Title: Fate and Transport of Contaminants from Acid Mine Drainage
1Fate and Transport of Contaminants from Acid Mine
Drainage
- US EPA Scientist-to-Scientist Meeting
- Las Vegas, NV
- June 14-15, 2000
- Richard T. Wilkin, Ph.D.
- National Risk Management Research Laboratory
- Ada, OK
2Fate Transport Issues
- Chemical, Physical, and Biological Processes from
Source gt - Media Type
- Air, Water, Sediment
- Metal Type
- Geochemical, Toxicity, Ore association
3Chemical Processes
- Dissolution, sorption, nucleation, growth
- Oxidation-Reduction reactions
- Acid-Base reactions
- Isotope exchange reactions
- Modeling exercises
- Chemical Speciation
- Saturation DGr RT lnQ/Keq
- Kinetics
4Physical Biological Processes
- Transport
- Water
- Sediment
- Wind
- Microbial
- S-oxidizers, Fe-oxidizers
- S-reducers, Fe-reducers
- Wetland Plants
5Metals
Hg, Pb
As, Se Cd, Sb, Ag, CN Cu, Zn Pb, U Cr, Fe Hg
6Metal Type Pearson Classification
7As Mobility/Speciation Redox
sw
gw
8Metal Mobility pH
Supersat.
solution
9Fate Transport Topics
- Kinetics/Mechanisms of S(-II) oxidation
- Microbial Processes
- Product Transport in Surface Waters
- Product Transport/Storage in Sediments
- Impact of ARD on Ground Waters
- Wetlands
- Supergene Processes
10Pyrite Oxidation
Pyrite Dissolution/Overall Reaction FeS2
15/4O2 7/2H2O Fe(OH)3 2H2SO4
Low pH, high acidity Metal rich As, Sb, Zn,
Cu Fe, Al, Mn rich Sulfate rich
11Pyrite Oxidation II
FeS2 7/2O2 H2O Fe2 2SO42- 2H FeS2
14Fe3 8H2O 15Fe2 2SO42- 16H
after Stumm and Singer (1980)
12Pyrite oxidation kinetics
After Langmuir (1996) using rate equations
from Williamson Rimstidt (1994), PyArea0.05
m2/g
13Pyrite Oxidation III
- Chemical
- oxygen, Fe(III), water, buffering
- Physical
- texture, grain size
- Ore processing, framboidal pyrite
- Biological
- Fe- and S-oxidizing bacteria
14AMD Prediction(EPA 530-R-4-036, December 1994)
- Assessment of Acid-generation and
Acid-neutralization capacity (acid, sulfate) - Hydrologic Assessment Availability of Oxygen and
Water (acid, sulfate) - Ore Deposit/Waste rock/Tailings Characterization
(metals)
15Ore Deposit Types
- Volcanic-hosted Massive Sulfides
- Sediment-hosted Massive Sulfides
- - Shale Type (Rammelsberg)
- - Carbonate Type (MVT)
- Mafic Intrusive Related (Sudbury, Duluth Complex)
- Porphyry Cu-Mo/Skarn
- Mesothermal Au
- Epithermal Au
- Carlin Type Au
- Continental Geothermal (Hg, As, Sb)
- Coals
16Ore Minerals Metal Mobilization
Sources from Metal Sulfides Fe - pyrite,
marcasite, pyrrhotite Hg - cinnabar Pb
galena Ag acanthite, galena As arsenopyrite,
As-rich pyrite, orpiment, tetrahedrite,
enargite Ni pentlandite, millerite Cu
covellite, chalcocite, djurleite, bornite,
chalcopyrite, enargite Cd greenockite Zn
spahlerite Co cobaltite
17Transport of OxidationProducts to Surface Waters
Sorption trend onto Fe ppt PbgtHggtAggtAsgtNigtCugtCdgtZn
18Wetland Processes
Other ORD work at SPRD T. Canfield et
al. Constructed Wetlands
19ARD-Ground Water Interactions
20ARD-Groundwater Interactions
21AMD Related Secondary Precipitates
pKsp
Alunite KAl3(SO4)2(OH)6 84 Anglesite PbSO4 7
.8 Anhydrite CaSO4 4.4 Coquimbite Fe2(SO4)39H
2O 3.6 Gibbsite Al(OH)3 33.9 Goethite FeOOH
24 Jarosite KFe3(SO4)2(OH)6 95 Melanterite FeS
O47H2O 2.2 Schwertmannite Fe(III), Fe(II)OH
SO4 ? Sulfur S8
22Ground Water/Anoxic LimestoneDrains
High Fe(II)/Fe(III) pH 2-6, low O2 Al, Metals
GW
Surface
High O2 Fe(II)gtFe(III) Fe(OH)3 ppt alk takes up
acid
Limestone Drain
- Calcite dissolution
- Alkalinity production
- Retain Anoxic (FeII/FeIII)
- pH increase