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Mine Water and the Environment

, Volume 25, Issue 2, pp 86–92 | Cite as

Summary of Deepwater Sediment/Pore Water Characterization for the Metal-laden Berkeley Pit Lake in Butte, Montana

  • Larry G. TwidwellEmail author
  • Christopher H. Gammons
  • Courtney A. Young
  • Richard B. Berg
Technical Article

Abstract.

Unconsolidated sediment at the bottom of the Berkeley pit lake is a mixture of detrital silicate minerals derived from sloughing of the pit walls and secondary minerals precipitated out of the water column. The latter include gypsum and K-rich jarosite. The pore waters have a similar pH to the overlying lake waters (pH 3.1 to 3.4), and have similarly high concentrations of dissolved heavy metals, including Al, Cd, Cu, Mn, Ni, and Zn. Sediment cores show that the top meter of the sediment column is moderately oxidized (jarosite-stable). Petrography, chemical analysis and geochemical modelling all suggest a transformation of poorly crystalline ferric compounds such as schwertmannite and/or ferrihydrite near the sediment surface to jarosite with depth in the core. No evidence of bacterial sulfate reduction was found in this study, despite the presence of 0.3 to 0.4 wt% organic carbon in the pit lake sediment.

Keywords

acid mine drainage characterization geochemistry jarosite pit lake pore water schwertmannite sediment solubility 

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Copyright information

© IMWA Springer-Verlag 2006

Authors and Affiliations

  • Larry G. Twidwell
    • 1
    Email author
  • Christopher H. Gammons
    • 2
  • Courtney A. Young
    • 1
  • Richard B. Berg
    • 3
  1. 1.Dept of Metallurgical and Materials EngMontana TechButte MT 59701USA
  2. 2.Dept of Geological EngMontana TechButte MT
  3. 3.Montana Bureau of Mines and GeologyButte MT

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