Manganoan rockbridgeite Fe4.32Mn0.62Zn0.06(PO4)3(OH)5:: structure analysis and 57Fe Mossbauer spectroscopy

被引:13
|
作者
Redhammer, GJ
Roth, G
Tippelt, G
Bernroider, M
Lottermoser, W
Amthauer, G
Hochleitner, R
机构
[1] Salzburg Univ, Dept Mat Sci, Div Mineral, A-5020 Salzburg, Austria
[2] Rhein Westfal TH Aachen, Inst Crystallog, D-52056 Aachen, Germany
[3] Bavarian State Collect Mineral, D-80333 Munich, Germany
关键词
D O I
10.1107/S0108270106002472
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The structure of the basic iron phosphate rockbridgeite [ iron manganese zinc tris( phosphate) pentahydroxide] was reinvestigated with special emphasis on the cation distribution deduced from new X-ray and Fe-57 Mossbauer data. Rockbridgeite is orthorhombic, space group Cmcm, and shows three different Fe sites, one with 2/m symmetry, another with m symmetry and the third in a general position. One phosphate group has the P atom on a site with m symmetry, while the other has the P atom at a site with mm symmetry. Two Fe sites are fully occupied by ferric iron, while Mn3+ and Fe2+ are situated at a third, principally Fe, site. Structural data, bond-valence sums and polyhedral distortion parameters suggest a new interpretation of the rockbridgeite Fe-57 Mossbauer spectrum.
引用
收藏
页码:I24 / I28
页数:5
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