1 Enhanced Coalbed Methane Recovery and CO 2 Storage in Coal Seams Sevket Durucan Department of Earth Science and Engineering Imperial College London APEC Seminar, AIST, Tsukuba, 7 December 2007 mINING AND ENVIRONMENTAL ENGINEERING RESEARCH GROUP Background Coalbeds as both the reservoir and source rock OUTLINE Retention and release of gas in coal Coal permeability, dynamic permeability modelling in coalbed reservoir simulation Reservoir simulation of enhanced Coalbed Methane recovery and CO storage in coal seams APEC Seminar, AIST, Tsukuba, 7 December 2007 CO 2 storage in coal seams Conclusions
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Enhanced Coalbed Methane Recovery and CO2 Storage in Coal Seams
Sevket Durucan Department of Earth Science and Engineering
Imperial College London
APEC Seminar, AIST, Tsukuba, 7 December 2007mINING AND ENVIRONMENTAL ENGINEERING RESEARCH GROUP
Background
Coalbeds as both the reservoir and source rock
OUTLINE
Retention and release of gas in coal
Coal permeability, dynamic permeability modelling in coalbedreservoir simulation
Reservoir simulation of enhanced Coalbed Methane recovery and CO storage in coal seams
APEC Seminar, AIST, Tsukuba, 7 December 2007
CO2 storage in coal seams
Conclusions
2
World Carbon Dioxide Storage Options
Deep Ocean
Saline Aquifers
Unminable Coal Seams >15 Gt CO
Depleted Oil Reservoirs
Depleted Gas Reservoirs
Unminable Coal Seams >15 Gt CO2
APEC Seminar, AIST, Tsukuba, 7 December 2007Source: USGS
Major Coal Basins
APEC Seminar, AIST, Tsukuba, 7 December 2007
3
Major Coal Basins
APEC Seminar, AIST, Tsukuba, 7 December 2007
Major Coal Basins and Methane ResourcesContinent Country Coal Resources Methane Resources
x 109 tonnes x 1012 m3
Europe and Belgium 0.075the Russian France 0.600Federation Germany 320 2.85Federation Germany 320 2.85
Methane Extraction from Coal Seams: Well Technology
APEC Seminar, AIST, Tsukuba, 7 December 2007
Coal as a Reservoir Rock: Structure
Uniform and orthogonal fracture (CLEAT) structure
APEC Seminar, AIST, Tsukuba, 7 December 2007
microcleat
5
Coal as a Reservoir Rock: Structure
f l t
butt cleat
adsorbed gas
Coal Matrixcontaining
pores
face cleat
Macropores > 50 nm
M 2 50
microcleat
APEC Seminar, AIST, Tsukuba, 7 December 2007
free gas
CH4
Mesopores 2 – 50 nm
Micropores < 2 nm
Cleat system (2mm - 25 mm)
Pore surface area 20 – 200 m2
Coal as a Reservoir Rock – Gas Retention
butt cleat
adsorbed gas
Coal Matrixcontainingmicropores
face cleat
8
12
16
20
s C
onte
nt, m
3 /t
CH4 adsorption isotherm
APEC Seminar, AIST, Tsukuba, 7 December 2007
free gas
CH4 0
4
0 1 2 3 4 5 6 7 8Pressure, MPa
Gas
6
Coal as a Reservoir Rock: CH4 / CO2 Retention in Coal - Adsorption Isotherm
COt)
1,000
Pressure (MPa)0 1.4 2.8 4.2 5.6 7
CO2
75%CO2 25%CH4
CH4
Gas
con
tent
(m3 /t
10
15
5
0
800
600
400
Gas
Con
tent
(sc
ft/t
onne
)
APEC Seminar, AIST, Tsukuba, 7 December 2007
Pressure (MPa)
0 200 400 600 800 1,000 1, 200Pressure (psi)
0
200
pPpVV+
=L
LLangmuir equation:
Enhanced Coalbed Methane Recovery (ECBM)two principal methods of ECBM, namely N2 and CO2 injection (inert gas stripping and displacement sorption respectively)
injection of nitrogen reduces the partial pressure of methane in the reservoir, th t th d ti ith t l i th t t l ithus promotes methane desorption without lowering the total reservoir pressure
20
25
m3 /t
)
CH4 7% moist. coal CO2
3 /t)
15
coal can adsorb approximately two to six times as much CO2 by volume as methane, therefore, the assumption has been that the CO2 injection stores 2-6 moles of CO2 for every mole of CH4 desorbed.
