Shear-enhanced permeability and poroelastic deformation in unconsolidated sands

Heavy oil production depends on the understanding of mechanical and flow properties of unconsolidated or weakly consolidated sands under different loading paths and boundary conditions. Reconstituted bitumen-free Athabasca oil-sands samples were used to investigate the geomechanics of a steam inject...

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Main Author: Hamza, Syed Muhammad Farrukh
Format: Others
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/2152/ETD-UT-2012-08-6353
id ndltd-UTEXAS-oai-repositories.lib.utexas.edu-2152-ETD-UT-2012-08-6353
record_format oai_dc
collection NDLTD
language English
format Others
sources NDLTD
topic Steam Assisted Gravity Drainage
SAGD
Geomechanics laboratory experiments
SAGD lab experiments
Triaxial compression
Radial extension
Pore pressure increase
University of Texas at Austin Geomechanics
Jon Olson
SEM (Scanning Electron Microscope)
Steam injection
Thermal recovery methods
Athabasca oil sands
Oil-sands
Absolute permeability
Relative permeability
Initial water saturation
Residual oil saturation
Corey type curves
End-point relative permeability
Reservoir geomechanics
spellingShingle Steam Assisted Gravity Drainage
SAGD
Geomechanics laboratory experiments
SAGD lab experiments
Triaxial compression
Radial extension
Pore pressure increase
University of Texas at Austin Geomechanics
Jon Olson
SEM (Scanning Electron Microscope)
Steam injection
Thermal recovery methods
Athabasca oil sands
Oil-sands
Absolute permeability
Relative permeability
Initial water saturation
Residual oil saturation
Corey type curves
End-point relative permeability
Reservoir geomechanics
Hamza, Syed Muhammad Farrukh
Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
description Heavy oil production depends on the understanding of mechanical and flow properties of unconsolidated or weakly consolidated sands under different loading paths and boundary conditions. Reconstituted bitumen-free Athabasca oil-sands samples were used to investigate the geomechanics of a steam injection process such as the Steam Assisted Gravity Drainage (SAGD). Four stress paths have been studied in this work: triaxial compression, radial extension, pore pressure increase and isotropic compression. Absolute permeability, end-point relative permeability to oil & water (kro and krw), initial water saturation and residual oil saturation were measured while the samples deformed. Triaxial compression is a stress path of increasing mean stress while radial extension and pore pressure increase lead to decreasing mean stress. Pore pressure increase experiments were carried out for three initial states: equal axial and confining stresses, axial stress greater than confining stress and confining stress greater than axial stress. Pore pressure was increased under four boundary conditions: 1) constant axial and confining stress; 2) constant axial stress and zero radial strain; 3) zero axial strain and constant confining stress; and 4) zero axial and radial strain. These experiments were designed to mimic geologic conditions where vertical stress was either S1 or S3, the lateral boundary conditions were either zero strain or constant stress, and the vertical boundary conditions were either zero strain or constant stress. Triaxial compression caused a decrease in permeability as the sample compacted, followed by appreciable permeability enhancement during sample dilation. Radial extension led to sample dilation, shear failure and permeability increase from the beginning. The krw and kro increased by 40% and 15% post-compaction respectively for the samples corresponding to lower depths during triaxial compression. For these samples, residual oil saturation decreased by as much as 40%. For radial extension, the permeability enhancement decreased with depth and ranged from 20% to 50% while the residual oil saturation decreased by up to 55%. For both stress paths, more shear-enhanced permeability was observed for samples tested at lower pressures, implying that permeability enhancement is higher for shallower sands. The pore pressure increase experiments showed an increase of only 0-10% in absolute permeability except when the effective stress became close to zero. This could possibly have occurred due to steady state flow not being reached during absolute permeability measurement. The krw curves generally increased as the pore pressure was increased from 0 psi. The increase ranged from 5% to 44% for the different boundary conditions and differential stresses. The kro curves also showed an increasing trend for most of the cases. The residual oil saturation decreased by 40-60% for samples corresponding to shallow depths while it increased by 0-10% for samples corresponding to greater depths. The reservoirs with high differential stress are more conducive to favorable changes in permeability and residual oil saturation. These results suggested that a decreasing mean stress path is more beneficial for production increase than an increasing mean stress path. The unconsolidated sands are over-consolidated because of previous ice loading which makes the sand matrix stiffer. In this work, it was found that over-consolidation, as expected, decreased the porosity and permeability (40-50%) and increased the Young’s and bulk moduli of the sand. The result is sand which failed at higher than expected stress during triaxial compression. Overall, results show that lab experiments support increased permeability due to steam injection operations in heavy oil, and more importantly, the observed reduction in residual oil saturation implies SAGD induced deformation should improve recovery factors. === text
