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American Mineralogist; July; v. 94; no. 7; p. 1071-1074; DOI: 10.2138/am.2009.3221
© 2009 Mineralogical Society of America
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Letter

Structure determination of the 2.5 hydrate MgSO4 phase by simulated annealing

Hongwei Ma1, David L. Bish1,*, Hsiu-Wen Wang1 and Steve J. Chipera2

1 Department of Geological Sciences, Indiana University, 1001 East 10th Street, Bloomington, Indiana 47405, U.S.A.
2 Chesapeake Energy Corporation, 6100 N. Western Avenue, Oklahoma City, Oklahoma 73118, U.S.A.

Correspondence: * E-mail: bish{at}indiana.edu

The crystal structure of the 2.5 hydrate MgSO4 phase was determined by simulated annealing from laboratory X-ray powder diffraction data measured from 2–140 °2{theta} using CuK{alpha} radiation. The 2.5 hydrate is monoclinic, space group C2/c, with unit-cell parameters a = 18.8636(4) Å, b = 12.3391(2) Å, c = 8.9957(2) Å, β = 94.568(2)°, V = 2087.1(6) Å3, and Z = 16. The model was refined using fundamental-parameters Rietveld refinement, converging to Rwp = 8.89%, Rp = 6.61%, Rexp = 3.33%, RBragg = 3.95%, and {chi}2 = 2.67. The refined structure is consistent with a formula of 2.5 H2O. Bond-valence calculations for the refined model show that the structure is chemically sensible. In the refined structure, [Mg(O,H2O)6] octahedra and [SO4] tetrahedra build up 2-D double-sheet slabs by sharing vertex O atoms, which are held together by inter-slab H-bonds involving (SO4)2– groups and H2O molecules coordinated with Mg2+ cations to form the layer structure of the 2.5 hydrate phase.

Key Words: MgSO4·2.5H2O • MgSO4·2.4H2O • crystal structure • simulated annealing • structure determination • powder diffraction • Rietveld refinement







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