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Title: Detection of magnetite particles in coal by ferromagnetic resonance

Journal Article · · J. Appl. Phys.; (United States)
DOI:https://doi.org/10.1063/1.334525· OSTI ID:5982062

The techniques of ferromagnetic (FMR) and electron paramagnetic resonance have been applied in studies of Pittsburgh No. 8 bituminous coal. The specimen has been found to be magnetically very heterogeneous, with paramagnetic Mn/sup 2 +/ and Fe/sup 3 +/, free radicals, and at least one ferromagnetic specie which is identified and characterized in the present paper. The temperature dependence of the spectral line shapes indicates the occurrence of a phase transition at 123 K for a finely ground powder sample and at 121 K for a hand-picked fragment; these temperatures are characteristic of the Verwey transition in magnetite, and confirm its presence in both samples. Linewidth data provide an upper limit of 0.07 ..mu..m on the particle size in the powdered sample. The chemical composition of the magnetite in the powdered sample is estimated, on the basis of the observed transition temperature, to be between Fe/sub 2.988/O/sub 4/ and Fe/sub 2.997/O/sub 4/. Spectra of the residue and the glass extract obtained after treatment of the powdered sample with HCl confirm the identification of magnetite, and indicate that it is not embedded in the organic matter in the coal, but should be easily removed either by acid treatment or magnetic separation. The results suggest the potential usefulness in the identification and physical and chemical characterization of ferro- and ferrimagnetic minerals in coals.

Research Organization:
Department of Physics, Texas Christian University, Fort Worth, Texas 76129
OSTI ID:
5982062
Journal Information:
J. Appl. Phys.; (United States), Vol. 57:4
Country of Publication:
United States
Language:
English

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