柯石英
硫化铜
硫化物
辉铜矿
氧化态
铜
化学
金属有机化学
产量(工程)
X射线光电子能谱
无机化学
结晶学
材料科学
冶金
黄铜矿
晶体结构
催化作用
化学工程
有机化学
工程类
作者
Siew Wei Goh,Alan N. Buckley,Robert N. Lamb
标识
DOI:10.1016/j.mineng.2005.09.003
摘要
Reference to covellite as copper(II) sulfide has been challenged. To support the nominally Cu(I) formal oxidation state for covellite suggested by X-ray photoelectron spectroscopy, the Cu L2,3 near-edge X-ray absorption fine structure spectrum for unoxidised covellite has been determined in fluorescence yield mode. Interpretation of the Cu L3-edge spectrum has been effected with the assistance of ab initio calculations of the density of unfilled states and the simulation of spectra from both Cu sites in the covellite structure. An alternative explanation has been provided for a covellite Cu L2,3-edge spectrum determined in electron yield mode that had been rationalised previously in terms of the presence of both Cu(I) and Cu(II) in the covellite structure. The relevance to mineral processing of the Cu(I) formal oxidation state in copper sulfides and other sulfide minerals has been discussed.
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