Abstract
The surfaces of fresh and tarnished bornite (Cu5FeS4) have been studied by measurement of reflectance and quantitative colour parameters in the visible region, X-ray photoelectron and Auger electron spectroscopy, and conversion electron Mossbauer spectroscopy. The tarnish is shown to be due to a surface coating of an iron hydroxy-oxide, leaving beneath it a layer with a copper sulphide composition, possibly due to metals in trigonal planar coordination resulting in destabilization of Fe3+ relative to Cu+, thus accounting for its preferential oxidation. -R.A.H.
Original language | English |
---|---|
Pages (from-to) | 285-293 |
Number of pages | 9 |
Journal | Mineralogical Magazine |
Volume | 51 |
Issue number | 2 |
DOIs | |
Publication status | Published - 1987 |