The structure of synthetic tinsleyite K[Al2(PO4)2(OH)(H2O)]•H2O

被引:0
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作者
Dick, S [1 ]
机构
[1] Sud Chem AG, D-85368 Moosburg, Germany
关键词
crystal structure; phosphate mineral; tinsleyite; leucophosphite;
D O I
暂无
中图分类号
O61 [无机化学];
学科分类号
070301 ; 081704 ;
摘要
Synthetic tinsleyite K[Al-2(PO4)(2)(OH)(H2O)]. H2O has been obtained by the reaction of gibbsite with a potassium-phosphate solution of pH = 7 at 423 K within five days. A single crystal X-ray structure analysis has shown that synthetic tinsleyite is isotypic with the mineral leucophosphite K[Fe-2(PO4)(2)(OH)(H2O)]. H2O. Crystal data: monoclinic space group P2(1) / n, a = 949.9(2), b = 950.3(2), c = 953,5(2) pm, beta = 103.26(3)degrees, Z = 4. The structure of tinsleyite consists of tetranuclear Al4O2 units formed by a central pair of edge sharing AlO6 octahedra, to which two additional AlO6 octahedra are attached sharing corners. These units are crosslinked by phosphate ions to a three dimensional framework structure with tunnels along [010], occupied by potassium cations. While one type of water molecules is attached to Al, a second type is fixed in the structure by hydrogen bonds only. As a consequence two steps for thermal loss of water at 341 K and 471 K are observed.
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页码:1385 / 1390
页数:6
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