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Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3. / Siidra, O.I.; Borisov, A.S.; Lukina, E.A.; Nekrasova, D.O.; Platonova, N.V.

In: Physics and Chemistry of Minerals, Vol. 46, No. 4, 2019, p. 403-416.

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

Harvard

Siidra, OI, Borisov, AS, Lukina, EA, Nekrasova, DO & Platonova, NV 2019, 'Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3.', Physics and Chemistry of Minerals, vol. 46, no. 4, pp. 403-416. <http://elibrary.ru/item.asp?id=38624440>

APA

Siidra, O. I., Borisov, A. S., Lukina, E. A., Nekrasova, D. O., & Platonova, N. V. (2019). Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3. Physics and Chemistry of Minerals, 46(4), 403-416. http://elibrary.ru/item.asp?id=38624440

Vancouver

Siidra OI, Borisov AS, Lukina EA, Nekrasova DO, Platonova NV. Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3. Physics and Chemistry of Minerals. 2019;46(4):403-416.

Author

Siidra, O.I. ; Borisov, A.S. ; Lukina, E.A. ; Nekrasova, D.O. ; Platonova, N.V. / Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3. In: Physics and Chemistry of Minerals. 2019 ; Vol. 46, No. 4. pp. 403-416.

BibTeX

@article{7f917534d627472c8e707657af483f6f,
title = "Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3.",
abstract = "Anhydrous alkali copper sulfates constitute the most abundant group of mineral species from the Second Scoria Cone of the Great Tolbachik Fissure Eruption (1975–1976), a location being renowned for its great mineral diversity. Euchlorine, ideally KNaCu 3 O(SO 4 ) 3 , is the prevalent mineral in the hot sulfate-rich zones of the fumaroles. In this work, its thermal expansion and hydration/dehydration behavior have been studied. The results of a structure refinement from new single-crystal diffraction data are also reported, and a description of the structure based on anion-centered coordination polyhedra is given. The strongly anisotropic character of the thermal expansion of euchlorine remains essentially unchanged up to its decomposition. The strongest α 11 expansion is observed approximately perpendicular to the alkali interlayer of the structure, whereas the minimal α 22 and α 33 thermal expansion coefficients are parallel to the",
author = "O.I. Siidra and A.S. Borisov and E.A. Lukina and D.O. Nekrasova and N.V. Platonova",
year = "2019",
language = "English",
volume = "46",
pages = "403--416",
journal = "Physics and Chemistry of Minerals",
issn = "0342-1791",
publisher = "Springer Nature",
number = "4",

}

RIS

TY - JOUR

T1 - Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu 3 O(SO 4 ) 3.

AU - Siidra, O.I.

AU - Borisov, A.S.

AU - Lukina, E.A.

AU - Nekrasova, D.O.

AU - Platonova, N.V.

PY - 2019

Y1 - 2019

N2 - Anhydrous alkali copper sulfates constitute the most abundant group of mineral species from the Second Scoria Cone of the Great Tolbachik Fissure Eruption (1975–1976), a location being renowned for its great mineral diversity. Euchlorine, ideally KNaCu 3 O(SO 4 ) 3 , is the prevalent mineral in the hot sulfate-rich zones of the fumaroles. In this work, its thermal expansion and hydration/dehydration behavior have been studied. The results of a structure refinement from new single-crystal diffraction data are also reported, and a description of the structure based on anion-cen