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American Mineralogist; April; v. 94; no. 4; p. 622-625; DOI: 10.2138/am.2009.3110
© 2009 Mineralogical Society of America
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Letter

Determination of the crystal structure of sanderite, MgSO4·2H2O, by X-ray powder diffraction and the charge flipping method

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: hongma{at}indiana.edu

The crystal structure of sanderite, MgSO4·2H2O, was determined from laboratory X-ray powder diffraction data measured from 2–140 °2{theta} using CuK{alpha} radiation. Sanderite is orthorhombic, space group P212121, with unit-cell parameters a = 8.8932(1) Å, b = 8.4881(1) Å, c = 12.4401(2) Å, V = 939.16(3) Å3, Z = 8. The crystal structure model was determined using the charge flipping method and was refined using fundamental parameters Rietveld refinement method to Rwp = 6.52%, Rexp = 1.89%, and {chi}2 = 3.43. Bond-valence calculations for the refined model show that the structure is chemically reasonable. In the refined structure, Mg2+ cations are coordinated by four O atoms from [SO4]2– groups tetrahedra and by two H2O molecules, forming distorted octahedra. By sharing vertex O atoms, [SO4] and [MgO4(H2O)2] octahedra build up a 3-D framework.

Key Words: Sanderite • MgSO4·2H2O • crystal structure • charge flipping • structure determination • powder diffraction




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H. Ma, D. L. Bish, H.-W. Wang, and S. J. Chipera
Structure determination of the 2.5 hydrate MgSO4 phase by simulated annealing
American Mineralogist, July 1, 2009; 94(7): 1071 - 1074.
[Abstract] [Full Text] [PDF]




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