In situ X-ray diffraction (XRD) was used to elucidate the thermal decomposition of dolomite. As opposed to previous efforts that required samples be heated to a specific temperature and held for the duration of an X-ray scan, data was collected at 4O C intervals while continuously heating the sampl
β¦ LIBER β¦
Non-isothermal, in situ XRD analysis of dolomite decomposition
β Scribed by Philip Engler; Mark W. Santana; Martin L. Mittleman; David Balazs
- Publisher
- Elsevier Science
- Year
- 1989
- Tongue
- English
- Weight
- 524 KB
- Volume
- 140
- Category
- Article
- ISSN
- 0040-6031
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## Abstract The decomposition of ammonium heptamolybdate (AHM, (NH~4~)~6~Mo~7~O~24~Γ4H~2~O) was studied in situ by Xβray diffraction and Xβray absorption spectroscopy, as well as by thermal analysis (TG/DTA). Decomposition conditions such as reactant atmospheres, (20% oxygen, 5% propene, 5% hydroge