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Difference in enthalpies of decomposition of dolomite-ankerites in variable atmospheres

โœ Scribed by J.V. Dubrawski


Publisher
Elsevier Science
Year
1992
Tongue
English
Weight
218 KB
Volume
198
Category
Article
ISSN
0040-6031

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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