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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
de
— 1
/18
A Numerical Study of Nonideal and Secondary Fractures in Shale-gas Reservoirs using Voronoi Grids
Thesis Defense 27 May 2011 — College Station, Texas
Olufemi OLORODEDepartment of Petroleum Engineering
Texas A&M UniversityCollege Station, TX 77843-3116 (USA)
+1.803.397.7623 — [email protected]
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Objectives:
●To present an unstructured mesh-maker that is used in gridding complex and non-ideal fracture geometries
●To study the effects of nonplanar and nonorthogonal fractures on reservoir performance
●To study the interaction between secondary and primary fractures
●To assess the validity of single-fracture representation of multiply-fractured horizontal wells
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
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Motivation:●Cartesian grids do not provide the
flexibility of modeling irregular fracture geometries.
●Cartesian grids require far more grid-blocks, many of which are unnecessary.
●No consensus on the effect of nonideal fracture geometries on production.
●Very little is known about the interaction between induced and hydraulic fractures (Houze et al. 2010).
Voronoi grids showing nonplanar fractures
Cartesian Mesh showing 4 planar fractures
Unnecessary refinement
X
Y
X
Y
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Approach:
324m260 x Magnification
~100μm
Relative Sandstone Pore Diameter
Relative Shale Pore Diameter
Visualize the grids
Develop Meshmaker
Construct Voronoi grids
Analyze rates using log-log plots
Perform simulation
Provide pressure maps where needed
Any bugs?
Base case?
Debug code
Yes
Yes
No
No
Validate with Ecrin
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode
xmf = n*xf
Sli
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Gridding: Single-fracture Representation
3D ViewSRV
Unstimulated Reservoir Volume
X-axis
Y-axis
1 2 3 4 5
xf
n=6
2D View
Horizontal well
Fractures
Y
Z
X
Y
X
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: Log-log Rate Profile
●Discussion: Single-fracture Representation of Multiple Fractures■ Fracture interference is absent in single fracture case■ Boundary-dominated flow is not seen in the single fracture case
Single fracture Representation
10 multi-stage fractures
1 month 5 years1 year
30 years
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: Distinguishing between kf and wf
●Conductivity is kept constant at 492 md-ft (1.5x10-10 mm-m2).
●Do we see distinct trends at early times?
wf, ft kfrac, md modified
0.010 50,000 0.33
0.049 10,000 0.066
0.098 5,000 0.033
0.328 1,500 0.0099
Table 1—Fracture parameters in field units
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: (after porosity modification)
●Porosity modification keeps mass accumulation constant
●Bad news: we cannot distinguish
between kf and wf.
●Good news: we can represent very
minute fracture cells with much bigger cells.
fified mod
newref wwf /
where,
Porosity Modification:
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Background: Nonplanar & Nonorthogonal Fractures
Nonorthogonal fracturelt = ala = a sin θwhere, lt is total length, andla is apparent length
f
e
d
b
c
θ
a
h = a sin θ
Nonplanar fracturelt = b+c+d+e+fla = lt sin θwhere, lt is total length,la is apparent length,
All segments are inclined at angle θ to the horizontal.
3D Schematic of a Nonplanar Fracture
2D Schematic of a Nonplanar Fracture
3D and 2D Schematics of a Nonorthogonal Fracture
Illustration of “Total” and “Apparent” Lengths
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Gridding2D Aerial View of Nonplanar Fractures
2D Aerial View of Nonorthogonal Fractures
Y
X
Y
X
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: Nonorthogonal and Nonplanar Fractures
●Discussion:■ Irregularities in the fracture geometry limits flow-regime analysis with
diagnostic rate plots
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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2/18
Results: Nonorthogonal and Nonplanar fractures
●Discussion:■ The cumulative production initially matches that of a planar fracture
with xf=lt, but drops gradually over time.
xf=lt
xf=la
Nonplanar frac
Nonorthogonal frac
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Gridding: Secondary Fractures
■ Three secondary fracture configurations are studied:
—A secondary fracture that intersects the primary fracture at height, h/4.
