The surface oxidation of metal sulfides in air and aqueous solution is of c
entral importance in mineral separation and environmental control of acid m
ine drainage. Mechanisms of oxidation, dissolution and surface restructurin
g have been extensively studied using XPS. High binding energy components i
n S 2p XPS spectra have been attributed to metal-deficiency formation of po
lysulfide S-n(2-), elemental sulfur and electronic defect structures (ie Cu
(I)/ZnS). The assignment of these components in S 2p XPS spectra has, howev
er, left significant uncertainties particularly in the formation of S-S bon
ding in polysulfide species requiring confirmation from other surface analy
tical techniques.
The use of static ToF-SIMS has provided a new avenue for identification of
these species and their development in oxidation of the sulfide surfaces. F
or the iron sulfides, there is a systematic change in the FeS2/FeS fragment
ratio from troilite (FeS) through pyrrhotite (Fe-1-S-x) to pyrite (FeS2) w
ith ratios varying from 0.59, 1.2 to 32 respectively. Similarly high ratios
for FeSn/FeS are found for pyrite compared with pyrrhotite and troilite mi
rrored in the S-n/S fragment ratios. Changes in surface oxidation, represen
ted in atomic concentrations and S 2p XPS spectra, are seen in the ToF-SIMS
signals for S-n/SOn ratios in the same iron sulfide sequence. These mass m
arkers, reflecting increased S-S bonding, increase in surfaces after oxidat
ion giving further confidence in XPS assignment to polysulfide species.
Freshly cleaved galena PbS surfaces reacted in pH8 aqueous solution for inc
reasing periods of time have also shown a systematic increase in S-n/S rati
os with increasing at.% of oxidised S-n(2-) species from XPS spectra. Stati
stical analysis of oxidised galena has shown that the ratios (PbO+)-Pb-206/
Pb-206(+) and (PbOH+)-Pb-208/Pb-208(+) directly reflect the degree of oxida
tion of the surface lead species whilst the O-S-, S-/total - ion yield and
SO3-/S- are the best measures for following the oxidation of sulfur species
. Results from these ratios suggest that initial air oxidation takes place
predominantly on the S sites rather than Pb sites but, in solution at pH9,
both sites are oxidised.
The ToF-SIMS results appear to directly reflect the surface chemistry of th
e metal and sulfur species and are not consistent with recombination or fra
gmentation of secondary neutral or ionic species. The results strongly sugg
est increasing polymerisation of S-S species with increasing oxidation in a
ccord with the XPS assignment to polysulfide of increasing chain length. (C
) 2000 Published by Elsevier Science Ltd. All rights reserved.