alkaline industrial waters and wetlands: prospects for ... industrial waters and wetlands: prospects...
TRANSCRIPT
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Alkaline industrial waters and wetlands:
prospects for effective treatment
Will Mayes1 & Jon Aumônier 2
1 Centre for Environmental and Marine Sciences, University of Hull, YO11 3AZ
2 Mineral Industry Research Organisation
• Successful programme of treating abandoned mine waters
• Circum-neutral pH, high Fe concentrations
Treatment wetlands and post-industrial pollution
Taff Merthyr coal mine treatment scheme, S. Wales
>50 full scale coal mine water treatment schemes
in UK, many incorporating wetlands;
>2000 tonnes Fe year prevented from stream
discharge
Inflow
Outflow
Gravel
substrate
Aerobic wetlands: shallow water planted with
reeds / rushes; enhances Fe settlement; residual
Fe uptake
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• Weathering of lime-rich residues produced in major global
industries: e.g. steel slags, fly ash, lime spoil, C&D waste,
Solvay Process waste
• CaO hydrolyzes and liberates OH- in solution
Ca(OH)2 → Ca2+ + 2OH-
• NaOH-derived alkalinity at some sites: Bayer Process sources
Alkaline leachates - sources
• High rates of calcite (CaCO3) precipitation as waters take in atmospheric CO2
Ca2+ + CO32- → CaCO3
• Potential elevation of trace elements – e.g. As, Cr, Se, V
• V potentially a key issue given pentavalent form prevails
Extremely alkaline waters
Drainage from a
former lime works at
Harpur Hill near
Buxton, UK
The Dene Burn
downstream of the
former Consett
Steelworks, UK
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• Acid dosing, recirculation of waters over spoil, aeration
• Requires sustained capital input
• Not usually suitable beyond economic life of workings
Conventional Management
F&N Hawley Award for Environmental Engineering, September 2007
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pH
Dene BurnHowden Burn
Workings closureWater pH in two
streams draining the
former Consett
Steelworks, Co. Durham,
UK
Statutory surface water
quality limit
Mayes et al. (2008). Water
Air Soil Pollut. 195: 39-40.
Natural wetland at Thrislington Limeworks, Co. Durham
The basis for treatment wetlands
• ‘Volunteer’ wetlands
• pH 12 lime spoil leachate
• pH 12 steel slag leachate
• Calcite precipitation from mass balance and direct measurement using immersed limestone blocks
Environ. Sci. & Technol. (2006)
40: 1237-1243
0 100 200 metres
Leachate
source zone
Pond
Wetland flow
zone
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2
4
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Culvert
Base of slag heaps
Base of slag
heaps
Extent of
wetland area
Sample location
Stream
Slag heap base
Hownsgill
Valley, Consett
Wetland extent
Flow
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Volunteer wetlands
• Precipitation rates between 0.8 and 9.9 g/day/m2 of wetland area from limestone blocks
• Rates from mass balance varied between 1.7 and 13.6 g/d/m2 of wetland area
• Highest rates coincide with areas where vegetation/algae begin to establish
• Infers importance of biological activity in enhancing removal
SOURCE LAGOON WETLAND
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2 3 4 5 6Site
pH
pH
Median pH values during study period. Y
error bars show range, n = 30 for each.
• Sufficient removal for economically viable wetland sizes (~50m2
and 14000m2 for 12 monitored discharges in UK)Mayes et al. (2006). Environ.
Sci. Technol. 40: 1237-1243
Pilot constructed wetland - Redcar
Mayes et al. (2009). Water
Sci. Technol. 59: 2253-2263.
