Geochemical and biological aspects of sulfide mineral dissolution: lessons from Iron Mountain, California

被引：102

作者：

Edwards, KJ

Bond, PL

Druschel, GK

McGuire, MM

Hamers, RJ

Banfield, JF

机构：

[1] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, McLean lab, Falmouth, MA 02543 USA

[2] Univ Wisconsin, Dept Geol & Geophys, Madison, WI 53706 USA

[3] Univ Wisconsin, Dept Chem, Madison, WI 53706 USA

来源：

CHEMICAL GEOLOGY | 2000年 / 169卷 / 3-4期

关键词：

acid mine drainage; pyrite; sulfide dissolution; microorganisms;

D O I：

10.1016/S0009-2541(00)00216-3

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 oxidative dissolution of sulfide minerals leading to acid mine drainage (AMD) involves a complex interplay between microorganisms, solutions, and mineral surfaces. Consequently, models that link molecular level reactions and the microbial communities that mediate them to field scale processes are few. Here we provide a mini-review of laboratory and field-based studies concerning the chemical, microbial, and kinetic aspects of sulfide mineral dissolution and generation of AMD at the Richmond ore body at Iron Mountain, California. (C) 2000 Elsevier Science B.V. All rights reserved.

引用

页码：383 / 397

页数：15

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