Author:
England K. E. R.,Charnock J. M.,Pattrick R. A. D.,Vaughan D. J.
Abstract
Abstract
The oxidation of chalcopyrite and pyrite was examined using
Fe-K- and Cu-K-edge
REFLEXAFS spectroscopy. The Fe XANES of the pyrite proved to be a very sensitive
indicator of oxidation, revealing the development of a goethite-like surface
species; the EXAFS data showed an increasing O:S ratio with the degree of
oxidation and gave Fe–O distances of c. 1.9 Å. On the
oxidized chalcopyrite surfaces, the development of Fe-O and Cu-O species was
observed, with both the XANES and EXAFS revealing the progressive development of
these species with oxidation. Differences in the sensitivity of the XANES and
EXAFS to the degree of oxidation can be related to the degree of long range order
and changes in the intensity of the pre-edge feature of the Fe are a function of
its oxidation state and coordination geometry in the surface species.
Subject
Geochemistry and Petrology
Cited by
35 articles.
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