Research output: Contribution to journal › Article › peer-review
Isostructural crystal hydrates of rare-earth metal oxalates at high pressure : From strain anisotropy to dehydration. / Zakharov, Boris A.; Gribov, Pavel A.; Matvienko, Alexander A. et al.
In: Zeitschrift fur Kristallographie - Crystalline Materials, Vol. 232, No. 11, 26.10.2017, p. 751-757.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Isostructural crystal hydrates of rare-earth metal oxalates at high pressure
T2 - From strain anisotropy to dehydration
AU - Zakharov, Boris A.
AU - Gribov, Pavel A.
AU - Matvienko, Alexander A.
AU - Boldyreva, Elena V.
PY - 2017/10/26
Y1 - 2017/10/26
N2 - The crystal structures of a series of isostructural rare-earth metal oxalates, (REE)2(C2O4)3·10H2O (REE=Sm, Y) and a 1:1 YSm(C2O4)3·10H2O solid solution, have been studied in situ by single-crystal X-ray diffraction and optical microscopy. The structures were followed from ambient pressure to 6 GPa in a DAC with paraffin as the hydrostatic fluid. Bulk compressibilities, anisotropic lattice strain on hydrostatic compression and the corresponding changes in the atomic coordinates were followed. Discontinuities/sharp changes in the slopes of the pressure dependences of volume and selected cell parameters have been observed for yttrium-containing salts at 3.5 GPa. This may be related to the re-distribution of water molecules within the crystal structure. Y2(C2O4)3·10H2O undergoes a partial dehydration at 1 GPa, forming monoclinic Y2(C2O4)3·6H2O as single-crystalline inclusions in the original phase.
AB - The crystal structures of a series of isostructural rare-earth metal oxalates, (REE)2(C2O4)3·10H2O (REE=Sm, Y) and a 1:1 YSm(C2O4)3·10H2O solid solution, have been studied in situ by single-crystal X-ray diffraction and optical microscopy. The structures were followed from ambient pressure to 6 GPa in a DAC with paraffin as the hydrostatic fluid. Bulk compressibilities, anisotropic lattice strain on hydrostatic compression and the corresponding changes in the atomic coordinates were followed. Discontinuities/sharp changes in the slopes of the pressure dependences of volume and selected cell parameters have been observed for yttrium-containing salts at 3.5 GPa. This may be related to the re-distribution of water molecules within the crystal structure. Y2(C2O4)3·10H2O undergoes a partial dehydration at 1 GPa, forming monoclinic Y2(C2O4)3·6H2O as single-crystalline inclusions in the original phase.
KW - dehydration
KW - high pressures
KW - isostructural salt hydrates
KW - ELEMENTS
KW - YTTRIUM
UR - http://www.scopus.com/inward/record.url?scp=85032960561&partnerID=8YFLogxK
U2 - 10.1515/zkri-2016-2038
DO - 10.1515/zkri-2016-2038
M3 - Article
AN - SCOPUS:85032960561
VL - 232
SP - 751
EP - 757
JO - Zeitschrift fur Kristallographie - Crystalline Materials
JF - Zeitschrift fur Kristallographie - Crystalline Materials
SN - 2194-4946
IS - 11
ER -
ID: 9561208