Mendeleev Commun., 2017, 27, 61–63
9 V. M. Kovrugin, M. Colmont, O. Mentre, O. I. Siidra and S.V. Krivovichev,
than its lowtemperature counterpart (due to an increase in both
29
Mineral. Mag., 2016, 80, 227.
0 S. V. Krivovichev, O. Mentre, O. I. Siidra, M. Colmont and S. K. Filatov,
Chem. Rev., 2013, 113, 6459.
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vibrational and configurational entropies ), which, together with
the data on density and unitcell volumes, strongly suggest that
the a and bmodifications of CuSe O are high and lowtem
perature polymorphs, respectively. This conclusion is consistent
with the 2D and 3D characters of their structures, respectively,
which is frequently observed in polymorphic inorganic com
pounds (that is, the structural dimensionality of a lowtempe
rature polymorph is higher than that of its hightemperature
1
2
5
1
1
2
664.
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1
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3
0,31
counterpart
).
This work was supported by the ANR (grant no. ANR
011JS08 00301) within the framework of the MultiInMaDe
project. The Fonds Europeen de Developpement Regional
FEDER), CNRS, Region Nord PasdeCalais, and Ministere
de l’Education Nationale de l’Enseignement Superieur et de la
Recherche are acknowledged for funding the Xray diffracto
meters. S.V.K. andV.M.K. acknowledge the support of the Russian
Science Foundation (theoretical studies; grant no. 141700071)
and the Russian Foundation for Basic Research (experimental
studies; grant no. 153520632).
1
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Received: 5th July 2016; Com. 16/4981
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