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A Novel Approach to Control Atmospheric Methane Emissions from Diffused Area Sources and Low-Volume Point Sources J. Patrick A. Hettiaratchi Professor of Environmental Engineering Department of Civil Engineering & CEERE Schulich School of Engineering, University of Calgary May 9, 2008 SWANA BC Chapter GHG from A to Z Workshop Victoria, BC
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Methane as a Greenhouse Gas
GWP over 100-year time-horizon = 23 GWP over 20-year time-horizon = 62 CH4 Atmospheric Lifetime = 12 years (Source: IPCC, 2003) Therefore, controlling methane could potentially provide fairly high near-term global warming benefits than we realize.
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Key Sources of Methane Emissions
Anthropogenic sources account for 60-80% of total emissions Some Anthropogenic Sources: Diffused Sources: Sanitary landfills (about 10% - 20% of global emissions)
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High emissions during waste placement, before closure!
Methane Emissions at Landfills High emissions during waste placement, before closure!
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(Flames from the Abyss)
Hot Spots - Zambisa Landfill (Flames from the Abyss)
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Hot Spots – Effect of Clay Intermediate Covers
X-section along the transverse direction
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Hot Spots “Clear” evidence (at a BC landfill)
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Key Sources of Methane Emissions
Additional Anthropogenic Sources: Low-volume Point Sources: Oil and gas industry (about 15% of global emissions) Flaring/Venting of solution gas and soil gas migration Fugitive emissions and engineered emissions during gas transmission
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CH4 Emissions at Oil Well Sites
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Microbial Techniques to Control Methane Emisisons
Oxidize Methane to Carbon Dioxide Using a Naturally Available Microorganism
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Methanotrophy Oxidation of CH4 to CO2 by methanotrophic bacteria, or “methanotrophs” (Methylomonas methanica)
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Methanotrophy- background
Methanotrophs are aerobic, attached-growth organisms They are naturally found: in paddy fields around gas leaks in landfill cover soils Three types of methanotrophs have been identified; I, II and X
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Methanotrophy- background
Methanotrophs require: Oxygen (could operate at low oxygen) Moisture (optimum MC around 15%) High temp (optimum around 25-35oC) Nutrients (N, P. Carbon source is methane) (Methylomonas methanica)
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Methanotrophy Methanotrophs are naturally occurring bacteria capable
of using methane as a carbon/energy source. They are found in forest soils, landfill cover soils, and around “gas leaking” oil wells/pipes Methanotrophs require: oxygen (can function in micro-oxygen environments), moisture, nutrients, moderate temperature, and a good solid medium Challenge: How to maximize the methane oxidation potential of methanotrophs under field conditions??
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Methanotrophy- Current R & D
Identify optimum conditions for different types of methanotrophs Determine the best granular medium and flux rates (determine oxygen availability) Predict behavior under various conditions (mathematical modeling) Study the effect of by-product formation on environment/methane oxidation (CO2, H2O, heat and EPS) (Methylomonas methanica)
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Moisture Needs of Methanotrophs (very important with compost based Biocaps)
Optimum Moisture Content for Max. Oxidation for Various Soil/Compost Mixtures (data from lab incubation studies)
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Passively-aerated Column Performance
% oxidation vs time in Sedge Peat (average CH4 input = 160 and 320 g m-2 day-1)
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Actively-aerated Column Performance
% oxidation vs time in Compost (average CH4 input = 650 g m-2 day-1)
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Engineering Applications - Current R & D
Provide optimum conditions for methanotroph growth on a continuous basis in field situations Predict field behavior, using Laboratory results Mathematical models Identify the best configurations of Biocaps and MBFs to suit each situation
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Engineering Applications of Methanotrophy
Biocaps at landfills to control diffused sources (Methylomonas methanica) MBF (Methano-Biofilter) to control point emissions in oil/gas industry to oxidize gas collected from landfills (instead of flaring!)
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Type I Biocaps: To control regular emissions from a closed landfill
30-60 cm thick layer of soil with about 5% C content Medium permeability Support vegetation (to increase evapo-transpiration; ET cover) With or without a 30 cm sub-soil layer Oxidize g/m2/d (average flux from a typical landfill is about 100 g/ g/m2/d)
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Biocap Modified Landfill Cover System
Commercial Recovery CO2 emission CH4 & CO2 emission Oxidation in Landfill Cover (Methanotrophs) CH4 & CO2 Generation CH4 & CO2 migration
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CH4 Oxidation in Biocaps: field testing
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East Calgary Landfill Test Cell
Field Measurements: 1. Surface flux 2. Depth Profile: Gas Concentration Temperature Moisture Content Pressure
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Type II Biocaps To control higher emissions (with some “hot spots”)
30-60 cm thick layer of compost/soil (medium permeability) Above a gas distribution layer (high permeability) Support vegetation (to increase evapo-transpiration; ET cover) Oxidize g/m2/d
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Type III Biocaps To control “hot spots”
30-60 cm thick layer of compost/soil (medium permeability) above a thick gas distribution layer (high permeability) Control lateral flow within the gas distribution layer Support vegetation (to increase evapo-transpiration; ET cover) Oxidize g/m2/d (Methylomonas methanica)
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Distribution layer (high k) “Hot Spot” flux (1,200 g/m2/day)
Soil/compost Bio-cap (medium k) 0.6m 400 g/m2/day Distribution layer (high k) “Hot Spot” flux (1,200 g/m2/day)
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Why soil/compost and not compost alone?
