The composition of coexisting jarosite-group minerals and water from the Richmond mine, Iron Mountain, California

被引:49
作者
Jamieson, HE [1 ]
Robinson, C
Alpers, CN
Nordstrom, DK
Poustovetov, A
Lowers, HA
机构
[1] Queens Univ, Dept Geol Sci, Kingston, ON K7L 3N6, Canada
[2] US Geol Survey, Sacramento, CA 95819 USA
[3] US Geol Survey, Boulder, CO 80303 USA
[4] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA
关键词
jarosite; acid mine-drainage; aqueous speciation; solid solution; Richmond mine; California;
D O I
10.2113/gscanmin.43.4.1225
中图分类号
P57 [矿物学];
学科分类号
070901 ;
摘要
Jarosite-group minerals accumulate in the form of stalactites and fine-grained mud on massive pyrite in the D drift of the Richmond mine, Iron Mountain, California. Water samples were collected by placing beakers under the dripping stalactites and by extracting pore water from the mud using a centrifuge. The water is rich in Fell and SO42-, with a pH of approximately 2.1, which is significantly higher than the extremely acidic waters found elsewhere in the mine. Electron-microprobe analysis and X-ray mapping indicate that the small crystals (< 10 mu m in diameter) are compositionally zoned with respect to Na and K, and include hydronium jarosite corresponding to the formula (H3O)(0.6)K0.3Na0.1Fe33+(SO4)(2)(OH)(6). The proton-microprobe analyses indicate that the jarosite-group minerals contain significant amounts of As, Pb and Zn, and minor levels of Bi, Rb, Sb, Se, Sn and Sr. Speciation modeling indicates that the drip waters are supersaturated with respect to jarosite-group minerals. The expected range in composition of jarosite-group solid-solution in equilibrium with the pore water extracted from the mud was found to be consistent with the observed range in composition.
引用
收藏
页码:1225 / 1242
页数:18
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