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• Brackish coastal setting
• Two leachate sources: input increases alkalinity (>1500mg/L as CaCO3), pH (>12) and Ca2+ (>600mg/L)
• CM2: Pilot CW sized by CaCO3 removal rates from volunteer system
• CM3: Monitored through natural wetland
• Much improved flow rate measurements
Pilot constructed wetland - Redcar
pH E.C. Alk Ca Mg Na Cl SO4 Fe Al Sr
CM1 8.2 2203 250 40 9 316 375 138 0.9 0.3 0.3
CM2 11.9 2203 664 80 0.4 284 326 59 0.3 0.4 0.4
CM3 12.4 7879 1930 601 0.1 258 116 52 0.5 0.5 2.2
Typical water quality composition of upstream reference site (CM1), and leachate source areas (CM2, CM3). All
values mg/L except pH, electrical conductivity (‘E.C’: μS/cm2), total alkalinity (‘Alk’: mg/L as CaCO3)
• PVC liner, 0.2m indigenous boulder clay
• Transplantation of Phragmites australis (Common Reed)
• Low flow rate – suitable for pilot testing
• Flow monitoring through 90o V-notch, tracer tests
Pilot constructed wetland
MARCH 2008 SEPTEMBER 2008
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• No ‘honeymoon period’ - modest decline in pH
• Improved performance over time
Early performance
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pH
pH IN Cell 1pH OUT Cell 1
• Alkalinity removal efficiency
Performance and metrics
% Total Alkalinity removal: CELL 1
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Trea
tme
nt E
ffic
ienc
y (%
)
% Total Alkalinity removal: CELL 1
Alkalinity removal to
reach background
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• Potential mechanisms:
– increased precipitation
nuclei: emergent plants
and micro-organisms /
debris
– increased microbial
activity
– Hydraulic efficiency
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0 200 400 600 800 1000
Ca2+ IN (mg/L)
CaC
O3 r
emo
val (
g/m
2/d
ay)
Seasonality
Consett winter Coatham winter
Coatham growing
season
Consett growing
season
Constructed
wetland
Natural wetland
Mayes et al. (2009). Water
Sci. Technol. 59: 2253-2263.
• Alkaliphilic bacteria shown to be present in many hyperalkaline settings
• Cultures used in treatment of alkaline pulp and textile waste
• Acid generation processes:
– Carbohydrate degradation: e.g. glucose metabolised to gluconic acid
• Scope for developing cultures to use in wetlands?
Microbially-mediated bufferingBurke et al. (2012). Geomicrobiol. J.
in press.
Kumar et al. (2011) World Academy
of Science, 76: 503-506
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• Lab tests using water and substrate from Coatham
Controlling mechanisms
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pH
CTRL CTRL_SSED1 SED1_S
Above pH~12: OH-
predominates
pH 10.3-12: CO32-
predominates
pH 6.4-10.3: HCO3- predominates
~7 days
~14 days
• Leachate buffering
~50% more rapid
when in contact
with wetland
substrate than
atmospheric CO2
transfer
• Good evidence of
importance of
microbial
processes
• Most trace elements below detection limits in water (e.g. Cd, Co, Pb, Se). Some Ni lost across wetland.
• Calcite-dominated secondary precipitates
• Supersaturation with a range of phases (e.g. CaCO3, SrCO3, Ni(OH)2
and a range of Fe and Al oxyhydroxides)
Trace elements
CM2 CM3 SC1Ca 373700 390800 264350Mg 817 767 7781Fe 16701 7326 8144Al 2457 2976 2451Ba 70 66 130Cr 10 15 12Cu 3 3 7Mn 2545 2370 7199Ni 6.4 4.4 7Sr 6216 3542 2785V 17 15 44Zn 41 51 70 Composition of digested secondary precipitates. Selected
elements in mg/kg.
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• Scunthorpe, Yarborough Landfill, constructed in Spring 2012; area ~1600m2
• Batch flow system – currently pumped from borehole
• Better residence time estimates for constraining alkalinity / Ca removal rates
• Aughinish, Ireland: trial cell for red mud leachate: 2012
Larger trial systems
• Increasing evidence of efficacy of wetlands for alkaline waters
• Some removal of trace metals in wetland through uptake in
secondary calcite precipitates
• More empirical data: robust sizing estimates for full scale
• Improved mechanistic understanding – process rates /
modelling; biotic / abiotic processes
Conclusions