Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva)

Abstract

The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO₂-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.

Original language	English
Pages (from-to)	1295-1305
Number of pages	11
Journal	Russian Geology and Geophysics
Volume	55
Issue number	11
DOIs	https://doi.org/10.1016/j.rgg.2014.10.004
Publication status	Published - 1 Jan 2014

Keywords

Carbon dioxide waters
Chemical composition
Choigan
Tuva
Water-rock interaction

ASJC Scopus subject areas

Geology
Geophysics

Access to Document

10.1016/j.rgg.2014.10.004

Fingerprint Dive into the research topics of 'Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva)'. Together they form a unique fingerprint.

Cite this

@article{d307b064c60b47528533d4c970132b88,

title = "Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva)",

abstract = "The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.",

keywords = "Carbon dioxide waters, Chemical composition, Choigan, Tuva, Water-rock interaction",

author = "Kopylova, {Yu G.} and Guseva, {Natalia Vladimirovna} and Arakchaa, {K. D.} and Khvashchevskaya, {Albina Anatolievna}",

year = "2014",

month = jan,

day = "1",

doi = "10.1016/j.rgg.2014.10.004",

language = "English",

volume = "55",

pages = "1295--1305",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier",

number = "11",

}

TY - JOUR

T1 - Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva)

AU - Kopylova, Yu G.

AU - Guseva, Natalia Vladimirovna

AU - Arakchaa, K. D.

AU - Khvashchevskaya, Albina Anatolievna

PY - 2014/1/1

Y1 - 2014/1/1

N2 - The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.

AB - The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.

KW - Carbon dioxide waters

KW - Chemical composition

KW - Choigan

KW - Tuva

KW - Water-rock interaction

UR - http://www.scopus.com/inward/record.url?scp=84922638823&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84922638823&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2014.10.004

DO - 10.1016/j.rgg.2014.10.004

M3 - Article

AN - SCOPUS:84922638823

VL - 55

SP - 1295

EP - 1305

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 11

ER -