Möqssbauer Spectroscopy for Quantification of Pyrrhotite in Pyrrhotite/Pentlandite Mixtures Related to Self-Heating

Canadian Institute of Mining, Metallurgy and Petroleum
A. Navarra J. T. Graham S. Somot D. H. Ryan J. A. Finch
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
8
File Size:
557 KB
Publication Date:
Jan 1, 2009

Abstract

Pyrrhotite (Po) is widely considered to be the most significant mineral in the self-heating of sulphides. It is therefore desirable to determine the amount of Po in mineral samples. This is commonly accomplished through x-ray diffraction (XRD) or quantitative evaluation of materials by scanning electron microscopy (QEM-SEM). This paper introduces another quantitative method based on Mossbauer analysis that requires limited sample preparation and has the additional potential to detect the sulphur/iron ratio within Po. The technique is explored using pentlandite/pyrrhotite mixtures.
Citation

APA: A. Navarra J. T. Graham S. Somot D. H. Ryan J. A. Finch  (2009)  Möqssbauer Spectroscopy for Quantification of Pyrrhotite in Pyrrhotite/Pentlandite Mixtures Related to Self-Heating

MLA: A. Navarra J. T. Graham S. Somot D. H. Ryan J. A. Finch Möqssbauer Spectroscopy for Quantification of Pyrrhotite in Pyrrhotite/Pentlandite Mixtures Related to Self-Heating. Canadian Institute of Mining, Metallurgy and Petroleum, 2009.

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