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Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA. / Chukanov, Nikita V.; Menor-Salvan, Cesar; Gurzhiy, Vladislav V.; Izatulina, Alina R.; Pekov, Igor V.; Vigasina, Marina F.; Ksenofontov, Dmitry A.; Britvin, Sergey N.

In: Minerals, Vol. 11, No. 5, 448, 23.04.2021.

Research output: Contribution to journalArticlepeer-review

Harvard

Chukanov, NV, Menor-Salvan, C, Gurzhiy, VV, Izatulina, AR, Pekov, IV, Vigasina, MF, Ksenofontov, DA & Britvin, SN 2021, 'Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA', Minerals, vol. 11, no. 5, 448. https://doi.org/10.3390/min11050448

APA

Chukanov, N. V., Menor-Salvan, C., Gurzhiy, V. V., Izatulina, A. R., Pekov, I. V., Vigasina, M. F., Ksenofontov, D. A., & Britvin, S. N. (2021). Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA. Minerals, 11(5), [448]. https://doi.org/10.3390/min11050448

Vancouver

Author

Chukanov, Nikita V. ; Menor-Salvan, Cesar ; Gurzhiy, Vladislav V. ; Izatulina, Alina R. ; Pekov, Igor V. ; Vigasina, Marina F. ; Ksenofontov, Dmitry A. ; Britvin, Sergey N. / Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA. In: Minerals. 2021 ; Vol. 11, No. 5.

BibTeX

@article{f0cddc94e25c4217957ede0cf424b73c,
title = "Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA",
abstract = "Centimeter-sized crystals of orthorhombic calcium formate, α-Ca(HCO2 )2 from Alkali Lake, Oregon, USA have been studied by means of powder and single-crystal X-ray diffraction analysis, infrared, and Raman spectroscopy. Based on the data on carbon isotope abundance in calcium formate and associated minerals, it was concluded that the formation of α-Ca(HCO2 )2 may be a result of a combination of two factors: lake microbial metabolism and anthropogenic pollution with Agent Orange. Possible causes of stability of the low-density tetragonal β-Ca(HCO2 )2 polymorph (formicaite) in boron ores are discussed.",
keywords = "Agent Orange, Alkali lake, Bacterial formate production, Calcium formate, Crystal structure, Formicaite, IR spectroscopy, Mineral, Oregon, Polymorphism, Raman spectroscopy, Sedimentary deposits",
author = "Chukanov, {Nikita V.} and Cesar Menor-Salvan and Gurzhiy, {Vladislav V.} and Izatulina, {Alina R.} and Pekov, {Igor V.} and Vigasina, {Marina F.} and Ksenofontov, {Dmitry A.} and Britvin, {Sergey N.}",
note = "Publisher Copyright: {\textcopyright} 2021 by the authors. Licensee MDPI, Basel, Switzerland. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.",
year = "2021",
month = apr,
day = "23",
doi = "10.3390/min11050448",
language = "English",
volume = "11",
journal = "Minerals",
issn = "2075-163X",
publisher = "MDPI AG",
number = "5",

}

RIS

TY - JOUR

T1 - Biogenic orthorhombic α-calcium formate from sediments of alkali lake, Oregon, USA

AU - Chukanov, Nikita V.

AU - Menor-Salvan, Cesar

AU - Gurzhiy, Vladislav V.

AU - Izatulina, Alina R.

AU - Pekov, Igor V.

AU - Vigasina, Marina F.

AU - Ksenofontov, Dmitry A.

AU - Britvin, Sergey N.

N1 - Publisher Copyright: © 2021 by the authors. Licensee MDPI, Basel, Switzerland. Copyright: Copyright 2021 Elsevier B.V., All rights reserved.

PY - 2021/4/23

Y1 - 2021/4/23

N2 - Centimeter-sized crystals of orthorhombic calcium formate, α-Ca(HCO2 )2 from Alkali Lake, Oregon, USA have been studied by means of powder and single-crystal X-ray diffraction analysis, infrared, and Raman spectroscopy. Based on the data on carbon isotope abundance in calcium formate and associated minerals, it was concluded that the formation of α-Ca(HCO2 )2 may be a result of a combination of two factors: lake microbial metabolism and anthropogenic pollution with Agent Orange. Possible causes of stability of the low-density tetragonal β-Ca(HCO2 )2 polymorph (formicaite) in boron ores are discussed.

AB - Centimeter-sized crystals of orthorhombic calcium formate, α-Ca(HCO2 )2 from Alkali Lake, Oregon, USA have been studied by means of powder and single-crystal X-ray diffraction analysis, infrared, and Raman spectroscopy. Based on the data on carbon isotope abundance in calcium formate and associated minerals, it was concluded that the formation of α-Ca(HCO2 )2 may be a result of a combination of two factors: lake microbial metabolism and anthropogenic pollution with Agent Orange. Possible causes of stability of the low-density tetragonal β-Ca(HCO2 )2 polymorph (formicaite) in boron ores are discussed.

KW - Agent Orange

KW - Alkali lake

KW - Bacterial formate production

KW - Calcium formate

KW - Crystal structure

KW - Formicaite

KW - IR spectroscopy

KW - Mineral

KW - Oregon

KW - Polymorphism

KW - Raman spectroscopy

KW - Sedimentary deposits

UR - http://www.scopus.com/inward/record.url?scp=85104559281&partnerID=8YFLogxK

U2 - 10.3390/min11050448

DO - 10.3390/min11050448

M3 - Article

AN - SCOPUS:85104559281

VL - 11

JO - Minerals

JF - Minerals

SN - 2075-163X

IS - 5

M1 - 448

ER -

ID: 76725139