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Published on: December 29, 2016
Schaurteite, Ca(3)Ge(SO(4))(2)(OH)(6)·3H(2)O.
Marcus J Origlieri1, Robert T Downs
1Department of Geosciences, University of Arizona, Tucson, AZ 85721, USA.
The crystal structure of schaurteite, a calcium germanium sulfate mineral, was determined for the first time using X-ray diffraction. This reveals its unique arrangement of polyhedra and hydrogen bonding, aiding mineralogical classification.
Area of Science:
- Mineralogy
- Crystallography
- Geochemistry
Background:
- Schaurteite (Ca(3)Ge(SO(4))(2)(OH)(6)·3H(2)O) is a rare mineral belonging to the fleischerite group.
- Understanding its crystal structure is crucial for mineral classification and understanding related compounds.
Purpose of the Study:
- To determine the first crystal structure of schaurteite using single-crystal X-ray diffraction.
- To elucidate the atomic arrangement and bonding within the schaurteite mineral structure.
Main Methods:
- Single-crystal X-ray diffraction was performed on a natural schaurteite sample.
- Full-matrix refinement was employed to locate atoms and hydrogen bonds within the crystal structure.
Main Results:
- The crystal structure of schaurteite was successfully determined, revealing its unique composition: tricalcium germanium bis-(sulfate) hexa-hydroxide trihydrate.
- The structure features slabs of calcium polyhedra interleaved with germanium octahedra and sulfate tetrahedra.
- Two hydrogen atoms were located, participating in O-H⋯O hydrogen bonds.
Conclusions:
- This study provides the definitive crystal structure of schaurteite, a significant contribution to mineralogy.
- The determined structure clarifies schaurteite's relationship within the fleischerite group of minerals.
- The findings offer insights into the structural chemistry of germanium-bearing minerals.
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