KW - water-rock system
KW - Western Siberia
UR - http://www.scopus.com/inward/record.url?scp=85091736905&partnerID=8YFLogxK
U2 - 10.1088/1742-6596/1451/1/012007
DO - 10.1088/1742-6596/1451/1/012007
M3 - Conference article
AN - SCOPUS:85091736905
VL - 1451
JO - Journal of Physics: Conference Series
JF - Journal of Physics: Conference Series
SN - 1742-6588
IS - 1
M1 - 012007
T2 - 2nd International Conference on Applied Physics, Power and Material Science, ICAPPM 2019
Y2 - 20 December 2019 through 21 December 2019
ER -
ID: 25613652