E3S Web Conf.
Volume 98, 201916th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference)
|Number of page(s)||6|
|Section||Geochemistry of Natural Waters: From Atmospheric Precipitations to Deep Brines|
|Published online||07 June 2019|
Chemical elements migration in water-travertin system (Tomsk region, Russia)
Tomsk Branch of Trofimuk Institute of Petroleum-Gas Geology and Geophysics of SB RAS, 4, Academichesky Ave., Tomsk 634055, Russia
2 National Research Tomsk Polytechnic University, Lenin Avenue, 30, Tomsk 634050, Russia
* Corresponding author: LepokurovaOY@ipgg.sbras.ru
To assess the mobility of chemical elements in carbonate, formation processes have calculated the water migration coefficient -Kx and the geochemical mobility coefficient -Kn. The series of geochemical mobility were constructed. The elements that can be deposited and that can be accumulated in water have been distinguished. It is shown that anionic elements - Cl, S, Br, I, U, As, as well as elements such as Na, Mg, Mo, Zr well pass into solution from rocks and remain in the water. Elements such as Ca, Fe, Al, Mn, Si, Ba, Zn, Pb, Co, Hg, Ti, La, Ag, Sn, Cr are most fully deposited in travertines.
© The Authors, published by EDP Sciences, 2019
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