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Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study. / Gorelova, Liudmila A. ; Pakhomova, Anna S. ; Krivovichev, Sergey V. ; Kasatkin, Anatoly V. ; Dubrovinsky, Leonid S.

в: Physics and Chemistry of Minerals, Том 47, № 5, 22, 01.05.2020.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Gorelova, LA, Pakhomova, AS, Krivovichev, SV, Kasatkin, AV & Dubrovinsky, LS 2020, 'Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study', Physics and Chemistry of Minerals, Том. 47, № 5, 22. https://doi.org/10.1007/s00269-020-01090-x

APA

Gorelova, L. A., Pakhomova, A. S., Krivovichev, S. V., Kasatkin, A. V., & Dubrovinsky, L. S. (2020). Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study. Physics and Chemistry of Minerals, 47(5), [22]. https://doi.org/10.1007/s00269-020-01090-x

Vancouver

Gorelova LA, Pakhomova AS, Krivovichev SV, Kasatkin AV, Dubrovinsky LS. Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study. Physics and Chemistry of Minerals. 2020 Май 1;47(5). 22. https://doi.org/10.1007/s00269-020-01090-x

Author

Gorelova, Liudmila A. ; Pakhomova, Anna S. ; Krivovichev, Sergey V. ; Kasatkin, Anatoly V. ; Dubrovinsky, Leonid S. / Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study. в: Physics and Chemistry of Minerals. 2020 ; Том 47, № 5.

BibTeX

@article{02033ceb35d147cfafd13b2b7f694cd7,
title = "Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study",
abstract = "Behaviour of hingganite-(Y), Y2□Be2Si2O8(OH)2, on compression to 47 GPa has been studied by synchrotron-based in situ high-pressure single-crystal X-ray diffraction at room temperature in a diamond anvil cell. In the studied pressure range no obvious phase transitions have been observed. The compression of hingganite-(Y) crystal structure is anisotropic, with b axis showing the maximal compressibility. A fit of the experimental pressure–volume data by the Birch-Murnaghan third-order equation of state yielded the bulk modulus of 131(2) GPa and its pressure first derivative of 3.5(2). The difference between high-pressure behaviour of hingganite-(Y) and structurally related datolite is governed by the different chemical nature of interlayer cations.",
keywords = "Crystal structure, Gadolinite group, High-pressure, Hingganite-(Y), Silicates, Synchrotron radiation",
author = "Gorelova, {Liudmila A.} and Pakhomova, {Anna S.} and Krivovichev, {Sergey V.} and Kasatkin, {Anatoly V.} and Dubrovinsky, {Leonid S.}",
note = "Gorelova, L.A., Pakhomova, A.S., Krivovichev, S.V. et al. Compressibility of hingganite-(Y): high-pressure single crystal X-ray diffraction study. Phys Chem Minerals 47, 22 (2020). https://doi.org/10.1007/s00269-020-01090-x",
year = "2020",
month = may,
day = "1",
doi = "10.1007/s00269-020-01090-x",
language = "English",
volume = "47",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer Nature",
number = "5",

}

RIS

TY - JOUR

T1 - Compressibility of hingganite‑(Y): high‑pressure single crystal X‑ray diffraction study

AU - Gorelova, Liudmila A.

AU - Pakhomova, Anna S.

AU - Krivovichev, Sergey V.

AU - Kasatkin, Anatoly V.

AU - Dubrovinsky, Leonid S.

N1 - Gorelova, L.A., Pakhomova, A.S., Krivovichev, S.V. et al. Compressibility of hingganite-(Y): high-pressure single crystal X-ray diffraction study. Phys Chem Minerals 47, 22 (2020). https://doi.org/10.1007/s00269-020-01090-x

PY - 2020/5/1

Y1 - 2020/5/1

N2 - Behaviour of hingganite-(Y), Y2□Be2Si2O8(OH)2, on compression to 47 GPa has been studied by synchrotron-based in situ high-pressure single-crystal X-ray diffraction at room temperature in a diamond anvil cell. In the studied pressure range no obvious phase transitions have been observed. The compression of hingganite-(Y) crystal structure is anisotropic, with b axis showing the maximal compressibility. A fit of the experimental pressure–volume data by the Birch-Murnaghan third-order equation of state yielded the bulk modulus of 131(2) GPa and its pressure first derivative of 3.5(2). The difference between high-pressure behaviour of hingganite-(Y) and structurally related datolite is governed by the different chemical nature of interlayer cations.

AB - Behaviour of hingganite-(Y), Y2□Be2Si2O8(OH)2, on compression to 47 GPa has been studied by synchrotron-based in situ high-pressure single-crystal X-ray diffraction at room temperature in a diamond anvil cell. In the studied pressure range no obvious phase transitions have been observed. The compression of hingganite-(Y) crystal structure is anisotropic, with b axis showing the maximal compressibility. A fit of the experimental pressure–volume data by the Birch-Murnaghan third-order equation of state yielded the bulk modulus of 131(2) GPa and its pressure first derivative of 3.5(2). The difference between high-pressure behaviour of hingganite-(Y) and structurally related datolite is governed by the different chemical nature of interlayer cations.

KW - Crystal structure

KW - Gadolinite group

KW - High-pressure

KW - Hingganite-(Y)

KW - Silicates

KW - Synchrotron radiation

UR - http://www.scopus.com/inward/record.url?scp=85083182784&partnerID=8YFLogxK

U2 - 10.1007/s00269-020-01090-x

DO - 10.1007/s00269-020-01090-x

M3 - Article

VL - 47

JO - Physics and Chemistry of Minerals

JF - Physics and Chemistry of Minerals

SN - 0342-1791

IS - 5

M1 - 22

ER -

ID: 52780593