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Metal Loading in Peru Creek
  • By:  Brendan Cusick
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Peru Creek Info
  • Summit County, Colorado.
  • Near Keystone Ski Resort
  • 8km in length and feeds into the Snake River.
  • About 27-51% of total flow for the Snake River.
  • Many mining catchments located within the watershed.
  • Elevation about 10,500ft.


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Importance
  • For remediation of Peru Creek it is imperative to locate the major sources of contamination.
  • Money has already been spent to clean up around Pennsylvania Mine.
  • Pennsylvania Mine found to be one of the smaller contributors of contamination.
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Source of Metal Loading
  • Caused by mines.
  • Process called Acid Rock Drainage (ARD).
  • Over 1900km of streams, rivers and lakes, in Colorado, are affected by ARD.




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Causes of ARD
  • Atmospheric oxidation of iron-sulfur minerals (FeS2).
  • Minerals usually isolated from the atmosphere, come in contact with atmosphere.
  • Runoff from tailings piles and drainage from adits are highly acidic and highly concentrated with metals.
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Reactions in ARD
  • 1) 2 FeS2 + 7 O2 + 2 H2O = 2 Fe2+ + 4 SO42- + 4 H+
  • Pyrite + Oxygen + Water = Ferrous Iron + Sulfate + Acidity
  • 2) 4 Fe2+ + O2 + 4 H+ = 4 Fe3+ + 2 H2O
  • Ferrous Iron + Oxygen + Acidity = Ferric Iron + Water
  • 3) 4 Fe3+ + 12 H2O = 4 Fe(OH)3 ¯ + 12 H+
  • Ferric Iron + Water = Ferric Hydroxide + Acidity
  • 4) FeS2 + 14 Fe3+ + 8 H2O = 15 Fe 2+ + 2 SO42- + 16 H+
  • Pyrite + Ferric Iron + Water = Ferrous Iron + Sulfate + Acidity
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Effects of ARD
  • Lowered pH in the tailings and adits leads to and increase in dissolved metals.
  • Mixes with the receiving waters creating a lowered pH and higher metal concentrations.
  • Low enough pH and high enough metal concentration kills aquatic life.


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Basis for my project
  • Sabre Duren’s Master thesis.
  • Tracer coupled with synoptic sampling.
  • Covered 7 km stretch of Peru Creek.
  • Attempted to locate the major area of metal loading along Peru Creek.
  • Took place August of 2002.
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Basis for My Project
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My Project
  • Tracer experiment coupled with synoptic sampling.
  • 6 sampling sites from below the wetlands to just below Warden Gulch.
  • From injection point to site #6, 1.3km.
  • Injection lasted 3 hours, from 10:45-13:45.
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My Project
  • Took place July 10, 2004.
  • LiCl used as the conservative substance.
  • Sampled for Fe, Zn, Li, Cl, DOC.
  • Flow, pH, conductivity, and temperature were taken on site.
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Field Methods
  • Samples
    • Li, taken directly from stream every 5 minutes during rising and falling limbs, and every 15 in-between.
    • Fe, Zn, and Cl, taken every half hour and filtered.
    • DOC, taken every hour.

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Field Methods
  • Readings
    • Flow, taken at beginning and end of experiment with pygmy meter.
    • pH, Conductivity, and Temperature, taken throughout the day with hand-held pH/Conductivity probe.
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Analysis
  • Li and Zn;  Atomic Absorption Spectrometer.
  • Fe;  UV Vis.
  • DOC;  Total Organic Carbon Analyzer.
  • Cl;  Ion Chromatograph.


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Calculations
  • Li    Flow
    • Inj. Rate (L/s) * Inj. Li Conc. (mg/L) = Set Flux (mg/s)
    • Set Flux (mg/s) / Site’s Avg. Plateau Li Conc. (mg/L) = Site’s Flow (L/s)
  • Fe / Zn Flux
    • Site’s Flow (L/s) * Site’s Fe or Zn Conc. (mg/L)
    • = Site’s Fe or Zn Flux (mg/s)


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Calculations
  • % Loading From Sites 1-6
    • (Site’s Flux (mg/s) / Sum of Flux for Sites 1-6 (mg/s)) *100
    • = % Loading From Sites 1-6
    • If sites Flux <0, then it was not considered for loading calculations.
  • % Loading For Entire Stream
    • % Loading From Sites 1-6 * August 2002 values of Loading for the Warden Gulch Reach = % Loading For Entire Stream



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Results
  • An inflow between sites 2 and 3 was found to be a major cause of the metal loading and pH drop associated with this stretch of Peru Creek.
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pH
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Conductivity
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DOC vs. Dist. Downstream
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Flow vs. Dist. Downstream
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Li Conc. vs. Dist. Downstream
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Fe vs. Dist Downstream
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Zn vs. Dist. Downstream
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Sites 1 and 2 LiCl Variability
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Sites 3 and 4 LiCl Variability
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Sites 5 and 6 LiCl Variability
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Results
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Conclusions
  • Inflow, major source of contamination.  Better place for remediation to occur.
  • Between Sites 2 and 3, there is also some unaccounted flux of Fe and Zn.  Possibly due to ground water inflow.
  • Between Sites 1 and 2, there is a high loading of Fe. Possibly due to ground water inflow.
  • If Sites 1-4 cleaned up, about 70% of Fe and 40% of Zn loading could be dealt with.


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Special Thanks
  • Advisor:  Diane McKnight
  • Grad Students:  Marcie Appel
  •                             Chris Jaros
  •                             Sabre Duren
  • REU participants (plus Pete)
  • Math/Bio program
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References
  • Interstate Mining Compact Commission (IMCC), 1992. Inactive and Abandoned Non-Coal Mines: a Scoping Study. Prepared for IMCC of Herndon, VA by Resource Management Associates, Clancy, MT. Cooperative Agreement, X-817900-01-0.


  • Duren, S., 2002. Quantitative Hydrologic Evaluation of Dissolves Metal Loading and Transport in Peru Creek, an Acid Rock Drainage Stream; Summit County, Colorado. University of Colorado at Boulder, p130.
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Questions
  • ?