Soft X-ray spectroscopic studies of the reaction of fractured pyrite surfaces with Cr(Vl)-containing aqueous solutions

被引:48
作者
Doyle, CS [1 ]
Kendelewicz, T
Bostick, BC
Brown, GE
机构
[1] Stanford Univ, Dept Geol & Environm Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA
[2] Dartmouth Coll, Dept Earth Sci, Hanover, NH 03755 USA
[3] SLAC, Stanford Synchrotron Radiat Lab, Menlo Pk, CA 94025 USA
基金
美国国家科学基金会;
关键词
D O I
10.1016/j.gca.2004.02.015
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
We have used synchrotron-based soft X-ray core-level photoemission and adsorption spectroscopies to study the reaction of aqueous sodium chromate solutions with freshly fractured pyrite surfaces. Pyrite surfaces were reacted with 50 muM sodium chromate solution at pH 7 for reaction times between 1 min and 37 hr. Additional experiments were performed at pH 2 and pH 4 with 50 muM sodium chromate solutions and at pH 7 with 5 mM solutions. At chromate concentrations of 50 muM, all chromium present on the pyrite surface was in the form of Cr(III), while at 5 mM, both Cr(III) and Cr(VI) were present at the pyrite surface. Minor quantities of oxidized sulfur species (sulfate, sulfite, and zero-valent sulfur) were identified as reaction products on the pyrite surface. The amount of oxidized sulfur species observed on the surface was greater when pyrite was reacted with 5 mM Cr(VI) solutions because the rate of chromium deposition exceeded the rate of dissolution of pyrite oxidation products, effectively trapping Cr(VI) and oxidized sulfur species in an overlayer of iron(III)-containing Cr(III)-hydroxide. This work shows that pyrite, an extremely cheap and readily available waste material, may be suitable for the removal of hexavalent chromium from acidic to circumneutral waste streams. The reduced chromium ultimately forms a coating on the pyrite surface, which passivates the pyrite surface towards further oxidation. Copyright (C) 2004 Elsevier Ltd.
引用
收藏
页码:4287 / 4299
页数:13
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