Geochemical features of Kulunda plain lakes (Altay region, Russia)

M. N. Kolpakova, S. L. Shvartsev, S. V. Borzenko, V. P. Isupov, S. S. Shatskaya

Research output: Contribution to journalConference article

4 Citations (Scopus)

Abstract

Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.

Original languageEnglish
Article number012007
JournalIOP Conference Series: Earth and Environmental Science
Volume33
Issue number1
DOIs
Publication statusPublished - 15 Apr 2016
EventInternational Conference on Modern Problems of Hydrogeology, Geology Engineering and Hydrogeoecology of Eurasia, SPGE 2015 - Tomsk, Russian Federation
Duration: 23 Nov 201527 Nov 2015

Fingerprint

lake water
saturation
secondary mineral
lake
barite
steppe
biological processes
gypsum
calcite
evaporation
chloride
sodium
salinity
mineral
index
plain

ASJC Scopus subject areas

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

Cite this

Geochemical features of Kulunda plain lakes (Altay region, Russia). / Kolpakova, M. N.; Shvartsev, S. L.; Borzenko, S. V.; Isupov, V. P.; Shatskaya, S. S.

In: IOP Conference Series: Earth and Environmental Science, Vol. 33, No. 1, 012007, 15.04.2016.

Research output: Contribution to journalConference article

Kolpakova, M. N. ; Shvartsev, S. L. ; Borzenko, S. V. ; Isupov, V. P. ; Shatskaya, S. S. / Geochemical features of Kulunda plain lakes (Altay region, Russia). In: IOP Conference Series: Earth and Environmental Science. 2016 ; Vol. 33, No. 1.
@article{500b3458392a46cebc4c085897263a4c,
title = "Geochemical features of Kulunda plain lakes (Altay region, Russia)",
abstract = "Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.",
author = "Kolpakova, {M. N.} and Shvartsev, {S. L.} and Borzenko, {S. V.} and Isupov, {V. P.} and Shatskaya, {S. S.}",
year = "2016",
month = "4",
day = "15",
doi = "10.1088/1755-1315/33/1/012007",
language = "English",
volume = "33",
journal = "IOP Conference Series: Earth and Environmental Science",
issn = "1755-1307",
publisher = "IOP Publishing Ltd.",
number = "1",

}

TY - JOUR

T1 - Geochemical features of Kulunda plain lakes (Altay region, Russia)

AU - Kolpakova, M. N.

AU - Shvartsev, S. L.

AU - Borzenko, S. V.

AU - Isupov, V. P.

AU - Shatskaya, S. S.

PY - 2016/4/15

Y1 - 2016/4/15

N2 - Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.

AB - Geochemical specifics of lake water of the Kulunda Steppe territory (Altay region, Russia) are studied. The results show that in the territory mainly chloride and less soda lakes with sodium compound are developed. It is presented that calcite and soda saturation indexes (SI) of lake water increase with growth of pH, but decrease in such minerals as gypsum and barite. The opposite situation is typical for SI depending on the salinity. It is revealed that evaporation, secondary mineral formation and various biological processes have the greatest impact on accumulation of elements in solution.

UR - http://www.scopus.com/inward/record.url?scp=84971373108&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84971373108&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/33/1/012007

DO - 10.1088/1755-1315/33/1/012007

M3 - Conference article

AN - SCOPUS:84971373108

VL - 33

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012007

ER -