—A centered secondary fracture.
—Two secondary fractures at heights h/4 and 3h/4, respectively.
Y
X
Z
h/4
h/2
h/4
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: Secondary Fracture Flow Profile
●Parallel half-slope lines depict linear flow into the SRV.
● Increase in rates correspond to the increase in the SRV that is drained into the wells.
●Change in slope at late times indicate outset of boundary-dominated flow.
●NB:Secondary fractures were modeled with infinite conductivity, and are 0.05 mm (0.00016 ft) wide.
2 secondary fracsCentered secondary frac
Secondary frac at h/4
Primary fracs only
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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5/18
Results: Effect of Secondary Fracture Conductivity
●Discussion:■ Dimensionless rate profiles show a reduction in the linear half-slope
when the dimensionless conductivity of the secondary fractures becomes less than 10 (finite conductivity)
■ This may be useful in optimizing fracture design
kfrac, md Cf, md-ft CfD
3x106 4.92x102 1.67x104
2x106 3.28x102 1.11x104
1x106 1.64x102 5.56x103
2x105 3.28x101 1.11x103
1x105 * 1.64x101 5.56x102
1x104 1.64x100 5.56x101
2x103 3.28x10-1 1.11x101
1x103 1.64x10-1 5.56x100
2x102 3.28x10-2 1.11x100
Table 2—Secondary fracture conductivity parameters
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Results: Effect of Primary Fracture Conductivity
●Discussion:■ Dimensionless rate profiles show a drop in production as the primary
fracture conductivity drops■ Results match those published by Freeman et al. (2010)
kfrac, md Cf, md-ft CfD
5.00x106 4.92x104 1.67x106
5.00x105 4.92x103 1.67x105
5.00x104 4.92x102 1.67x104
5.00x103 4.92x101 1.67x103
5.00x102 4.92x100 1.67x102
1.67x102 1.64x100 5.56x101
3.33x101 3.28x10-1 1.11x101
1.67x101 1.64x10-1 5.56x100
3.33x100 3.28x10-2 1.11x100
Table 3—Primary fracture conductivity parameters
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Conclusions:
●Irregularities in fracture geometry can limit the analysis of these reservoirs with diagnostic plots.
●Production increases as SRV increases for infinite-conductivity secondary fractures.
●All infinite-conductivity secondary fractures with the same SRV have identical flow behavior, while finite-conductivity secondary fractures show a reduction in magnitude of the half-slope line.
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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A Numerical Study of Nonideal and Secondary Fractures in Shale-gas Reservoirs using Voronoi Grids
End of Presentation
Thesis Defense 27 May 2011 — College Station, Texas
Olufemi OLORODEDepartment of Petroleum Engineering
Texas A&M UniversityCollege Station, TX 77843-3116 (USA)
+1.803.397.7623 — [email protected]
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode
Questions?
Sli
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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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Parameters SI Unit Field Unit Frac half-length, xf 90 m 300 ftFrac width, wf 3 mm 0.00984 ftFrac spacing, df 100 m 328 ftWell length, Lw 1200 m 4000 ftNumber of fracs 12 12
Reservoir thickness, h 100 m 330 ftPermeability, kshale 1.0x10-19 m2 1.0 x10-4 ft
Frac permeability, kfrac 5.0x10-11 m2 5.0 x104 ftPorosity, 4 % 4 %Frac porosity, frac 33 % 33 %Temperature, T 93.33 0C 200 0FWell radius, rw 0.1 m 0.32 ft
Reservoir pressure, pi 3.45x107 Pa 5000 psiaWell pressure, pwf 3.45x106 Pa 500 psia
Table 1.1—Representative Barnett Shale-gas Parameters
27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures
O.M. Olorode Sli
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wfiD ppkh
2.141
2
0002637.0
ftD xc
ktt