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 language | English |
|---|---|
| Article number | 07029 |
| Journal | E3S Web of Conferences |
| Volume | 98 |
| DOIs | |
| Publication status | Published - 7 Jun 2019 |
| Event | 16th 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 2019 → 26 Jul 2019 |
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ASJC Scopus subject areas
- Environmental Science(all)
- Energy(all)
- Earth and Planetary Sciences(all)
Cite this
Hydrogeochemistry of thermal waters of the Baikal Rift, South-Eastern Tuva, Russia. / Shestakova, Anastasia; Guseva, Natalia; Kopylova, Yulia; Khvaschevskaya, Albina; Arakchaa, Kara Kys.
In: E3S Web of Conferences, Vol. 98, 07029, 07.06.2019.Research output: Contribution to journal › Conference article
}
TY - JOUR
T1 - Hydrogeochemistry of thermal waters of the Baikal Rift, South-Eastern Tuva, Russia
AU - Shestakova, Anastasia
AU - Guseva, Natalia
AU - Kopylova, Yulia
AU - Khvaschevskaya, Albina
AU - Arakchaa, Kara Kys
PY - 2019/6/7
Y1 - 2019/6/7
N2 - 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.
AB - 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.
UR - http://www.scopus.com/inward/record.url?scp=85067280944&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=85067280944&partnerID=8YFLogxK
U2 - 10.1051/e3sconf/20199807029
DO - 10.1051/e3sconf/20199807029
M3 - Conference article
AN - SCOPUS:85067280944
VL - 98
JO - E3S Web of Conferences
JF - E3S Web of Conferences
SN - 2555-0403
M1 - 07029
ER -