Microbial populations associated with the generation and treatment of acid mine drainage

被引:91
作者
Benner, SG [1 ]
Gould, WD
Blowes, DW
机构
[1] Univ Waterloo, Dept Earth Sci, Waterloo, ON N2L 3G1, Canada
[2] Nat Resources Canada, CANMET, Ottawa, ON K1A 0G1, Canada
关键词
microbial populations; acid mine drainage; SRB;
D O I
10.1016/S0009-2541(00)00219-9
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
Bacterial populations and water chemistry were profiled throughout the groundwater flow system associated with the Nickel Rim mine tailings impoundment Ontario, Canada. Groundwater containing high concentrations of sulfate (2000-12,000 mg/l) and iron (500-4000 mg/l) flows from the tailings into an adjacent aquifer, A portion of the plume then discharges to the surface where ferrous iron is oxidized creating low pH (pH < 3) conditions. The remaining groundwater passes through a permeable reactive barrier which induces sulfate reduction and metal sulfide precipitation. Elevated populations of iron-oxidizing bacteria (IOB) and sulfur-oxidizing bacteria (SOB) are restricted to hydrologically defined zones of recharge and discharge. Sulfur oxidizers are highest in the tailings (1.27 X 10(3) most probable number (MPN)/g) where sulfide minerals an exposed to oxygen and oxygen-rich recharge water. IOB were highest (9.56 X 10(5) MPN/g) where tailings-derived effluent, rich in Fe(II), discharges to the aerobic surface water environment. Populations of both iron and SOB bacteria in the zone of active oxidation are low compared to those found at other, less mature, tailing sites. Active oxidation in the Nickel Rim tailings is occurring immediately above the water table where the water content is high. The high water content limits oxygen ingress acid sulfide oxidation, and the associated populations of oxidizing bacteria are low. Populations of sulfate-reducing bacteria (SRB) are elevated in the tailings and in portions of the down-gradient aquifer where organic carbon concentrations are high. The highest population (3.73 X 10(7) MPN/g) of SRB were found where sulfate-bearing water migrates through the organic carbon-rich permeable reactive barrier. At locations with high populations of SRB, elevated populations of SOB were also found, suggesting SOB in these zones are metabolizing the reduced sulfur species produced by the SRB in adjacent, but disparate, redox microenvironments. (C) 2000 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:435 / 448
页数:14
相关论文
共 23 条
[1]  
ALEXANDER M, 1965, METHODS SOIL ANAL, V2, P1467
[2]   Modelling of sulfide oxidation with reactive transport at a mine drainage site [J].
Bain, JG ;
Blowes, DW ;
Robertson, WD ;
Frind, EO .
JOURNAL OF CONTAMINANT HYDROLOGY, 2000, 41 (1-2) :23-47
[3]  
BAIN JG, 1996, THESIS U WATERLOO WA
[4]   Geochemistry of a permeable reactive barrier for metals and acid mine drainage [J].
Benner, SG ;
Blowes, DW ;
Gould, WD ;
Herbert, RB ;
Ptacek, CJ .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 1999, 33 (16) :2793-2799
[5]   A full-scale porous reactive wall for prevention of acid mine drainage [J].
Benner, SG ;
Blowes, DW ;
Ptacek, CJ .
GROUND WATER MONITORING AND REMEDIATION, 1997, 17 (04) :99-107
[6]   Geochemical, mineralogical and microbiological characterization of a sulphide-bearing carbonate-rich gold-mine tailings impoundment, Joutel, Quebec [J].
Blowes, DW ;
Jambor, JL ;
Hanton-Fong, CJ ;
Lortie, L ;
Gould, WD .
APPLIED GEOCHEMISTRY, 1998, 13 (06) :687-705
[7]   MICROBIOLOGICAL, CHEMICAL, AND MINERALOGICAL CHARACTERIZATION OF THE KIDD-CREEK MINE TAILINGS IMPOUNDMENT, TIMMINS AREA, ONTARIO [J].
BLOWES, DW ;
AL, T ;
LORTIE, L ;
GOULD, WD ;
JAMBOR, JL .
GEOMICROBIOLOGY JOURNAL, 1995, 13 (01) :13-31
[8]   GEOCHEMICAL EVOLUTION OF INACTIVE PYRITIC TAILINGS IN THE ELLIOT LAKE URANIUM DISTRICT [J].
DUBROVSKY, NM ;
CHERRY, JA ;
REARDON, EJ ;
VIVYURKA, AJ .
CANADIAN GEOTECHNICAL JOURNAL, 1985, 22 (01) :110-128
[9]   Microbial sulfate reduction within sulfidic mine tailings: Formation of diagenetic Fe sulfides [J].
Fortin, D ;
Beveridge, TJ .
GEOMICROBIOLOGY JOURNAL, 1997, 14 (01) :1-21
[10]  
Fortin D, 1996, FEMS MICROBIOL ECOL, V21, P11