Research output: Contribution to journal › Article › peer-review
Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu3O(SO4)3. / Siidra, Oleg I.; Borisov, Artem S.; Lukina, Evgeniya A.; Depmeier, Wulf; Platonova, Natalia V.; Colmont, Marie; Nekrasova, Diana O.
In: Physics and Chemistry of Minerals, Vol. 46, No. 4, 01.04.2019, p. 403-416.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Reversible hydration/dehydration and thermal expansion of euchlorine, ideally KNaCu3O(SO4)3
AU - Siidra, Oleg I.
AU - Borisov, Artem S.
AU - Lukina, Evgeniya A.
AU - Depmeier, Wulf
AU - Platonova, Natalia V.
AU - Colmont, Marie
AU - Nekrasova, Diana O.
PY - 2019/4/1
Y1 - 2019/4/1
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 3O(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 plane of {Cu 3O(SO 4) 3} 2− layers. Hydration experiments controlled by X-ray powder diffraction reveal a very complex behavior with multicomponent phase formation. Remarkably, upon heating stepwise dehydration occurs, whereby the complex mixture of hydrated sulfates gradually reverses and becomes again essentially single-phased anhydrous euchlorine.
AB - 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 3O(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 plane of {Cu 3O(SO 4) 3} 2− layers. Hydration experiments controlled by X-ray powder diffraction reveal a very complex behavior with multicomponent phase formation. Remarkably, upon heating stepwise dehydration occurs, whereby the complex mixture of hydrated sulfates gradually reverses and becomes again essentially single-phased anhydrous euchlorine.
KW - Euchlorine
KW - Evolution of minerals
KW - Exhalative minerals
KW - Reversible hydration/dehydration
KW - Sulfates
KW - Thermal expansion
KW - Tolbachik volcano
KW - X-ray diffraction
KW - CRYSTAL-STRUCTURE
KW - KAMCHATKA
KW - TETRAHEDRA
KW - REFINEMENT
KW - TOLBACHIK VOLCANO
KW - Reversible hydration
KW - dehydration
KW - HYDRATED SULFATE MINERALS
UR - http://www.scopus.com/inward/record.url?scp=85056428357&partnerID=8YFLogxK
U2 - 10.1007/s00269-018-1011-9
DO - 10.1007/s00269-018-1011-9
M3 - Article
AN - SCOPUS:85056428357
VL - 46
SP - 403
EP - 416
JO - Physics and Chemistry of Minerals
JF - Physics and Chemistry of Minerals
SN - 0342-1791
IS - 4
ER -
ID: 36116061