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Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite. / Krylov, D. P.; Kuznetsov, A. B.; Akimova, E. Yu.

In: Doklady Earth Sciences, Vol. 482, No. 2, 01.10.2018, p. 1354-1356.

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

Harvard

Krylov, DP, Kuznetsov, AB & Akimova, EY 2018, 'Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite', Doklady Earth Sciences, vol. 482, no. 2, pp. 1354-1356. https://doi.org/10.1134/S1028334X18100240

APA

Krylov, D. P., Kuznetsov, A. B., & Akimova, E. Y. (2018). Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite. Doklady Earth Sciences, 482(2), 1354-1356. https://doi.org/10.1134/S1028334X18100240

Vancouver

Krylov DP, Kuznetsov AB, Akimova EY. Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite. Doklady Earth Sciences. 2018 Oct 1;482(2):1354-1356. https://doi.org/10.1134/S1028334X18100240

Author

Krylov, D. P. ; Kuznetsov, A. B. ; Akimova, E. Yu. / Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite. In: Doklady Earth Sciences. 2018 ; Vol. 482, No. 2. pp. 1354-1356.

BibTeX

@article{3a3780febce84da69a9b85ec323f082b,
title = "Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite",
abstract = "The isotope fractionation β-factors have been determined for hydroxyapatite, fluorapatite, and carbon–apatite upon 18O/16O, 13C/12C, and 44Ca/40Ca substitutions depending on the temperature. Calculations were performed based on density functional theory (DFT). The results are expressed in terms of cubic polynomials against x = 106/T(K)2 and can be utilized as geothermometers if combined with β-factors of the coexisting phases. The new values of β-factors completely supersede the conventional semi-empirical (estimated by the method of increments) calibrations of isotopic equilibria involving apatite.",
author = "Krylov, {D. P.} and Kuznetsov, {A. B.} and Akimova, {E. Yu}",
year = "2018",
month = oct,
day = "1",
doi = "10.1134/S1028334X18100240",
language = "English",
volume = "482",
pages = "1354--1356",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - Calculation of Stable Isotope (O, C, Ca) Fractionation Factors for Apatite

AU - Krylov, D. P.

AU - Kuznetsov, A. B.

AU - Akimova, E. Yu

PY - 2018/10/1

Y1 - 2018/10/1

N2 - The isotope fractionation β-factors have been determined for hydroxyapatite, fluorapatite, and carbon–apatite upon 18O/16O, 13C/12C, and 44Ca/40Ca substitutions depending on the temperature. Calculations were performed based on density functional theory (DFT). The results are expressed in terms of cubic polynomials against x = 106/T(K)2 and can be utilized as geothermometers if combined with β-factors of the coexisting phases. The new values of β-factors completely supersede the conventional semi-empirical (estimated by the method of increments) calibrations of isotopic equilibria involving apatite.

AB - The isotope fractionation β-factors have been determined for hydroxyapatite, fluorapatite, and carbon–apatite upon 18O/16O, 13C/12C, and 44Ca/40Ca substitutions depending on the temperature. Calculations were performed based on density functional theory (DFT). The results are expressed in terms of cubic polynomials against x = 106/T(K)2 and can be utilized as geothermometers if combined with β-factors of the coexisting phases. The new values of β-factors completely supersede the conventional semi-empirical (estimated by the method of increments) calibrations of isotopic equilibria involving apatite.

UR - http://www.scopus.com/inward/record.url?scp=85056318348&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18100240

DO - 10.1134/S1028334X18100240

M3 - Article

AN - SCOPUS:85056318348

VL - 482

SP - 1354

EP - 1356

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 51217480