CSG Short Course
Reservoir Engineering
Brisbane, Friday 16th October 2010
Prof. George STEWART
Weatherford International
Heriot-Watt IPE
Casing
Tubing
Testing Valve(operated by
annulus pressure)
Drillstem
Testing
Assembly
Downhole
Memory
Surface
Recording
Packer(set by weight on
string)
PressureTransducer
Tailpipe
Figure 2.1.1
Choke
GasSurface Choke providesRate Control
Q
Test Separator
Well Test Surface Hardware
Oil
Orifice PlateFlow Measurement
qo
Test Rate Limited by
Separator Capacity
Fig 2.1.1b
Test Separator
Transient Well Testing
Buildup Analysis - Horner (Theis) Plot
BuildupAffectedby
WellboreStorage Intercept
ETR MTR LTR
p*pws
Nomenclature
due to D.
Pozzi (EPR)
Fig 2.1.3
4 k hπ
q Bs
µ
Semilog Analysislnt + tp ∆
∆t
Storage InterceptgivesskinfactorS
Affectedby
Boundariesslope = −
altered
zone
p
Unaltered
Permeability
k
Fig2.1.4a
Near Wellbore Altered Zone
pw
pw f
∆ps
k
rw rs re
wellbore
radius
altered zone
radius
external
radius
∆p = Incremental Skin Pressure Drop
s
ks
x Heated Bar
Thermocouples in thermowells
Inner B.C.
Linear Flow
t
FaceTemp.
Dynamic Temperature Distribution
∂ ∂T k T=
2q
kT
= −∂
Constant
heat
flux
T(t=0)
x
Transient Heat
Conduction Equation
i.e.
. . . specified
gradient
(2 kind BC)nd
t
Penetration Depth
Initial Temp.
T
Fig 2.1.9
∂
∂ ρ
∂
∂
T
x
k
C
T
xp
=2
q
AkT
xx
= −
=
∂
∂0
∂
∂
T
x
q
kAx=
= −
0
The Conduction
of Heat in Solids
by
H.S. Carslawand
J.C. Jaeger
Clarendon PressOxford1959
PanMesh
Finite Element
Numerical
Simulation
of
Diffusion Equation
Problems
FEM
Comprehens ive
Library of
Analyt ical
Solut ions
All Commercial
Heat Conduction
Codes are FEM
e.g. NASTRAND
Used to Solve
Perforation Completion
and RFT Probe
Problems
Foundation of
Many Transent Well
Testing Papers
Foundation of Many
Transient Well Testing
Papers
Sydney Opera House
t
p(r ,t)
pi
Well-Bore
Fig 2.2.2
ln r
tBore
Trans ient Deve lopment o f
the Format ion Pressure
Dis t r ibu t i on
p EirtDD
D
=
1
2 4
2
For
( )∆ pq
p EiDµ12
10 2194
2011= = = =
..
r
ti e r tD
D
Di D
2
41 4= =. .
Radius of Influence
qkhµ
π22 2
Arbitrarily chosen as defining the appreciable depth
of penetration of the pressure disturbance
r tk tci
t
= =44
αφµ
Classical depth of penetration formula in diffusional processes
Synonomous with depth of investigation
pt
SwDD= +
12
4ln
γ
Dynamic Formation
Dimensionless
Quasi-Steady-State
Dimensionless Skin
Addition of Quasi-Steady-State Skin Effect
Dimensionless
Pressure Drop
Dimensionless Skin
Pressure Drop
( )p t pq
khk tc r
Swf it w
= − + +
µπ φµ4
0 80908 22ln .i.e.
