An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses

In this study we investigated the propagation of an induced hydraulic fracture experimentally. A true triaxial stress cell (TTSC) was used to apply three independent stresses of vertical, maximum and minimum horizontal to a cube of tight sandstone 100mm in size. A large stress anisotropy was applied...

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Main Authors: Gotti, A., Fallahzadeh, S., Rasouli, Vamegh
Other Authors: Prof Fuad Khoshnaw
Format: Conference Paper
Published: WITS Press 2012
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/37091
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author Gotti, A.
Fallahzadeh, S.
Rasouli, Vamegh
author2 Prof Fuad Khoshnaw
author_facet Prof Fuad Khoshnaw
Gotti, A.
Fallahzadeh, S.
Rasouli, Vamegh
author_sort Gotti, A.
building Curtin Institutional Repository
collection Online Access
description In this study we investigated the propagation of an induced hydraulic fracture experimentally. A true triaxial stress cell (TTSC) was used to apply three independent stresses of vertical, maximum and minimum horizontal to a cube of tight sandstone 100mm in size. A large stress anisotropy was applied in order to help the fracture to initiate more easily. Injection of the fracturing fluid was possible through a hole drilled at the centre of the sample which was plugged in top and bottom sections to give an openhole length of approximately 40mm in the sample centre. A pronounced notch was created in the direction of minimum horizontal stress, i.e. different than the direction at which the fracture intends to open naturally. The hydraulic fracturing tests were conducted on four different samples with different locations for the notch to investigate how the fracture would propagate from different starting angles. The results indicated that while the fracture initiates along the direction of the notch, it tends to rotate towards the maximum stress direction as it moves away from the wellbore wall. As a fracture is propagating through rock, it passes through inhomogeneities which cause a deviation in the propagation direction. The results showed that a fracture will still reorient to the direction of maximum stress after passing inhomogeneities not just at the wellbore wall, but throughout the rock. The complexity of hydraulic fracturing became apparent in this experiment as even in a highly controlled laboratory environment, some fractures propagated in directions that were unexpected. The presented results demonstrate the need for having a good understanding about the state of stresses when designing a hydraulic fracturing job for the field.
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institution Curtin University Malaysia
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publishDate 2012
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spelling curtin-20.500.11937-370912017-09-13T16:05:30Z An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses Gotti, A. Fallahzadeh, S. Rasouli, Vamegh Prof Fuad Khoshnaw hydraulic fracturing true triaxial stress cell fracture propagation direction fracture reorientation in-situ stresses In this study we investigated the propagation of an induced hydraulic fracture experimentally. A true triaxial stress cell (TTSC) was used to apply three independent stresses of vertical, maximum and minimum horizontal to a cube of tight sandstone 100mm in size. A large stress anisotropy was applied in order to help the fracture to initiate more easily. Injection of the fracturing fluid was possible through a hole drilled at the centre of the sample which was plugged in top and bottom sections to give an openhole length of approximately 40mm in the sample centre. A pronounced notch was created in the direction of minimum horizontal stress, i.e. different than the direction at which the fracture intends to open naturally. The hydraulic fracturing tests were conducted on four different samples with different locations for the notch to investigate how the fracture would propagate from different starting angles. The results indicated that while the fracture initiates along the direction of the notch, it tends to rotate towards the maximum stress direction as it moves away from the wellbore wall. As a fracture is propagating through rock, it passes through inhomogeneities which cause a deviation in the propagation direction. The results showed that a fracture will still reorient to the direction of maximum stress after passing inhomogeneities not just at the wellbore wall, but throughout the rock. The complexity of hydraulic fracturing became apparent in this experiment as even in a highly controlled laboratory environment, some fractures propagated in directions that were unexpected. The presented results demonstrate the need for having a good understanding about the state of stresses when designing a hydraulic fracturing job for the field. 2012 Conference Paper http://hdl.handle.net/20.500.11937/37091 10.2495/PMR120181 WITS Press restricted
spellingShingle hydraulic fracturing
true triaxial stress cell
fracture propagation direction
fracture reorientation
in-situ stresses
Gotti, A.
Fallahzadeh, S.
Rasouli, Vamegh
An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title_full An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title_fullStr An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title_full_unstemmed An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title_short An experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
title_sort experimental study to investigate hydraulic fracture reorientation with respect to principal stresses
topic hydraulic fracturing
true triaxial stress cell
fracture propagation direction
fracture reorientation
in-situ stresses
url http://hdl.handle.net/20.500.11937/37091