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Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O. / Charykova, M. V.; Charykov, N. A.

In: Geochemistry International, Vol. 42, No. 2, 01.02.2004, p. 169-177.

Research output: Contribution to journal › Article › peer-review

Harvard

Charykova, MV & Charykov, NA 2004, 'Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O', Geochemistry International, vol. 42, no. 2, pp. 169-177.

APA

Charykova, M. V., & Charykov, N. A. (2004). Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O. Geochemistry International, 42(2), 169-177.

Vancouver

Charykova MV, Charykov NA. Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O. Geochemistry International. 2004 Feb 1;42(2):169-177.

Author

Charykova, M. V. ; Charykov, N. A. / Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O. In: Geochemistry International. 2004 ; Vol. 42, No. 2. pp. 169-177.

BibTeX

@article{93e6694af65e450d8d35238a58b26e75,
title = "Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O",
abstract = "This paper presents the results of calculations of binary and ternary parameters of the Pitzer equation and the thermodynamic potentials of solid phases crystallizing in the water-salt systems that model chloride brines taking into account the presence of strontium and barium ions. Phase solubility diagrams were calculated for the respective three- and four-component systems containing sodium, potassium, magnesium, calcium, strontium, and barium chlorides within a temperature interval of 0-40°C. The results of calculations are consistent with the limited experimental data on solubility and can be used for modeling the crystallization of salts in the course of seawater and brine concentration, subsequent burial, and interaction with the host rocks. Copyright {\textcopyright} 2004 by MAIK {"}Nauka/Interperiodica{"} (Russia).",
author = "Charykova, {M. V.} and Charykov, {N. A.}",
year = "2004",
month = feb,
day = "1",
language = "English",
volume = "42",
pages = "169--177",
journal = "Geochemistry International",
issn = "0016-7029",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Thermodynamic model of natural brines accounting for the presence of trace components. I. System Na+, K+, Mg 2+, Ca2+, Sr2+, Ba2+ ∥ Cl-, SO42- - H2O

AU - Charykova, M. V.

AU - Charykov, N. A.

PY - 2004/2/1

Y1 - 2004/2/1

N2 - This paper presents the results of calculations of binary and ternary parameters of the Pitzer equation and the thermodynamic potentials of solid phases crystallizing in the water-salt systems that model chloride brines taking into account the presence of strontium and barium ions. Phase solubility diagrams were calculated for the respective three- and four-component systems containing sodium, potassium, magnesium, calcium, strontium, and barium chlorides within a temperature interval of 0-40°C. The results of calculations are consistent with the limited experimental data on solubility and can be used for modeling the crystallization of salts in the course of seawater and brine concentration, subsequent burial, and interaction with the host rocks. Copyright © 2004 by MAIK "Nauka/Interperiodica" (Russia).

AB - This paper presents the results of calculations of binary and ternary parameters of the Pitzer equation and the thermodynamic potentials of solid phases crystallizing in the water-salt systems that model chloride brines taking into account the presence of strontium and barium ions. Phase solubility diagrams were calculated for the respective three- and four-component systems containing sodium, potassium, magnesium, calcium, strontium, and barium chlorides within a temperature interval of 0-40°C. The results of calculations are consistent with the limited experimental data on solubility and can be used for modeling the crystallization of salts in the course of seawater and brine concentration, subsequent burial, and interaction with the host rocks. Copyright © 2004 by MAIK "Nauka/Interperiodica" (Russia).

UR - http://www.scopus.com/inward/record.url?scp=2942573231&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:2942573231

VL - 42

SP - 169

EP - 177

JO - Geochemistry International

JF - Geochemistry International

SN - 0016-7029

IS - 2

ER -

ID: 127758907