Additional (constant) pressure drop is given by:
Both S and q are presumed constant
Skin factor is a measure of completion efficiency
Different meaning in fractured systems
∆ pq
khSs =
µπ2
rD01 200
q
t = 10pD
4
t = 10D
4
∆
50
200
2 103
pwsD
5
0t pD
∆ t D
Pressure Build-Up in a Reservoir
Figure 2.5.2
10
∆p
p =d( p)∆
d( t)ln
. . . Local slope ofsemilog graph
Tangents to Curve(Obtained by Numerical
Differentiation)
Logarithmic Derivative
Ln p
Ln t
Ln t
Differentiation)
Plateau
ETR MTR LTR
Slug
TestingNote RisingLiquid Level
hCushion
Valve
Closed
GaugeRegisters
pi
Fig 6.11.1
p = ρgh
- assuming negligible friction and KE losses
q Adh
dt
A
g
dp
dt
w= =ρ
Field Units qA dp
dt
w= 9 86.ρ
Well with Rising Liquid Level
Field Units qdt
= 9 86.ρ
q : bbl/D
A : ft
: g/cc
p : psi
t : hr
2
ρ
w
- flow-rate obtained from the natural derivative of the pressure
Note form:
q Cdp
dt=
p q
Draw-down
VRD
Build-up
VRB
Slug
Schematic of Complete Slug Test including Shut-in
pi
pw
po
q
0ValveOpens
ValveCloses
Slug
Tes t
Fig 6.11.3Time, t
∆ t
Australian CSG (CBM) DST
rw = 0.3542 ft h = 14.1 ft φ = 0.02 Bw = 1.0038 µw = 0.736 cp cw =
3.177×10-6 psi-1 ct = 3.6468×10-6 psi-1 T = 93oF
85.2
66.1q = 101 bbl/d
Australian CSG (CBM) DST
pwf(tp) = 344.0 psia
pi = 386.1
psia
47
po = 272.8
psia
Log-Log Diagnostic of Final Buildup
US
k = 124 md
DP
k = 124 md
S = 6.83
Three rate points in history
Elapsed Time (hr)
pppp2222
pppp1111
Control Volume
X-sectional Area, A
Steady-State Realisation of a Naturally Fractured Reservoir
No Flow
C P
F r a c t u r e
N e t w o r k
kf = Bulk Average Fracture Network Permeability
( Continuum Theory ) Fig 10.1.1
q
A
k p p
L
fb=−
µ
2 1
WaterFlowOnly
CDP
Pressure Drawdown Profileof a Single Well
Only
DiscontinuousGas Flow
ContinuousGas Flow
After Airlie
500
400
300
Ca
pa
city
(scf/
ton
) Gas Storage Capacity450 scf/ton
InitialGas
Content355 scf/ton
InitialReservoir
CriticalDesorption
Langmuir Isotherm and Gas Desorption Calculations
200
100
0
Ga
s
Sto
rage
C
5000 1000 1500 2000
Pressure (psia)
ReservoirPressure
1,620 psia
DesorptionPressure632 psia Maximum Gas Recovery
230 scf/ton
Abandonment Gas Content125 scf/ton
Abandonment Pressure100 psia
Gas Recovery Factor
230355
= 0.648
After Airlie
Gas - Water Relative Permeability CurvesGas - Water Relative Permeability CurvesGas - Water Relative Permeability CurvesGas - Water Relative Permeability Curves
0.6
0.8
1
kkkkrrrr
m = 3.5 n = 2.0
krgo = 1.0 krw
o = 0.365
Swc = 0.365 Sgr = 0.3
0
0.2
0.4
0.35 0.4 0.45 0.5 0.55 0.6 0.65 0.7
SSSSwwww
kkkkrrrr
Fig 19.6.1
1.0
0.8
0.6
kr
Gas - Water Relative Permeability Curves
KC32KB24
KA12
Low kGroup
0.013 md ( = 0.0151)φ
0.14 md ( = 0.0158)φ
0.262 md ( = 0.0263)φ krw
2.5 in dia
0.4
0.2
05040 60 70 80 90 100
S (%)w
After Shedidand Rahman
Group
krg
2.5 in diacore plugs
Australian Coal
6
8
10
12
SGB
Gas Block Skin, SGB
rw = 0.35 ft
ka = 0.365k
k/k − 1 = 1.74
0
2
4
6
0 50 100 150 200 250 300
SGB
Radius of Gas Block Region, ra (ft)
a
k/ka − 1 = 1.74
w
a
a
GBr
rln1
k
kS
−=
Log-Log Diagnostic and Type Curve
p
∆ t
ETRWBS
MTR
singlephasegas
DP
DP
Radial Composite
twophase Transition
k k1
1µ µ=LNMOQP
k k2
2µ µ=LNMOQP
Radial Composite Behaviour in a
CBM System
∆ t e
∆ t e
pws
Semilog Plot
SecondSt raigh tLine
FirstStraightLine
Total(Pseudoradial)
Skin
Fig 16.3.3
slopek
→ 1
1µ
