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ICGGE 2003 Mike Wireman US EPA Region 8 303-312-6719

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Presentation on theme: "ICGGE 2003 Mike Wireman US EPA Region 8 303-312-6719"— Presentation transcript:

1 ICGGE 2003 Mike Wireman US EPA Region 8 303-312-6719 wireman.mike@epa.gov

2 “Characterizing Ground-Water Flow Paths in High Altitude Fractured Rock Settings Impacted by Mining Activities.” Mike Wireman, U.S. EPA Region 8 Dr. Mark Williams, University of Colorado

3 Chalk Creek Mining District-Collegiate Range, CO

4 Mary Murphy Gold Mine Applied Research Site Research Objectives: * To Develop Tools for Characterization of Site Hydrology and Geochemistry * To Better Understand Role of Ground Water Transport of Metals to Chalk Creek. Remedial Objectives: * To Determine Metals Loading Sources and Pathways * To Reduce Metal Loadings to Chalk Creek Partners: * USGS, USFS, University of Colorado & CDMG

5 Mary Murphy Gold Mine—Applied Research Site Site History Placer Mined in 1860’s-1870: Vein Deposits Located 1883-1893: Period of Greatest Mining Activity Mary Murphy Mine: 1870—1951 * 75% Gold, Silver, Lead, Zinc, Copper * 5 Main Veins * 14 Main Levels * 2200 Vertical Feet * Golf Adit—Drain / Haul Adit * Connected to Iron Chest Mine Remedial Work: * 1991—3 Piles Consolidated 69,000 cu. yds., Golf Tunnel Unplugged, Lined Settling Pond * 1992—Golf Adit Water Rerouted * 1998—1400 Level Opened / Stabilized * 1999—700 Level Partially Opened * 2003—Lady Murphy Adit Opened

6 Mary Murphy Mine Site Environmental Characterization History > Flow Measurements > Steam Tracing 14 Times –1990—2003 > GW Tracing > Metal Loading > Geochemical 5 Times- 1990—1994 Modeling > Sediment Sampling > Hydrometrics / Sept. ’93 & June ’99 Isotopic Research > Water Chemistry > Surficial 17 Times- 1990—2003 Geophysical Work > Toxicity Testing / Fish Data 11 Times- 1991—2003

7 Focus Of This Talk > Metals Loading > Stream & Ground-Water Tracing > Hydrometrics / Isotopic Results

8 Geology and Mine Features Mary Murphy Mine & Vicinity

9 Elements of Conceptual Model Strong GW / SW Interaction > Gaining Streams > Strong Upward Gradient in Valley Bottom Fracture Dominated Flow Paths Multiple GW Flow Systems Many Seeps / Springs Significant Seasonal Variation in Flow and Water Quality ( GW & SW) Several Water Types Chemistry of GW & SW is Strongly Impacted by Geology and Mineralogy of Ore Body, and Mine Features.

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11 Mary Murphy Gold Mine—Chafee County, CO DISSOLVED ZINC CONCENTRATIONS Location Date Conc. (ug/l) GW Wells MM-3 9/93 17,131 MM-3 7/00 15,830 MM-3 2/02 21,500 MM-3 5/03 5,570 MM-11 9/93 188 MM-11 7/00 210 MM-11 7/02 179 MM-11 5/03 560 MM-6 9/93 2605 MM-6 7/02 13,700 MM-6 122,000 MM-15 9/93 45 MM-15 7/02 08

12 Mary Murphy Gold Mine—Chafee County, CO DISSOLVED ZINC CONCENTRATIONS (CONTINUED) Location Date Conc. (ug/l) Chalk Creek CC-0 9/90 < 100 CC-0 7/02 08 CC-6 9/90 420 CC-6 2/02 417 CC-6 5/03 534 CC-7 9/90 18,000 CC-7 7/00 27,710 CC-7 7/02 24,300 CC-7 3,620 CC-7D 9/90 110 CC-7D 7/02 44 CC-7D 5/03 53.2 CC-9 9/90 < 100 CC-9 7/00 118 CC-9 7/02 24 CC-9 5/03 35.2

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16 Scope of Ground-Water Tracing Mary Murphy Mine—Applied Research Site

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20 Results of Ground Water Tracing Mary Murphy Mine

21 Inverse Geochemical Modeling

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25 Variation of Discharge Components Versus Time in 1400 Level. Mary Murphy Gold Mine

26 Isotopic Composition of Waters Mary Murphy Gold Mine

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28 Delta O-18 in Selected Tributary Inflows, 1400 Level Mary Murphy Gold Mine

29 Pre-event Water and Event Water in Total Discharge From 1400 Portal Mary Murphy Gold Mine

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