Volume 628, Issue 2 pp. 357-362
Article

Synthesis and Characterization of the Synthetic Minerals Villyaellenite and Sarkinite, Mn5(AsO4)2(HAsO4)2 · 4H2O and Mn2(AsO4)(OH)

N. Stock Dr.

Corresponding Author

N. Stock Dr.

Munich, Ludwig-Maximilians-Universität, Department Chemie

Department Chemie der Ludwig-Maximilians-Universität, Butenandtstr. 5213, Haus E, D-81377 Munich, GermanySearch for more papers by this author
G. D. Stucky

G. D. Stucky

Santa Barbara/U.S.A., University of California, Department of Chemistry

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A. K. Cheetham

A. K. Cheetham

Santa Barbara/U.S.A., University of California, Materials Research Laboratory

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Abstract

Using hydrothermal methods, two manganese arsenates have been synthesized and characterized by single crystal X-ray diffraction. The products Mn5(AsO4)2(HAsO4)2 ?4H2O (1) and Mn2AsO4(OH) (2), the Mn end-members of the minerals villyaellenite and sarkinite, respectively, have been obtained (crystal data 1: monoclinic, C2/c, a = 18.109(4), b = 9.332(2), c = 9.809(2) Å, β = 96.172(4)?, Z = 4; 2: monoclinic, P21/c, a = 10.219(2), b = 13.613(2), c = 12.780(2) Å, β = 108.834(2)?, Z = 16). In both compounds a three-dimensional framework of edge-sharing MnO polyhedra is observed. Based on the availability of the all Mn2containing form of villyaellenite (1), the ordering scheme of the impurity cations of the natural samples could be confirmed. Magnetic susceptibility measurements of 1 indicate the presence of high-spin Mn2+ ions. The comparison of the data on sarkinite (2) with the data obtained from the natural sample indicates that the mineral has either a very high Mn content, or an absence of impurity cation ordering.

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