Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia)

Abstract

The basin model of total dissolved salt transformation in river water has been developed. It was tested in the Kirgizka River, the right tributary of the Tom River (Russia, Western Siberia, Tomsk). It was shown that the river system has the capacity of selfpurification and is characterized by rather stable salt composition. It is explained by the fact that the growth in dissolved salt concentration in river water is limited to some extent by, firstly, dilution of more mineralized groundwaters drained by rivers, and, secondly, relatively low solubility of some compounds.

Original language	English
Article number	012028
Journal	IOP Conference Series: Earth and Environmental Science
Volume	43
Issue number	1
DOIs	https://doi.org/10.1088/1755-1315/43/1/012028
Publication status	Published - 11 Oct 2016
Event	20th International Scientific Symposium of Students, Postgraduates and Young Scientists on Problems of Geology and Subsurface Development, PGON 2016 - Tomsk, Russian Federation Duration: 4 Apr 2016 → 8 Apr 2016

ASJC Scopus subject areas

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

Access to Document

10.1088/1755-1315/43/1/012028

Fingerprint Dive into the research topics of 'Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia)'. Together they form a unique fingerprint.

Cite this

@article{4b633fe1497245ff86036446c1028373,

title = "Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia)",

abstract = "The basin model of total dissolved salt transformation in river water has been developed. It was tested in the Kirgizka River, the right tributary of the Tom River (Russia, Western Siberia, Tomsk). It was shown that the river system has the capacity of selfpurification and is characterized by rather stable salt composition. It is explained by the fact that the growth in dissolved salt concentration in river water is limited to some extent by, firstly, dilution of more mineralized groundwaters drained by rivers, and, secondly, relatively low solubility of some compounds.",

author = "Savichev, {O. G.} and Matveenko, {I. A.} and Titov, {I. V.}",

year = "2016",

month = oct,

day = "11",

doi = "10.1088/1755-1315/43/1/012028",

language = "English",

volume = "43",

journal = "IOP Conference Series: Earth and Environmental Science",

issn = "1755-1307",

publisher = "IOP Publishing Ltd.",

number = "1",

note = "20th International Scientific Symposium of Students, Postgraduates and Young Scientists on Problems of Geology and Subsurface Development, PGON 2016 ; Conference date: 04-04-2016 Through 08-04-2016",

}

TY - JOUR

T1 - Basin Model of Total Dissolved Salts Transformation in Water of a Small River (the Kirgizka River, Tomsk, Russia)

AU - Savichev, O. G.

AU - Matveenko, I. A.

AU - Titov, I. V.

PY - 2016/10/11

Y1 - 2016/10/11

N2 - The basin model of total dissolved salt transformation in river water has been developed. It was tested in the Kirgizka River, the right tributary of the Tom River (Russia, Western Siberia, Tomsk). It was shown that the river system has the capacity of selfpurification and is characterized by rather stable salt composition. It is explained by the fact that the growth in dissolved salt concentration in river water is limited to some extent by, firstly, dilution of more mineralized groundwaters drained by rivers, and, secondly, relatively low solubility of some compounds.

AB - The basin model of total dissolved salt transformation in river water has been developed. It was tested in the Kirgizka River, the right tributary of the Tom River (Russia, Western Siberia, Tomsk). It was shown that the river system has the capacity of selfpurification and is characterized by rather stable salt composition. It is explained by the fact that the growth in dissolved salt concentration in river water is limited to some extent by, firstly, dilution of more mineralized groundwaters drained by rivers, and, secondly, relatively low solubility of some compounds.

UR - http://www.scopus.com/inward/record.url?scp=84997817451&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=84997817451&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/43/1/012028

DO - 10.1088/1755-1315/43/1/012028

M3 - Article

AN - SCOPUS:84997817451

VL - 43

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012028

T2 - 20th International Scientific Symposium of Students, Postgraduates and Young Scientists on Problems of Geology and Subsurface Development, PGON 2016

Y2 - 4 April 2016 through 8 April 2016

ER -