author Hamza, Syed Muhammad Farrukh
author_facet Hamza, Syed Muhammad Farrukh
author_sort Hamza, Syed Muhammad Farrukh
title Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
title_short Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
title_full Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
title_fullStr Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
title_full_unstemmed Shear-enhanced permeability and poroelastic deformation in unconsolidated sands
title_sort shear-enhanced permeability and poroelastic deformation in unconsolidated sands
publishDate 2012
url http://hdl.handle.net/2152/ETD-UT-2012-08-6353
work_keys_str_mv AT hamzasyedmuhammadfarrukh shearenhancedpermeabilityandporoelasticdeformationinunconsolidatedsands
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spelling ndltd-UTEXAS-oai-repositories.lib.utexas.edu-2152-ETD-UT-2012-08-63532015-09-20T17:11:44ZShear-enhanced permeability and poroelastic deformation in unconsolidated sandsHamza, Syed Muhammad FarrukhSteam Assisted Gravity DrainageSAGDGeomechanics laboratory experimentsSAGD lab experimentsTriaxial compressionRadial extensionPore pressure increaseUniversity of Texas at Austin GeomechanicsJon OlsonSEM (Scanning Electron Microscope)Steam injectionThermal recovery methodsAthabasca oil sandsOil-sandsAbsolute permeabilityRelative permeabilityInitial water saturationResidual oil saturationCorey type curvesEnd-point relative permeabilityReservoir geomechanicsHeavy oil production depends on the understanding of mechanical and flow properties of unconsolidated or weakly consolidated sands under different loading paths and boundary conditions. Reconstituted bitumen-free Athabasca oil-sands samples were used to investigate the geomechanics of a steam injection process such as the Steam Assisted Gravity Drainage (SAGD). Four stress paths have been studied in this work: triaxial compression, radial extension, pore pressure increase and isotropic compression. Absolute permeability, end-point relative permeability to oil & water (kro and krw), initial water saturation and residual oil saturation were measured while the samples deformed. Triaxial compression is a stress path of increasing mean stress while radial extension and pore pressure increase lead to decreasing mean stress. Pore pressure increase experiments were carried out for three initial states: equal axial and confining stresses, axial stress greater than confining stress and confining stress greater than axial stress. Pore pressure was increased under four boundary conditions: 1) constant axial and confining stress; 2) constant axial stress and zero radial strain; 3) zero axial strain and constant confining stress; and 4) zero axial and radial strain. These experiments were designed to mimic geologic conditions where vertical stress was either S1 or S3, the lateral boundary conditions were either zero strain or constant stress, and the vertical boundary conditions were either zero strain or constant stress. Triaxial compression caused a decrease in permeability as the sample compacted, followed by appreciable permeability enhancement during sample dilation. Radial extension led to sample dilation, shear failure and permeability increase from the beginning. The krw and kro increased by 40% and 15% post-compaction respectively for the samples corresponding to lower depths during triaxial compression. For these samples, residual oil saturation decreased by as much as 40%. For radial extension, the permeability enhancement decreased with depth and ranged from 20% to 50% while the residual oil saturation decreased by up to 55%. For both stress paths, more shear-enhanced permeability was observed for samples tested at lower pressures, implying that permeability enhancement is higher for shallower sands. The pore pressure increase experiments showed an increase of only 0-10% in absolute permeability except when the effective stress became close to zero. This could possibly have occurred due to steady state flow not being reached during absolute permeability measurement. The krw curves generally increased as the pore pressure was increased from 0 psi. The increase ranged from 5% to 44% for the different boundary conditions and differential stresses. The kro curves also showed an increasing trend for most of the cases. The residual oil saturation decreased by 40-60% for samples corresponding to shallow depths while it increased by 0-10% for samples corresponding to greater depths. The reservoirs with high differential stress are more conducive to favorable changes in permeability and residual oil saturation. These results suggested that a decreasing mean stress path is more beneficial for production increase than an increasing mean stress path. The unconsolidated sands are over-consolidated because of previous ice loading which makes the sand matrix stiffer. In this work, it was found that over-consolidation, as expected, decreased the porosity and permeability (40-50%) and increased the Young’s and bulk moduli of the sand. The result is sand which failed at higher than expected stress during triaxial compression. Overall, results show that lab experiments support increased permeability due to steam injection operations in heavy oil, and more importantly, the observed reduction in residual oil saturation implies SAGD induced deformation should improve recovery factors.text2012-11-06T20:24:14Z2012-11-06T20:24:14Z2012-082012-11-06August 20122012-11-06T20:25:18Zthesisapplication/pdfhttp://hdl.handle.net/2152/ETD-UT-2012-08-63532152/ETD-UT-2012-08-6353eng