Structure of magnesium hydroxide sulfate [2MgSO(4).Mg(OH)(2)] and solid solution in magnesium hydroxide sulfate hydrate and caminite

被引:21
作者
Fleet, ME
Knipe, SW
机构
[1] Department of Earth Sciences, University of Western Ontario, London
来源
ACTA CRYSTALLOGRAPHICA SECTION B-STRUCTURAL SCIENCE | 1997年 / 53卷
关键词
D O I
10.1107/S0108768197000104
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
Magnesium hydroxide sulfate [2MgSO(4).Mg(OH)(2); MHS] is tetragonal with a = 7.454(1), c = 12.885(2) Angstrom, V = 716.0 Angstrom(3), space group P4(3)2(1)2, Z = 4 and D-x 2.774 g cm(-3). The structure (single-crystal X-ray, R = 0.025, wR = 0.023) comprises spiral (43) Single chains of corner-shared Mg(2) octahedra cross-linked by SO4 tetrahedra and face-shared Mg(1) octahedra. A linear ternary group of face-shared Mg octahedra [Mg(2)-Mg(1)-Mg(2)] alternates with an unoccupied octahedral position in rows along [<(1)over bar 10>]. A crystal of MHS was grown hydrothermally (0.15 Cpa, 673 K) from gold-bearing MgS-O-H fluid. The MHS structure, with Mg(1) octahedra sharing two octahedral faces with Mg(2) octahedra, revises the structure assumed for the complex solid solution magnesium hydroxide sulfate hydrate and the related ocean-floor mineral caminite [2MgSO(4).xMg(OH)(2).(2 - 2x)H2O; 0.5 less than or equal to x < 1.0]. The substitution reaction appears to be Mg(1)(2+) reversible arrow 2H(+). The H-substituted MHS structure is distinguished from that of kieserite (MgSO4.H2O), which has straight single chains of corner-shared Mg octahedra.
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页码:358 / 363
页数:6
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