APEC Seminar, AIST, Tsukuba, 7 December 2007
Pressure (MPa)0 4 8 122 6 10 16
10
5
15
20
014
Gas
con
tent
(m
N2 7% moist. coal
Pressure (MPa)0 1.4 2.8 4.2 5.6 7
75%CO2 25%CH4
CH4
Gas
con
tent
(m3
10
15
5
0
7
CoalSite
Durango
Tiffany Unit
Florida River Plant
McElmoD
Simon Pilot
San Juan BasinSimon Pilot
Colorado
NewMexico
Sweet
COLORADONEW MEXICO
SpotFarmington
Overpressured:Sw = 1.0
Allison Unit
Tiffany UnitDomeCO2 Field
APEC Seminar, AIST, Tsukuba, 7 December 2007
Underpressured:Sw < 1.0
Underpressured:Sw = 1.0
Scale, miles0 10 20
Amoco Simon N2 Injection Pilot
Simon Pilot
Nitrogen
1,600
1,200
800
Start NitrogenInjection
Total Gas
End NitrogenInjection
Rat
e M
scf/
D o
r ST
B/D
APEC Seminar, AIST, Tsukuba, 7 December 2007
Natural Gas
1988 1989 1990 1991 1992 1993 1994 1995
400
0Water
NaturalGas
Gas
/Wat
er R
Source: Wong, Gunter, Law and Mavor, 2000
8
CoalSite
Durango
Tiffany Unit
Florida River Plant
McElmoD
Simon Pilot
San Juan BasinTiffany Unit
Colorado
NewMexico
Sweet
COLORADONEW MEXICO
SpotFarmington
Overpressured:Sw = 1.0
Allison Unit
Tiffany UnitDomeCO2 Field
APEC Seminar, AIST, Tsukuba, 7 December 2007
Underpressured:Sw < 1.0
Underpressured:Sw = 1.0
Scale, miles0 10 20
BP Tiffany Unit N2 Injection (Full Scale Commercial Pilot)
“… contrary to what is usually supposed, solid coal is extremely airtight, and lets very little air or gas through, even with a driving pressure of a whole atmosphere.”
Ivor GRAHAM, 1916
“….that the rate of gas flow through the coal is a function of thedifference in partial pressure of methane along the flow path. Therefore, the emission of methane from a lump of coal is not
APEC Seminar, AIST, Tsukuba, 7 December 2007
, pdependent on the total external pressure, but upon the partial pressure of the methane in the atmosphere and the pressure of the gas in coal.”
Ivor GRAHAM, 1919
Strength, Elastic and Flow Properties of Coal
Coal structure is highly elastic
LimestoneSandstoneWeak
Reservoir S d t
Coal(Various) Shale
fractures matrix
0.86 - 3.9 35 - 5510- 200.4 – 1.8
Young’s Modulus, E
(GPa)
Sandstone( )
5 - 70
10
15
20
25
Stre
ss (M
Pa)
APEC Seminar, AIST, Tsukuba, 7 December 2007
Coal permeability is• Anisotropic
• Highly stress dependent
0
5
10
0 10 20 30 40 50 60Axial Strain (millistrain)
Axia
l S
CAYDAMARBARNSLEYCOCSHEADBANBURYDUNSILDEEP HARD
12
Stress Effects and Permeability
0.5
0.6
md) Durucan Puri et al Somerton
10-1
5 m
2
3001000
Three Yard
APEC Seminar, AIST, Tsukuba, 7 December 2007
1000 1200 1400 1600 1800 2000 2200 24000
0.1
0.2
0.3
0.4
Effective Stress (psi)
Perm
eabi
lity
(m
•Intact coal
10
Perm
eabi
lity
(k),
1
Confining Stress (MPa)0 2 4 6 8
0.313
1030
100300
Great RowCannel Row
•Fractured coal
Field Experience: San Juan Basin Field Permeability Behaviour
0 4 8 12 16 20 24Elapsed time from the start of N2 flooding (day)
Iwel
lblo
ck /
0.1
1
Wel
lblo
ck p
epermeability
flooding
start of CO2
injection
Model Prediction vs Field Data: Pre- and Post- N2 Flooding CO2 Injection Rates
30002
model field (injected amount) field (24-hour rate)
Pre-N2 flooding
Post N2 flooding CO 2 injection rate 20000
0
600
1200
1800
2400
3000
10-Apr 15-Apr 20-Apr 25-Apr 30-Apr 5-May 10-May
2006
Rec
orde
d da
ily a
mou
nt in
ject
ed (m
3 )/ C
O2
inje
ctio
n ra
te (m
3 /d)
Post-N2 flooding
0
4000
8000
12000
16000
20000
0 2 4 6 8 10Injection time (day)
CO
2in
ject
ion
rate
(m3 /d
)
model
field
APEC Seminar, AIST, Tsukuba, 7 December 2007
N2 flooding temporarily improved CO2 injectivity, which declined quickly back to the pre-flooding level (~ 3 tones/ day) after two days.
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Concluding remarks
• Coalbed reservoirs have unique characteristics: storage, transport and production mechanisms, permeability b h ibehaviour.
• Considerable advances in the reservoir simulation of ECBM, especially in permeability modelling have been made.
• While matrix shrinkage is desirable during primary recovery, CO2 matrix swelling can have a severe impact on coalbed permeability and well injectivity
APEC Seminar, AIST, Tsukuba, 7 December 2007
permeability and well injectivity.
• Long term fate of injected CO2 in coalbeds is uncertain, as CO2, especially at supercritical conditions, reacts with the reservoir rock and fluids.