Abstract
On the basis of x-ray analysis of its crystal structure, weddellite (the tetragonal crystal of calcium oxalate polyhydrate) has been determined to be a zeolitic dihydrate salt. The oxalate ion has at least the symmetry 2mm and possibly the symmetry mmm . The calcium ion is coordinated with eight oxygen atoms arranged in the form of a distorted cubic antiprism.
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Publication Info
- Year
- 1964
- Type
- article
- Volume
- 146
- Issue
- 3643
- Pages
- 518-519
- Citations
- 20
- Access
- Closed
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Identifiers
- DOI
- 10.1126/science.146.3643.518