Abstract :
XPS, Fe La,b and Cu La,b X-ray emission and Fe L-, Cu L-, S L-edge and O K-edge absorption spectroscopies, Mo¨ssbauer
spectroscopy and cyclic voltammetry were applied to study reacted surface layers of natural chalcopyrite, CuFeS2. The surfaces
became metal-depleted after the anodic oxidation in 1 M HCl and the leaching in 1 M H2SO4 þ 0:2 M Fe2(SO4)3 or 1 M
HCl þ 0:4 M FeCl3 solutions, with the sulfur excess and iron/copper ratio been higher in the last instance, and were enriched in
copper after the electrochemical reduction. The electronic structures of the metal-deficient layers up to several tenths of
micrometer thick were similar to that of chalcopyrite, except that the density of the highest occupied states depended on sulfur
anions formed (predominant S3-anions after the ferric sulfate treatment, S4-anions after the ferric chloride leaching or the
potential sweep to 0.9 V, etc.). The layers created by the preliminary oxidation had only a small effect on the chalcopyrite
voltammetry. We suggest a new reaction mechanism considering a role of the surface changes, including disordering and
Anderson localization of the electronic states.
# 2003 Elsevier B.V. All rights reserved
Keywords :
Oxidative leaching , X-ray photoelectron spectroscopy , X-ray emission , X-ray absorption spectroscopy , Voltammetry , Chalcopyrite