slopek
→ 2
2µ
2nd Australian CSG (CBM) DST
Rate steps: 70.8, 66.9, 63, 60.5, 57.5 bbl/d
rw = 0.1573 ft h = 10.3 ft φ = 0.02 Bw = 1.008 µw = 0.589 cp cw =
3.03×10-6 psi-1 ct = 2.03×10-4 psi-1 T = 113.6oF
Log-Log Diagnostic of Final Buildup
Five rate points in history
k h1 1
Region 2
k h2 2
Pressure Propagation in a Linear Composite System
Region 1
k h1 1 k h2 2k h2 2
Active Well
Koenig, R.A., Choi, S.K. and Meany, K.T.A.:“Dartbrook Coal Mine
Two-Phase Well Testing, Boreholes
DDH79, DDH81, DDH83, DDH84, DDH94, DDH106 and
DDH107”, ACPRC Report No. 068, CSIRO Petroleum Australia, May
1994
• Variation of permeability with depth was investigated by Koenig et al
• Injection, falloff and production tests carried out in six wells
• Depths in the range 180 – 292 m
• Wynn Upper A seam (4m interval)
• Trend of decreasing permeability with increasing effective stress apparent• Trend of decreasing permeability with increasing effective stress apparent
• Mean permeability from an interference test and laboratory measurements
also plotted
Durucan, S. And Edwards, J.S.:“The Effects of Stress and Fracturing on the Permeability
of Coal”, Mining Science and Technology, 3, 1986, 205-216
• The high sensitivity of coal permeability to effective stress is well known
3
1
σ∝k approximately
10000
1000
100
Permeability, k
*103
(md)
Laboratory Permeability versus Effective Stress
All Tests
Well DDH140
10
10 2 4 6
Effective Stress, (Mpa)σ
(md)
k = −756 3 06σ .
After Wold and Jeffreys
φ
φi = 1 +
p − pi
φiM
k
= φ 3
Palmer and Mansoori CBM Rock Mechanics Model
Recommended
by Mavor
- Based on Linear Elasticity
Code Porosity Cutoff
φ = 0.00001
Does not handle
permeability rebound
very sensitive to φi
k
ki =
φ
φi
M = E1 − ν
(1 + ν)(1 − 2ν)
K = M
3
1 + ν
1 − ν
E = Young’s Modulus ν = Poisson’s Ratio
Constrained Axial
Modulus
Bulk Modulus
Palmer and Mansoori Data for the San Juan Basin
Poisson’s Ratio, ν• Poisson’s ratio measured on core in the laboratory fall in a range 0.27 – 0.4
• Large scale Poisson’s ratio should be about a factor of 1.15 greater
• “Good” average, large scale ν = 0.39
Young’s Modulus, E
Elastic Parameters
• Young’s modulus has been determined in two ways
• Static core measurements
• Measurements of PV compressibility, c• Measurements of PV compressibility, cf
• cf = 1/(2Eφi)
• Core measurements
• Range of (3 – 7)×105 psi (Jones et al)
• Large scale modulus should be about 4 times smaller
• This gives Els (0.75 – 1.75)×105 psi
• Pore volume compressibility
• Average of several cf measurements lie in the range (23.3 –
96.9)×10-5 psi-1
• φi lies in the range 0.001 – 0.005
• Hence E = (1.72 – 7.15)×105 psi
• Mean of core and PV compressibility results E = (1.24 – 4.45)×105 psi
Choking Condition in Production (Drawdown)
rw = 0.26 ft h = 2.5 ft µ = 0.65 cp Bo = 1.005 ct = 3.003×10-3 psi-1
E = 500,000 psi ν = 0.25 n = 3
pi = 734 psia ki = 11.3 md φi = 0.001
Parameters from Mavor IFO Field Example (q = -96 bbl/d)
qcrit = 7 bbl/d
tp = 10 hr
CRD
Invasion of Natural Fractures
by Mud Solids
NTS
Candidate for UnderbalanceDrilling
High Fluid Loss whenDrilled Overbalance
15
20
25
30To
tal A
pp
are
nt
Sk
in,
Sa
Apparent Skin from Conventional Buildup Analysis
φi = 0.01
Effect of True Skin is Magnified
0
5
10
0 1 2 3 4 5 6 7 8
Tota
l A
pp
are
nt
Sk
in,
S
True Skin, S
