1 / 23

Geology, Mining, and Water Quality

Geology, Mining, and Water Quality. by Matthew A. Sares. Acid Mine Drainage. Water - from rain and snowmelt + Oxygen - from the air + Pyrite - from the mine Reaction = Sulfuric Acid. Sources of Acid Mine Drainage (AMD). Mine Effluent. Burbank Mine, San Juan Co. Mine Dump.

steins
Download Presentation

Geology, Mining, and Water Quality

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript

  1. Geology, Mining, and Water Quality by Matthew A. Sares

  2. Acid Mine Drainage Water - from rain and snowmelt + Oxygen - from the air + Pyrite- from the mine Reaction = Sulfuric Acid

  3. Sources of Acid Mine Drainage (AMD) • Mine Effluent Burbank Mine, San Juan Co.

  4. Mine Dump • Mill Tailings Lewis Mine and Mill, San Miguel Co.

  5. Fe2+ + 2SO4 +2H+ Reaction 1: FeS2(s) + H2O + 7/2O2 Fe(OH)3(s) + 3H+ Reaction 4: Fe3+ + 3H2O THE CHEMISTRY ofACID MINE DRAINAGE pyrite water sulfate acid Reaction 2:* Fe2+ + 1/4O2 +H+ Fe3+ + 1/2H2O Reaction 3: FeS2(s)+ 8H2O + 14Fe3+ 15Fe2+ + 2SO4 + 16H+ * catalyzed by bacteria

  6. Background Water Quality Lewis Mine and Mill, San Miguel Co.

  7. Fe2+ + 2SO4 +2H+ Reaction 1: FeS2(s) + H2O + 7/2O2 Fe(OH)3(s) + 3H+ Reaction 4: Fe3+ + 3H2O THE CHEMISTRY ofACID MINE ROCK DRAINAGE pyrite water sulfate acid Reaction 2:* Fe2+ + 1/4O2 +H+ Fe3+ + 1/2H2O Reaction 3: FeS2(s)+ 8H2O + 14Fe3+ 15Fe2+ + 2SO4 + 16H+ * catalyzed by bacteria

  8. Acid Rock Drainage (ARD) sources: • Abandoned mines • Natural springs and drainages in hydrothermally altered areas

  9. Hydrothermal alteration is a process whereby hot water circulating within the earth changes the composition of rocks. Intensely altered rocks have yellow, orange, and red colors from the oxidation of iron in pyrite. East Mancos River headwaters, Montezuma Co.

  10. Hydrothermal Alteration Feldspars >> Clays Iron and Sulfur >> Pyrite (mod. from Guilbert and Park, 1986)

  11. A number of streams in eleven different headwater areas of Colorado have naturally high concentrations of metals and/or acidity, upstreamof any significant human impacts. Rocks in these areas have been affected by intense “hydrothermal alteration” in the geologic past.

  12. Red Cone, Park Co.

  13. Springs Red Mountain, Chaffee and Pitkin Co.

  14. Natural acid rock drainage dissolves metals present in the rock, affecting downstream water quality. PEEKABOO GULCH SPRING pH=2.17, conductance=2470 µS, Q=25 gpm 1,724 x Al Cd 42 x Cu 164 x Fe 100 x Mn Constituent Pb Ag 6 x Zn 21 x SO4 6 x 1 10 100 1000 10000 Factor Above Aquatic Life Standard

  15. Lookout Mountain, Conejos Co.

  16. Ferrosinter deposits are characteristic of springs in hydrothermally altered areas. Iron Creek Lower Spring, Conejos Co.

  17. Some hydrothermally altered areas have high rates of erosion, and are prone to debris flows and landslides because bedrock has been weakened. Alum Creek, Conejos Co. Headwall Slide Red Mountain #2, Ouray Co.

  18. Slumgullion landslide is in an area of hydrothermally altered rock. Movement and erosion continually expose acid-producing minerals. Drainage from the slide area is very acidic (pH  3.4). Headwall Slumgullion Landslide near Lake City, Mineral Co.

  19. Conclusions • Acid rock drainage is generated at mines and naturally where sulfide minerals are present and the buffering capacity of the water is exceeded. • AMD degradation can be acute because: • 1) Mines act as collectors of groundwater • 2) Water is in contact with high grade ore minerals • 3) Mine dumps and tailings provide dramatically increased surface areas for the interaction of water, oxygen, and sulfide minerals.

  20. Conclusions • Natural ARD is important in areas of intense hydrothermal alteration because: • 1) Rocks contain disseminated sulfide minerals. • 2) Rocks are depleted of buffering minerals. • 3) Large volumes of rock are affected. • Both ARD sources must be characterized to determine realistic remediation goals.

More Related