Whitaker, A. (1968) The decomposition of struvite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 820-824 doi:10.1180/minmag.1968.036.282.09
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The decomposition of struvite | ||
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society | ||
| Authors | Whitaker, A. | Author | |
| Year | 1968 (June) | Volume | 36 |
| Issue | 282 | ||
| Publisher | Mineralogical Society | ||
| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-282-820.pdf+ | ||
| DOI | doi:10.1180/minmag.1968.036.282.09Search in ResearchGate | ||
| Generate Citation Formats | |||
| Mindat Ref. ID | 6161 | Long-form Identifier | mindat:1:5:6161:6 |
| GUID | 0 | ||
| Full Reference | Whitaker, A. (1968) The decomposition of struvite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 820-824 doi:10.1180/minmag.1968.036.282.09 | ||
| Plain Text | Whitaker, A. (1968) The decomposition of struvite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 820-824 doi:10.1180/minmag.1968.036.282.09 | ||
| In | (1966) Mineralogical Magazine Vol. 36 (282) Mineralogical Society | ||
| Abstract/Notes | SummaryThe 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. | ||
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