Research output: Contribution to journal › Article › peer-review
Synthesis and thermal behavior of pauflerite, β-VOSO4, and its α-modification. / Paufler, Peter; Filatov, Stanislav K.; Bubnova, Rimma S.; Krzhizhanovskaya, Maria G.
In: Zeitschrift fur Kristallographie - Crystalline Materials, Vol. 229, No. 11, 2014, p. 725-729.Research output: Contribution to journal › Article › peer-review
}
TY - JOUR
T1 - Synthesis and thermal behavior of pauflerite, β-VOSO4, and its α-modification
AU - Paufler, Peter
AU - Filatov, Stanislav K.
AU - Bubnova, Rimma S.
AU - Krzhizhanovskaya, Maria G.
PY - 2014
Y1 - 2014
N2 - Powder alpha-VOSO4 was prepared by dehydration of VOSO4 center dot 3H(2)O. beta-VOSO4 was synthesized by boiling of V2O5 in H2SO4. Thermal behaviour of VOSO4 center dot 3H(2)O, alpha- and beta-VOSO4 modifications is studied by high-temperature powder X-ray diffraction and thermal analysis, including two-step dehydration of VOSO4 center dot 3H(2)O, formation of alpha-VOSO4, thermal expansion and decomposition of both modifications into V2O5. Higher anisotropy of thermal expansion of the tetragonal alpha-modification alpha(c) = 39(2).10(-6) K-1 along the vanadyl ion and alpha(a) = 2.4(6).10(-6) K-1 in the perpendicular direction) comparing to the orthorhombic beta-modification (alpha(a) = 20.2(7), alpha(b) = 2.8(8), alpha(c) = 17.8(4).10(-6) K-1) is explained from a crystal chemical point of view.
AB - Powder alpha-VOSO4 was prepared by dehydration of VOSO4 center dot 3H(2)O. beta-VOSO4 was synthesized by boiling of V2O5 in H2SO4. Thermal behaviour of VOSO4 center dot 3H(2)O, alpha- and beta-VOSO4 modifications is studied by high-temperature powder X-ray diffraction and thermal analysis, including two-step dehydration of VOSO4 center dot 3H(2)O, formation of alpha-VOSO4, thermal expansion and decomposition of both modifications into V2O5. Higher anisotropy of thermal expansion of the tetragonal alpha-modification alpha(c) = 39(2).10(-6) K-1 along the vanadyl ion and alpha(a) = 2.4(6).10(-6) K-1 in the perpendicular direction) comparing to the orthorhombic beta-modification (alpha(a) = 20.2(7), alpha(b) = 2.8(8), alpha(c) = 17.8(4).10(-6) K-1) is explained from a crystal chemical point of view.
U2 - 10.1515/zkri-2014-1752
DO - 10.1515/zkri-2014-1752
M3 - Article
VL - 229
SP - 725
EP - 729
JO - Zeitschrift fur Kristallographie - Crystalline Materials
JF - Zeitschrift fur Kristallographie - Crystalline Materials
SN - 2194-4946
IS - 11
ER -
ID: 5743720