Abstract
The features of the conductivity of K9H7(SO4)8 · H2O single-crystal samples in the temperature range of superprotonic phase transition have been investigated. The K9H7(SO4)8 · H2O crystal structure is determined and refined taking into account hydrogen atoms by X-ray diffraction analysis at a temperature of 295 K: monoclinic symmetry, sp. gr. P21/c, Z = 4, a = 7.059(1), b = 19.773(1), c = 23.449(1) Å, β = 95.33(1)°, R 1/wR 2 = 2.71/1.71. The structural data obtained suggest that the occurrence of high conductivity in K9H7(SO4)8 · H2O crystals with an increase in temperature is related to the diffusion of crystallization water and motion of K ions, as well as to the transformation of the system of hydrogen bonds and protonic motion. The stabilization of the high-temperature superprotonic phase and its supercooling to low temperatures are due to the presence of channels for the motion of K ions and slow backward diffusion of water in the crystal.
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Dedicated to the memory of N.V. Belov
Original Russian Text © I.P. Makarova, T.S. Chernaya, V.V. Grebenev, V.V. Dolbinina, I.A. Verin, A.A. Simonov, 2011, published in Kristallografiya, 2011, Vol. 56, No. 6, pp. 1062–1072.
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Makarova, I.P., Chernaya, T.S., Grebenev, V.V. et al. Investigation of the structure and properties of K9H7(SO4)8 · H2O single crystals. Crystallogr. Rep. 56, 994–1003 (2011). https://doi.org/10.1134/S1063774511060174
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DOI: https://doi.org/10.1134/S1063774511060174