the role of biofilm on the long-term performance of a shallow...
TRANSCRIPT
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The role of biofilm on the long-term performance of a shallow water cover to limit reactive tailings oxidation and
metal mobilisation.
Bernard Vigneault*, Y.T. John Kwong*
and Lesley Warren╪
*Environment Group, CANMET-MMSL╪McMaster University
For 15th Annual BC MEND Workshop, Vancouver, December 3 and 4 2008
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Current study
Louvicourt Mine Experimental Cells• Constructed in 1996 to study the performance of shallow water coverto limit oxidation of reactive tailings
• 21 m x 21 m
• 3 m of mine tailings
• 0.3 m water cover
• First geochemical field studyconducted from 1996 to 1999 (MEND project 2.12.1, report published in 2002)
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Louvicourt Mine Experimental Cells
• Current study, initiated 7 years after the last measurements
• Cells decommissioned in 2005
July 2005 August 2005
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Biofilm
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Project Objectives•To assess the long-term performance of the shallow water cover by determining porewaterchemistry and submerged tailings geochemistry nine years after disposal.
•To provide additional information on the role and impacts of the fully established periphyton layer at the tailings–water interface and on observable changes in geochemistry and mineralogy of the submerged tailings.
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Methodological Approach
Sampling and porewater analysis• Electrochemical micro-profiles• Interstitial water profiles
Biofilm/Tailings Analysis• Core sampling and extrusion• Sequential extraction analysis• Mineralogical analysis (SEM-EDX)• Molecular biological analysis
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Micro-Profiles – O2
Dissolved oxygen (µM)
0 100 200 300 400 500 600 700
Dep
th (m
m)
-20
-15
-10
-5
0
5
10
15
5700 Lux 18500 Lux >20000 Lux
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Micro-Profiles - pH
pH
6.5 7.0 7.5 8.0 8.5 9.0 9.5 10.0 10.5
Dep
th (m
m)
-30
-20
-10
0
10
20
>20000 Lux5700 Lux 18500 Lux
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Porewater
-6
-4
-2
0
2
4
[ ] (µg · L-1)
0.0 0.1 0.2 0.3 0.4-6
-4
-2
0
2
4
0 10 20 30 40
Dep
th (c
m)
-6
-4
-2
0
2
4
Copper
Zinc
Cadmium
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Cu Zn Cd
Diff
usiv
e flu
x to
the
wat
er c
over
(m
ol ·
cm-2
· s-1
)
10-19
10-18
10-17
10-16
10-15
10-14
1998 2005
No flux
Porewater - Metal Fluxes
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Core Extrusion
biofilm
4.5 – 5.0 cm of tailings
0 - 0.5 cm of tailings
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Total Concentrations (2005)
MetalCu Cd Zn
Tota
l con
cent
ratio
ns
(mg
· kg-
1 )
1
10
100
1000
10000
Biofilm 0 - 0.5 cm (tailings) 4.5 - 5.0 cm (tailings)
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Seq. Ext. – First 0.5 cm of TailingsCu - 1996 Cu - 2005
Cd - 1996 Cd - 2005
Zn - 1996 Zn - 2005
MgCl2CH3COOH (pH 5)NH2OH-HClNH2OH-HCl at 96 °CH2O2HF, HNO3 and HClO4
Cu
Cd
Zn
Most labile
Least labile
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Mineralogical ObservationsIncreasing abundance of sulfides with depth but well crystalline pyrite persists at tailings-water interface
(C2: 0-0.5 cm)
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Molecular Biological Analysis
26%
33%
26%
4%
4%7%
unknown function
methanogenic consortium;lithotrophs, anaerobic NH4oxidationPhototrophs
chemoorganoheterotrophs
grazer
fungus-decomposer
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Does the biofilm affect metal toxicity of discharged water?
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Assessing the Biological Impacts of Submerged Tailings
• Update of the MEND literature review conducted in 1993
• Methods reviewed included the Biotic Ligand Model for the prediction of metal toxicity in water
• The BLM approach allows prediction of acute toxicity of several metals within a factor of 2 to 3.
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Biotic ligands
Ca2+
Na+Mg2+
H+
interactions at toxic binding sites
reactions with dissolved ligands
cationic competitioncomplexation
Lorg. = DOC (FA and HA)
Linorg. = Cl-, SO42-, HCO3
-…
Mez+
Ligands
The Biotic Ligand Model approachProtective effect of DOC derived from the biofilmin the Louvicourt water cover?
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[ ] (mg · L-1)
10 15 20 25 30 35 40
Dep
th (c
m)
-6
-4
-2
0
2
4DOC
Water Cover: DOC Profiles
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Effect Ratio Rainbow trout = Toxicity with DOCToxicity without DOC
(also for Daphnia magna or Ceriodaphnia dubia)
• Hydroqual BLM used to predict median lethal concentrations (LC50)•The final effect ratio is the geometric mean of the effect ratios (CCME 2005).
Water Cover: DOC Protective Effect
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Water Cover: DOC Protective Effect
Copper Zinc Cadmium
DO
C E
ffect
Rat
io
0
5
10
15
20
25
30
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Water Cover: DOC Protective Effect
Cu Zn Cd
Con
cent
ratio
ns (µ
g · L
-1)
0.001
0.01
0.1
1
10
100
1000
EstimatedWQG (CCME 2006)Site Specific WQG
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Conclusions• The system had not reached equilibrium after nine years of operation.
• Mobilisation of trace metals occurred at the tailings surface but the overlying biofilm effectively trapped the released metals.
• Given the water volume in the actual tailings pond the observed Cu, Cd and Zn fluxes would not lead to exceedance of water-quality guidelines.
• Biofilm development on submerged tailings isgenerally beneficial for the application of water covers.
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Future WorkBiofilms has a key component of shallow water cover tailings disposal:
• At Louvicourt, the conditions in the actual tailings impoundment might differ from the experimental cells
• Biofilms have likely developed at other sites with shallow water covers
• Can biofilm be used as tool ?
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Acknowledgements• John Chaulk (CANMET-MMSL)
• Teck (formerly Aur Resources)
• INRS-ETE
• Mine Environment Neutral Drainage (MEND) Program
• Mining Association of Canada
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Summary of Observations• O2 is limited to the first -0.5 mm to -1.4 mm of the biofilm/tailings with concentration affected by photosynthesis.
• pH is locally elevated near the tailings/water interface due tophotosynthesis.
• Fluxes for Zn and Cd to the overlying water are 10x lower than those obtained 7 years ago but the tailings have becomea source of Cu to the overlying water.
• Between 1996 and 2005, there is a notable reduction in H2O2-oxidizable Cu, Cd and Zn (presumably as sulfides) in the surface tailings and the amount of Zn in the more labile fractions has significantly decreased while that for Cd has slightly increased.
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Summary Observations (cont.)• Sulfide abundance increases with depth but well crystalline pyrite persists at tailings-water interface.
• There is evidence of galvanic interaction among the prevailing sulfides which could explain the efflux of Cu observed in 2005.
• The biofilm and associated tailings & Fe-oxyhydroxidehave elevated metal concentrations.
• The biofilm was a highly dynamic system in terms of vertical distribution and temporal variation.
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Evidence of Galvanic Interaction
pysp
ank
(C2: 4.5-5.5 cm)
- Note that Cu is also widespread among the sulfide phases- This could explain the efflux of Cu undetected previously