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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures O.M. Olorode Slide — 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 OLORODE Department of Petroleum Engineering Texas A&M University College Station, TX 77843-3116 (USA) +1.803.397.7623 — [email protected]

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Thesis Defense 27 May 2011 — College Station, Texas. A Numerical Study of Nonideal and Secondary Fractures in Shale-gas Reservoirs using Voronoi Grids. Olufemi OLORODE Department of Petroleum Engineering Texas A&M University College Station, TX 77843-3116 (USA) - PowerPoint PPT Presentation

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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]

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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

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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

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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

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27 May, 2011 — College Station, TX Study of Nonideal and Secondary Fractures

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xmf = n*xf

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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

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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

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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

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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:

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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

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Gridding2D Aerial View of Nonplanar Fractures

2D Aerial View of Nonorthogonal Fractures

Y

X

Y

X

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Results: Nonorthogonal and Nonplanar Fractures

●Discussion:■ Irregularities in the fracture geometry limits flow-regime analysis with

diagnostic rate plots

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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

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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

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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

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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

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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

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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.

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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]

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Questions?

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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

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