Role of water-rock interactions in the formation of the composition of radon waters of the Zaeltsovsky field (the southern part of West Siberia)

D. A. Novikov, F. F. Dultsev, A. V. Chernykh

Research output: Contribution to journalConference articlepeer-review

3 Citations (Scopus)

Abstract

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.

Original languageEnglish
Article number012007
JournalJournal of Physics: Conference Series
Volume1451
Issue number1
DOIs
Publication statusPublished - 9 Sep 2020
Event2nd International Conference on Applied Physics, Power and Material Science, ICAPPM 2019 - Secunderabad, Telangana, India
Duration: 20 Dec 201921 Dec 2019

Keywords

  • equilibrium
  • hydrogeochemistry
  • Novosibirsk
  • radon waters
  • water-rock system
  • Western Siberia

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