Chemical elements migration in water-travertin system (Tomsk region, Russia)

Research output: Contribution to journalConference article

Abstract

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.

Original languageEnglish
Article number07014
JournalE3S Web of Conferences
Volume98
DOIs
Publication statusPublished - 7 Jun 2019
Event16th International Symposium on Water-Rock Interaction, WRI 2019 and 13th International Symposium on Applied Isotope Geochemistry, 1st IAGC International Conference - Tomsk, Russian Federation
Duration: 21 Jul 201926 Jul 2019

Fingerprint

chemical element
Chemical elements
Water
travertine
water
Carbonates
Rocks
carbonate
rock

ASJC Scopus subject areas

  • Environmental Science(all)
  • Energy(all)
  • Earth and Planetary Sciences(all)

Cite this

Chemical elements migration in water-travertin system (Tomsk region, Russia). / Lepokurova, Olesya.

In: E3S Web of Conferences, Vol. 98, 07014, 07.06.2019.

Research output: Contribution to journalConference article

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