Oxidation of synthetic and natural samples of enargite and tennantite: 2. X-ray photoelectron spectroscopic study

被引:73
作者
Fullston, D [1 ]
Fornasiero, D [1 ]
Ralston, J [1 ]
机构
[1] Univ S Australia, Ian Wark Res Inst, Mawson Lakes, SA 5095, Australia
关键词
D O I
10.1021/la981525w
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The surface oxidation of synthetic and natural samples of enargite and tennantite has been monitored by X-ray photoelectron spectroscopy, XPS. The minerals were conditioned at pH 11.0 in an aqueous solution purged with nitrogen gas for 20 min or with oxygen gas for 60 min. The XPS results show that the oxidation layer on the mineral surface is thin. The surface oxidation products comprise copper and arsenic oxide/hydroxide, sulfite, and a sulfur-rich layer made of metal-deficient sulfide and/or polysulfide. The proportion of all of these oxidation products at the mineral surface is more important when the minerals are treated in more oxidizing conditions (i.e., with oxygen gas and for a longer time) for tennantite than for enargite and for the natural samples than for the synthetic samples. Different arsenic sulfide species have been found at the surfaces of enargite and tennantite: As4S4 Or As2S3 constitutes the major arsenic sulfide species at the surface of enargite, but these are the minor arsenic sulfide species at the surface of tennantite and in the bulk of both minerals. This difference is not related to a surface impurity in the natural enargite sample as it is also observed in the synthetic enargite sample.
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页码:4530 / 4536
页数:7
相关论文
共 32 条
[1]  
BARR TL, 1990, PRACTICAL SURFACE AN, V1, P357
[2]   THE SURFACE-COMPOSITION OF ARSENOPYRITE EXPOSED TO OXIDIZING ENVIRONMENTS [J].
BUCKLEY, AN ;
WALKER, GW .
APPLIED SURFACE SCIENCE, 1988, 35 (02) :227-240
[3]   INTERACTION OF GALENA WITH HYDROSULFIDE IONS UNDER CONTROLLED POTENTIALS [J].
BUCKLEY, AN ;
KRAVETS, IM ;
SHCHUKAREV, AV ;
WOODS, R .
JOURNAL OF APPLIED ELECTROCHEMISTRY, 1994, 24 (06) :513-520
[4]   AN X-RAY PHOTOELECTRON SPECTROSCOPIC STUDY OF THE OXIDATION OF CHALCOPYRITE [J].
BUCKLEY, AN ;
WOODS, R .
AUSTRALIAN JOURNAL OF CHEMISTRY, 1984, 37 (12) :2403-2413
[5]   AN XPS INVESTIGATION OF THE SURFACE OF NATURAL SPHALERITES UNDER FLOTATION-RELATED CONDITIONS [J].
BUCKLEY, AN ;
WOODS, R ;
WOUTERLOOD, HJ .
INTERNATIONAL JOURNAL OF MINERAL PROCESSING, 1989, 26 (1-2) :29-49
[6]  
BUCKLEY AN, 1988, 16 P INT MIN PROC C, P589
[7]   Process development for the separation of tetrahedrite from chalcopyrite in the Neves-Corvo ore of Somincor SA, Portugal [J].
Byrne, M ;
Grano, S ;
Ralston, J ;
Franco, A .
MINERALS ENGINEERING, 1995, 8 (12) :1571-1581
[8]   SURFACE CHARACTERIZATION OF GAAS AFTER THE REACTIVE ION ETCHING OF GEMOW OHMIC CONTACT IN RADIO-FREQUENCY SF6-O2 PLASMA [J].
CAMPO, A ;
CARDINAUD, C ;
TURBAN, G ;
DUBONCHEVALLIER, C ;
AMARGER, V ;
ETRILLARD, J .
JOURNAL OF VACUUM SCIENCE & TECHNOLOGY A-VACUUM SURFACES AND FILMS, 1993, 11 (05) :2536-2542
[9]  
Chen TT, 1980, CAN MINERAL, V18, P173
[10]   ROLE OF NATIVE OXIDE IN THE ACTIVATION OF IMPLANTED SI IN GAAS [J].
CHO, J ;
PAWLOWICZ, LM ;
SAHA, NC .
JOURNAL OF APPLIED PHYSICS, 1992, 72 (09) :4172-4177