Structure of microporous QUI-MnGS-1 and in situ studies of its formation using time-resolved synchrotron x-ray powder diffraction

被引:36
作者
Cahill, CL [1 ]
Ko, YH
Hanson, JC
Tan, KM
Parise, JB
机构
[1] SUNY Stony Brook, Dept Chem, New York, NY 11794 USA
[2] SUNY Stony Brook, Dept Geosci, New York, NY 11794 USA
[3] Brookhaven Natl Lab, Dept Chem, Upton, NY 11973 USA
关键词
D O I
10.1021/cm980026d
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 ; 081704 ;
摘要
The structure of QUI-MnGS-1 has been determined from single-crystal X-ray diffraction on a similar to 0.03 x 0.03 x 0.02 mm sample using synchrotron radiation. This material [(C7H13N)Mn0.25Ge1.75S4 . H2O] crystallizes in space group I (4) over bar 2d with unit cell a = 11.581(1) and c = 18.741(3) A. The extended framework of this structure consists of corner-linked [Ge4S10](4-) clusters, the centers of which occupy nodes of a distorted diamond lattice. The B-rings defined by this lattice form channels that contain the water and organic components of this compound. In situ synchrotron X-ray diffraction studies of its synthesis indicate that an Mn-free precursor phase forms prior to transformation to QUI-MnGS-1. In situ calcination experiments demonstrate that this material is thermally stable to approximately 360 degrees C.
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页码:1453 / 1458
页数:6
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