tan thesis defense 0814 final
TRANSCRIPT
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Two Dimensional Hydraulic Fracture
Simulations Using FRANC2D
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Vapor extraction well intersecting horizontal
hydraulic fracture, from Bradner (2002)
kfrx/k
10 100 1000 100001
10
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Importance of 2-D
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Objective
Develop and apply a model for predicting the
forms of curving hydraulic fractures in twodimensions
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Overview
Previous work
Vertical and horizontal fracture Analytical models
Theoretical Analysis Coupling mechanical and fluid flow analysis
Code Development Automatic propagation (EXC_AUTO_DRIVER_FLOW)
Fracture form calculation routines
Fluid flow simulation routines
Application Shallow soil model
Effects of layering and lateral residual compression
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Hydraulic Fracture Design
Vertical Fractures
a
Qh
X
Y
Z Horizontal Fractures
(a)
(d)(c)
(b)
a
Qd
Z
r
Q
a
d
Z
r
Y
Z
Q
h
X
a
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Previous Models
Pressure
Length
Aperture
time
time
time
1
1CtfP
2
2
Ctfa
3
3
Ctf
)],,,([ 3,2,1 QKEff
)2.05.0( 1 C
)44.025.0(2C
)5.011.0(3C
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Simulate Hydraulic Fracture
Fracture apertureanalyze as elastic
displacements due to fluid pressure
Fluid pressureanalyze as flow in
deforming fracture
Propagation
require stress intensity to
equal critical value
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Problem with Analysis in 2-D
Fracture curves-- numerical methods for
stress analysis required
Fracture propagation-- analyze as a series of
quasi static models. Requires many
analyses to be conducted.
Need FEM method with automaticregridding around fracture
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FRANC2D
2-D stress and displacement
Developed for structural
fracture mechanicsapplications
Auto regrid around
fracture Fluid flow within
fracture not included
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Fracture with Fluid Flow-
Coupled Approach
Modify FRANC2D to perform mechanical analysis,then calculate geometry of fracture, caused by fluidpressure, and other loadings
Fluid flow analysis adjust fluid pressure due to theshape changes of fracture, coupled with mechanicalanalysis
Propagation criterion:
is decided by fracture geometry and fluid
pressure
ICIKK
IK
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Flow and Deformation Coupling
Aperture
From 1-D implicit solution; flow bc at well, head bc at tip
From FEM elasticity solution
x
x
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Propagation
KI=Stress intensity factor
KI=KIc for propagation
KIC is material property, calledfracture toughness.
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How to ensure KI=KIc?
Pressu
re
Ptip
KI
Ptip
KIc
x
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Code Development
Fracture propagation control routine-EXC_AUTO_DRIVER_FLOW
Fracture geometry calculation routines-EXC_LENGTH_FLOW
-EXC_APER_FLOW
-EXC_VOLU_FLOW
Fluid flow simulation routines
-FLUID_FLOW_INIT
-FLUID_FLOW_CALC
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Automatic Propagation Subroutine
ICIKK
Fluid flow and mechanical analysis
coupling to decide pressure and geometry
Propagation criterion: KI=KIC
Auto-remesh around fracture tip
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Fracture Form Calculation
Length
EXC_LENGTH_FLOW Aperture EXC_APER_FLOW
Volume EXC_VOLU_FLOW
Obtain Crack node info Calculation in each segment, then integral
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Fluid Flow and Aperture
Subroutine
Calculate new heads using initial aperture
Calculate aperture using new head
Calculate heads using new aperture
Repeat and compare heads and apertures between
successive iterations
Converge when change is less than tolerance,usually less than 7 iterations
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Propagation Subroutine
Calculate KI for pressure at tip
Adjust pressure at tip slightly, redo fluid
pressure calculations, and calculate new KI
Use two values of KI and pressure tip to
interpolate new value of pressure tip that
should give KI=KIc
Check KI and revise pressure tip as needed
until KI is within tolerance of KIc
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Verification
Uniform Pressure: Model Setting
PInfinite elastic
media
Uniform
pressure
Radialsymmetric
a
z
r
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Verification-Driving Pressure
5
10
0 5 10 15
Time(min)
P
ressure(KPa)
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Verification (II): Fracture Length
1
3
5
0 5 10 15Time(min)
Length(m)
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Verification (III): Fracture Aperture
0.5
1.0
1.5
0 5 10 15
Time(min)
Aperture
(mm)
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Error Analysis
-0.08
-0.06
-0.04
-0.02
0
0.02
0.04
0.06
1 2 3 4 5
Length (m)
Relative
Error
Error PError aError d
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Applications
Hydraulic fracture in shallow soil:
- Gravity
- Fluid injection
Soil with under-lying softer material
Soil with high lateral residual stress
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Forms of Hydraulic Fractures
in the Field
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Field Data Adoption
Four cross-sectionselection
Each cross-section
starts from center of
fracture to the edge ofit, perpendicular with
each other
Fracture path, uplift,and sand extent data
are adopted
0 5 10 15feet
0.1
0.3
0.5
0.7
N
0.9
Cross 1
Cross 4
Cross 3
Cross 2
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General case-Model Setting
Depth
0 m
-2 m
12 m
-5 m
Distance from well0 m
frx-1.6 m
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Vertical Stress During Propagation
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Pressure Log
0
10
20
30
40
50
60
0 2 4 6 8
Time (minutes)
Pressure
(psi)
Measured
Simulated
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Fracture Form
-1.8
-1.5
-1.2
-0.9
0 1 2
Distance from center of fracture (m)
Depthbelow
grou
ndsurface
(m)
simulated
Well H Cross-s 1Well H Cross-s 2
Well H Cross-s 3
Well H Cross-s 4
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Aperture and Uplift
0.00
0.02
0 1 2 3 4
distance from center (m)
Uplift
fromf
ield,orsimulated
apertu
re
simulated
Well H cross 1
Well H cross 2
Well H cross 3
Well H cross 4
Average radial
extent of sand
(m)
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Effects of Layering
-2
-1.5
-1
-0.5
0
0 1 2 3 4 5
E2=2000psi, E1 = 5000psi
E1=E2=5000psi
E2=3000psi, E1=5000psi
E2=4000psi, E1=5000psi
Richardson
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Effects of Lateral compression
-1.8
-1.2
-0.6
0 1 2 3 4 5 6 7
Distance from Wellbore m
De
pth(m)
Fracture Path from lowresidual area
Fracture path from high
residual compressionregion
v
h
v
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Conclusions
FRANC2D has been modified to simulate
hydro-mechanical coupling conditions during
hydraulic fracturing.
A new simulation tool, HFRANC2D?, is
available
The model has been verified using analyticalsolutions, error within a few percent
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Conclusions, applications
Gentle bowl-like forms of hydraulic
fractures in shallow soils can be predicted.
Effects of state of stress and material
properties can be predicted and results
resemble field observations.