CONFIRMATION OF A SULFUR-RICH LAYER ON PYRITE AFTER OXIDATIVE DISSOLUTION BY FE(III) IONS AROUND PH-2

被引:105
作者
SASAKI, K [1 ]
TSUNEKAWA, M [1 ]
OHTSUKA, T [1 ]
KONNO, H [1 ]
机构
[1] NAGOYA INST TECHNOL,DEPT APPL CHEM,NAGOYA,AICHI 466,JAPAN
关键词
D O I
10.1016/0016-7037(95)00203-C
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The stoichiometry of pyrite dissolution by Fe(III) ions was studied in chloride media around pH 2. Pyrite was found to dissolve nonstoichiometrically during the initial tens of hours and a S-rich layer was formed on the pyrite due to preferential dissolution of iron. The major constituent of the layer was elemental S, identified by X-ray photoelectron spectroscopy (XPS) and Raman spectroscopy.
引用
收藏
页码:3155 / 3158
页数:4
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