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Commensurate structure of Ca(2)CoSi(2)O(7), a new twinned orthorhombic structure
1Department of Life Science, Himeji Institute of Technology, Japan. hagiya@sci.himeji-tech.ac.jp
Summary
The crystal structure of dicalcium cobalt disilicate (Ca(2)CoSi(2)O(7)) was determined using a novel least-squares program for twinned crystals. Its arrangement of calcium polyhedra and cobalt tetrahedra differs from previous findings.
Area of Science:
- Crystallography
- Materials Science
- Solid State Chemistry
Background:
- The melilite group minerals exhibit complex crystal structures.
- Understanding variations in these structures is crucial for materials science applications.
- Previous studies on Ca(2)CoSi(2)O(7) have suggested certain structural arrangements.
Purpose of the Study:
- To elucidate the crystal structure of the commensurate phase of dicalcium cobalt disilicate (Ca(2)CoSi(2)O(7)).
- To refine the structure using a specialized least-squares program for twinned crystals.
- To compare the derived structure with previously reported findings.
Main Methods:
- Derivation of the crystal structure from a (3+2)-dimensional modulated structure.
- X-ray diffraction analysis of twinned Ca(2)CoSi(2)O(7) crystals at 170 K.
- Refinement using a newly developed least-squares program for twinned crystal data.
Main Results:
- The crystal structure is orthorhombic with space group P2(1)2(1)2 and dimensions a = 23.510 (4), b = 23.510 (4), c = 5.025 (1) Å.
- The structure features a regular arrangement of sixfold coordinated calcium polyhedra and CoO(4) tetrahedra along the [001] direction.
- The observed distribution of these structural units differs from prior reports.
Conclusions:
- The crystal structure of Ca(2)CoSi(2)O(7) in its commensurate phase has been successfully determined.
- The use of a specialized refinement program was essential due to crystal twinning.
- The findings provide new insights into the structural variations within the melilite group.