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7/27/2019 Coal Bed Methane Development (Tom Myers)
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Coal Bed Methane
DevelopmentTom Myers, PhD
Hydrologic Consultant
Western Mining Action NetworkSept. 29-Oct. 1, 2005
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What is coal bed methane?
Standard natural gas:CH4Methane forms along
with coalIt is held in the cleatswith the coal
Substantial water
pressure needed tokeep methane in thecoal: 400 to 1000 ft ?
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Process of Developing CBM
Relieve pressure to
release methane by
removing water
Domestic wellscompleted in seams
produce methane due to
drawdown caused by
nearby pumping
6-7 times more natural
gas than in traditional
natural gas fields
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Set of wells in southeast MT
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What Happens to Developed
Water?
Most developed water is:
Discharged to surface water
Discharged to containment pond
Land applied for evaporation
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Discharge to Impoundment in Wyoming: Disposal
by evaporation, percolation or sometimes diverted
to LAD
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What are hydrologic impacts?
Groundwater depletion
Water table drawdown
Decreased flow to springs and streams
Groundwater Contamination
- Methane in the groundwater
- Seepage of disposed CBM water
Surface Water
- Water quality: Excess Sodium or Salt- Wasted water
- Changing channel shape
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How much water produced?
Gallons per minute/ WELL
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How much water?
In Montana
25000 wells in Powder River basin
Up to 9,000,000 acre-feet
No water right!
In Wyoming
Up to 50000 wells in PRB
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Effects of Withdrawing That Much Water
2003 Drawdown in Wyoming PRB
North to Left
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Lets look at more details
Hydrology of coal: effects of depletion
Quality of water being discharged: effects
on rivers/stream/plants.
Alternatives to wasting the water
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Montana Powder
River Basin
Many coal seams
down to 1800 feet
Coal seams
relatively small
proportion of total
thickness
Dietz up to 100 feet
thick
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Coal Seams as a Source
Coal seams a major source of water in the
PRB of Montana.
Thin conductive seams with low porosity
lead to a rapid expansion in the effects of
drawdown.
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Effects of CBM Pumping
Rapid
Drawdown.
Effect onadjacent
aquifer?
Well WRE-51 and 51A, 09S 40E S29
3200
3250
3300
3350
3400
3450
3500
3550
Aug-76 Aug-80 Aug-84 Aug-88 Aug-92 Aug-96 Aug-00 Aug-04
MSL(ft)
W R-51 W R-51A
Overburden
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Effects of Coal Mining
09S 40E S13
3280
3300
3320
3340
3360
3380
3400
3420
3440
3460
Dec-73 Dec-78 Nov-83 Nov-88 Nov-93 Nov-98 Nov-03
MSL(ft)
WRE-09, Screen 213-238 WRE-10, Screen 163-178 WRE-11, Screen 92-122
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Unaffected hydrology
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CBM effects on hydrology
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Coal Seams Next to Tongue River
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Effects of Discharge to Surface Water
Water Quality
Surface Water QualityEffects on Irrigation/Stockwater Usage
Changing Riparian Ecosystems to more
salt tolerant system
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Water
Chemistry
Horseshoe Canyon
Formation (Alberta,
Canada)Powder River Basin,
WY Piceance Basin,CO San Juan BasinCO, NM, AZ, UT Black Warrior Basin,ALMax
(mg/L)
min
(mg/L)
max
(mg/L)
Min
(mg/L)
Max
(mg/L)
Min
(mg/L)
Max
(mg/L)
min
(mg/L)
max
(mg/L)
min
(mg/L)
Na 861.0 112.0 800.0 110.00 2673. 1976. 5939. 3674. 3100. 570.0
Ca 128.00 2.70 69.00 5.90 1839.00 13.20 118.70 6.50 100.00 2.50
Mg 23.50 0.20 46.00 1.60 7.77 0.00 39.00 2.88 34.00 1.10
As 0.0022
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Recommend: Most Sustainable
Practice
Reinjection into aquifers depleted byCBM production.
Injection or percolation into depleted
aquifers with water treatment as requiredprotecting and/or enhancing waterquality.
Replace other uses where quality allows.Surface discharges with water treatment as requiredresulting in improved stream flows with adequatemitigations against negative impacts.
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Hydrology effects with Reinjection
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