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The decomposition of struvite

Published online by Cambridge University Press:  14 March 2018

A. Whitaker
A. Whitaker*
Affiliation:
Department of Physics, Brunel University, Woodlands Avenue, London, W. 3
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Summary

The subaerial decomposition of struvite has been investigated at room temperature (21±2° C), from which it has been concluded that the decomposition product is newberyite. X-ray power patterns of newberyite, both from a diffractometer and Debye-Scherrer cameras, are given. Comparison of these patterns with other newberyite patterns suggest that the camera pattern is more reproducible; this may be due to grain orientation in the diffraetometer mounts.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 36 , Issue 282 , June 1968 , pp. 820 - 824
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1968

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