Mossbauer quantification of pyrrhotite in relation to self-heating

Finch, J. A.; Somot, S.; Navarra, A.; Ryan, D. H.; Graham, J. T.

Abstract

Pyrrhotite (Po) is widely considered the most significant mineral in the self-heating of sulphide ores and concentrates. It is therefore desirable to determine the amount of Po in a sample. This is commonly accomplished through X-ray diffraction (XRD) or quantitative evaluation of materials by scanning electron microscopy (QEM-SEM), neither of which are suited to oxidizing samples such as Po. The sample preparation for these methods often requires heating and drying, which may alter the composition. This paper introduces another quantitative method based on Mossbauer analysis, whose sample preparation is limited, and not as likely to alter the sample. The technique is tested using binary and ternary mixtures containing pyrrhotite with pentlandite (Pn), pyrite (Py) and sphalerite (Sp). A detection limit of 2 wt.% Po is easily obtained in the Po-Pn binary mixtures. The Po is also successfully measured in Pn-Po-Py and Sp-Po-Py mixtures: however, the presence of sphalerite increases the time required loran accurate measurement. The time required to measure Po in complex samples may be optimized through future work. (C) 2010 Elsevier Ltd. All rights reserved.

Más información

Título según WOS: ID WOS:000278791400009 Not found in local WOS DB
Título de la Revista: MINERALS ENGINEERING
Volumen: 23
Número: 8
Editorial: PERGAMON-ELSEVIER SCIENCE LTD
Fecha de publicación: 2010
Página de inicio: 652
Página final: 658
DOI:

10.1016/j.mineng.2010.03.022

Notas: ISI