Iron content of pyrrhotites produced in continuous liquefaction units

The XRD measurement of d102 has been used to study pyrrhotites formed by the liquefaction of coal. The amount of Fe in the coal may affect the distillate yield. Some reactor conditions produce asymmetric XRD peaks in the pyrrhotite which may reflect stacking disorder. This is the first time XRD has...

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Bibliographic Details
Published inThe American mineralogist Vol. 66; no. 11-12; pp. 1258 - 1262
Main Authors Pollack, S. S, Spitler, C. A
Format Journal Article
LanguageEnglish
Published Mineralogical Society of America 01.12.1981
Subjects
abundance
beneficiation
chemical properties
coal
crystal chemistry
experimental studies
Geochemistry
iron
liquefaction
metals
minerals
organic residues
production
properties
pyrrhotite
rock, sediment, soil
sedimentary rocks
sulfides
X-ray data
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Summary:The XRD measurement of d102 has been used to study pyrrhotites formed by the liquefaction of coal. The amount of Fe in the coal may affect the distillate yield. Some reactor conditions produce asymmetric XRD peaks in the pyrrhotite which may reflect stacking disorder. This is the first time XRD has been used to report stacking disorder.
ISSN:0003-004X
1945-3027