Sσ = 1.3725
Well “Chokes”
Mavor Field Example Data (Unreduced)
Injection Falloff
pwf(tp) = 1504.56 psia
pw
(psia)
q = −96 bbl/d
Time (hr)
Mavor Field Example (Injection and Falloff)
Falloff period
(IFO)∆p(psi)
rw = 0.26 ft h = 2.5 ft m = 0.65 cp cw = 3.0×10-6 psi-1 Bw = 1.005
q = -96 bbl/d pwf(tp) = 1504.56 psia tp = 8.6458 hr
Elapsed Time, ∆t (hr)
Manual Match of Mavor Data
SDPP + NIWBS Model
(Hegeman)∆p(psi)
k = 11 md S = 4.5 φi = 0.0009 Cs = 3×10-5 bbl/psi
t = 0.075 hr Cf = -6900 psi
E = 5×105 psi ν = 0.25 n = 3
Elapsed Time, ∆t (hr)
tp = 8.6458 hr
5
6R
ate
, q
(
bb
l/d
)Production Forecast (Dewatering)
pi = 734 psia
pwf = 500 psia
Constant BHFP
k = 10.8 md S = 2 n = 2.466
3
4
0 200 400 600 800 1000
Flo
w-R
ate
, q
(
bb
l/d
)
Time, t (hr)
Mavor Field Example Analysed with 90o Fault Boundary Model
(No Stress Dependency)
φi changed from 0.001 to 0.01
Results from Nonlinear Regression
Cs = 1.789×10-4 bbl/psi τ = 0.0742 hr Cφ = -1000 psi
k = 30.63 md S = -0.0105 L1 = 24 ft L2 = 54.5 ft pi = 723 psia
Dewatering Transient Rate Based on Fault Model
Mavor Field Example
Wa
ter
13 bbl/d
SDPP Model predicted 4 bbl/d
Structure
• Formation Geometry
• Natural Fractures
• Faulting
• Folding
• Stress/Compression
Well
A
Well
C
Well
BPermeability
Facies Change
Channel
Sandstone Belt
Fault
Offset
Coal
Pinch
Out
Offset
Schematic Diagram of Coalbed Reservoir Geometry
Components that affect lateral continuity, cleat
properties, permeability, and porosity
CRB
Derivative L-L Diagnostic Derivative L-L Diagnostic
Apparent
Testing Strategy for CBM Wells
Buildup Following Production Falloff Succeeding Injection
IFO
k DP k DP
ApparentDP
Ideal SDPP Alone
Including Storage andBoundary Effect
ApparentDP
Buildup Identifies Presenceof Boundary Effects
In Falloff SDPP andBoundary Effects are Similarand Combine to Give Steep
Derivative Response
k DPik DPi
Strategy for Testing CBM (CSG) Wells
• In Australia Rising Liquid Level DSTs (Slug Tests) have largely been employed
• Objective has been to determine permeability, skin and pressure• Results have often indicated high skin the nature of which must be
clarified• Origins of skin are:
• Drilling (formation) damage• Stress effect on near wellbore permeability• Gas block due to gas desorption• Gas block due to gas desorption
• DST Test Results have revealed considerable complexity:• Faulting (boundary) effects• Radial composite behaviour• Reservoir compartmentalisation• Limited Entry
• Radial composite effect may be:• Formation damage inner region• Reservoir effect such as increasing kh away from the well• Linear composite• Gas block
Porosity Dilemma
• In CBM (CSG) wells it is difficult to obtain porosity from either logs or core data
• Well test interpretation requires a realistic φ value to correctly model the diffusional aspect of the pressure propagation
• Fortunately the determination of permeability does not involve porosity
• Effect of porosity on computed skin is weak because φenters a logarithmic term
• Operators have used a porosity which allows production data (dewatering) to be modelled
• This is not the value which should be used in the Palmer-Mansoori SDPP model
• Practitioners in the US have used φi = 0.001 in the SDPP model
• This is misleading!• Porosity can be determined in well-to-well interference
testing