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Calibration standard for X-ray diffraction analyses of coal liquefaction residues: Mössbauer spectra of synthetic pyrrhotite

✍ Scribed by R.H. Shiley; S.J. Russell; D.R. Dickerson; C.C. Hinkley; G.V. Smith; H. Twardowska; M. Saporoschenko

Book ID
107755561
Publisher
Elsevier Science
Year
1979
Tongue
English
Weight
227 KB
Volume
58
Category
Article
ISSN
0016-2361

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Synthetic almandine garnet, Fe3A12Si3012, has been studied by temperature -dependent single crystal X-ray diffraction and 57Fe M6ssbauer spectroscopy. The Fe 2+ doublet in almandine is characterized by a small asymmetry between the high and low-velocity peaks that decreases in magnitude with decreas