Optimum Moisture Content for Max. Oxidation for Various Soil/Compost Mixtures (data from lab incubation studies)
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Type IV Biocaps: Intermediate Thin Biocovers (TBCs)
To control emissions during cell filling 30 cm thick layer of compost/coarse grain medium (high permeability) as intermediate covers Use high permeable material, if the cell is operated as a Bioreactor Open for a short time period Oxidize about g/m2/d (Methylomonas methanica)
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Intermediate TBC at Calgary Biocell (unique “bioreactor landfill”)
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TBCs in Calgary Biocell
CO2 emissions CH4 & CO2 emissions Commercial recovery Oxidation in landfill bio-cover (Methanotrophs) Solid waste-1st lift (5m) Solid waste-2nd lift (5 m) 2nd Intermediate thin biocover (30 cm) 1st Intermediate thin biocover (30 cm) Solid waste-3rd lift (8 m) Final bio-cover GL CH4 & CO2 generation
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1st Intermediate Bio-cover 2nd Intermediate Bio-cover
(80m*80m) 2nd Intermediate Bio-cover (110m*110m)
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Mathano-biofilters (MBFs)
To control “point sources” (could be “hot spots” at landfills) Collect gas from a (small) landfill and oxidize in a MBF. Point sources in oil/gas facilities Typical medium: fully stable compost (Methylomonas methanica)
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Field Scale MBF @ a natural gas metering station
X 35cm Compost Gravel Geotextile Geomembrane Cross section on XX
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Type I MBFs Passively aerated compost or compost/soil MBFs
Bed thickness; 30 to 50 cm (depends on surface area) Oxidize about g/m2/d
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Type II MBFs Actively aerated compost or compost/soil MBFs
Bed thickness; 50 to 100 cm (higher thicknesses are possible because of active aeration) Oxidize about g/m2/d or more
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Field Application of MBFs – Our Experience
Passively aerated compost based MBFs: Control vent gases from natural gas metering stations (volume: m3/day) Operated during cold winters (heat generated by methanotrophic activity) Maximum oxidation: about 400 g/m2/d
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Field MBF Experimental Results
max 33 min 10 max 34 max 24 min 14 min 20 % Methane Oxidation vs Time High Moisture Temperature profile (5, 20 & 35 cm) Atmospheric temperature = 10 0C
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Field Application of MBFs – Our Experience with Solution Gas Oxidation
Passively aerated compost based MBFs to control casing/solution gas at oil well sites: Divert gas normally vented into the atmosphere through a compost biofilter Low efficient, low maintenance unit at a heavy oil well site
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Field Application of MBFs – Our Experience with Landfill Gas
Actively or Passively aerated compost based MBFs to control landfill gas (from a passive extraction system): To be installed at a landfill in Ecuador Final design (size, active or passive aeration) depends on gas flow rates and lab experiments/mathematical modeling
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Mathematical Modeling: Reactive-Transport Model
Model Input Bulk density Soil particle density Soil moisture content Biological kinetic parameters (Ko2, KCH4, Vmax) Soil temperature CH4 source strength Model Output Gas concentration profiles CH4 oxidation rate
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Design Curves from 1-D Reactive Transport Model Simulations
a. depth=0.3m; m.c.=7.5% b. depth=0.3m; m.c.=15% c. depth=0.9m; m.c.=7.5% d. depth=0.9m; m.c.=15%
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Advantages of Biocaps and Biofilters
Methane oxidation without undesirable by-product formation (compare with flaring of landfill gas) Cost effective (compare with combustion with or without energy recovery, catalytic oxidation) Cost of Biocaps; $1 to $5/tonne of CO2E Cost of MBFs; $2-10/tonne of CO2E Low operation/maintenance requirements
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Barriers to Large-scale Application of Biocaps
Not well known to landfill operators, consultants and regulators need more pilot projects, field demonstration projects (Nanaimo landfill project with SHA, Nanaimo municipality) Too simple, too cheap and not established, yet. More expensive, well established technologies are available (gas extraction for energy recovery or flaring) But no competition for low volume diffused gas escape via final covers No benefits other than GHG credits Regulatory requirements for landfill covers. Biocaps are not compatible with dry-tomb covers, but compatible with ET covers)
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Issue 1: Formation of Exo-polysacharides (EPS)
EPS is a by-product of methanotrophy Observed in laboratory flow-through column studies Decreases methane oxidation efficiency over time (at least in 15 cm diameter columns) However, this may not be an issue in field biocaps or MBFs Or develop biocap/MBF maintenance plan to eliminate EPS impacts
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The growth of slime (extra-cellular polymeric substances) reduces CH4 oxidation efficiency.
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Issue 2: Stability of granular medium (eg. compost))
Stability is an issue when the biocap granular medium contains high levels of organic material (eg. compost) If compost is not fully stabilized, it will be difficult to establish methanotrophic bacteria
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Issue 3: Determination of methane oxidation in the field
Needed to determine Carbon off-sets of a Biocap project Measure methane oxidation directly (from field data) Carbon isotope measurements (expensive; good for research projects) mathematical modeling (not popular) universal method not yet available Could measure methane emissions before and after Biocap implementation Need several field measurements (before and after) easier, need less equipment/expertise but labor intensive Need regulator “buy-in” (who are the regulators?) Flux chamber method being used at Nanaimo landfill
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Operational Problems with MBF: Gopher and
Badger damage results in short-circuiting of CH4
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Operational Problems: Cold Climate
Heat generated by bacteria and compost’s self- insulation help keep the biofilter warm Heating is required for the really cold days
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Conclusions High quantities of CH4 are emitted from landfills and oil and gas industry sources Methanotrophy-based technologies can be applied to reduce these emissions in a cost effective manner Biocaps with soil or soil-compost mixtures can be used effectively to eliminate low volume diffused CH4 emissions MBFs, either passively or actively aerated, could be used to control low-volume point sources of CH4 Mathematical models could be used to optimize design of Biocaps and MBFs Need more field pilot-scale demonstration projects to “educate” stake holders Thank You!!!
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