Hydrogeochemistry of thermal waters of the Baikal Rift, South-Eastern Tuva, Russia

Anastasia Shestakova, Natalia Guseva, Yulia Kopylova, Albina Khvaschevskaya, Kara Kys Arakchaa

Research output: Contribution to journalConference articlepeer-review

Abstract

The spa resort of the Ush-Beldir is located in the south-eastern part of the Tuva region, Russia in the zone of influence of the Baikal rift. The Ush-Beldir territory has about 10 thermal springs and 4 exploration wells used for treatment and prevention of diseases. Hydrological and hydrochemical features of the thermal groundwaters are considered. The studied waters are thermal (T=50-83°C), alkaline (pH=9.3-10), low mineralized (TDS<370 mg/L) Na- waters with a high content of SiO (up to 125 mg/L) and F (up to 14 mg/L). The correlation of F with SiO, , Cl, Na as well as the calculation of saturation indices of minerals, allows one plausible solute source for these thermal waters, viz. the dissolution of rock-forming aluminosilicates, most likely plagioclase, gabbro and/or amphiboles in shales.

Original languageEnglish
Article number07029
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

ASJC Scopus subject areas

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

Fingerprint Dive into the research topics of 'Hydrogeochemistry of thermal waters of the Baikal Rift, South-Eastern Tuva, Russia'. Together they form a unique fingerprint.

Cite this