Direct laboratory observation of velocity-saturation relation transition during rocks saturation

Copyright © (2008) by the Society of Exploration Geophysicists All rights reserved. Ultrasonic velocities and fluid saturations are measured simultaneously during water injection into sandstone core samples. The experimental results obtained on low-permeability samples show that at low saturation va...

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Main Authors: Lebedev, Maxim, Gurevich, Boris, Toms, J., Clennel, B., Pervukhina, Marina, Mueller, T.
Format: Conference Paper
Published: 2018
Online Access:http://hdl.handle.net/20.500.11937/74796
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author Lebedev, Maxim
Gurevich, Boris
Toms, J.
Clennel, B.
Pervukhina, Marina
Mueller, T.
author_facet Lebedev, Maxim
Gurevich, Boris
Toms, J.
Clennel, B.
Pervukhina, Marina
Mueller, T.
author_sort Lebedev, Maxim
building Curtin Institutional Repository
collection Online Access
description Copyright © (2008) by the Society of Exploration Geophysicists All rights reserved. Ultrasonic velocities and fluid saturations are measured simultaneously during water injection into sandstone core samples. The experimental results obtained on low-permeability samples show that at low saturation values the velocity-saturation dependence can be described by the Gassmann-Wood relationship. However, with increasing saturation a sharp increase of P-wave velocity is observed, eventually approaching the Gassmann-Hill relationship. We relate this transition behavior to the change of the fluid distribution characteristics inferred from CT scans. In particular, we show that for relatively large fluid injection rate this transition occurs at smaller degrees of saturation as compared with high injection rate.
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institution Curtin University Malaysia
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publishDate 2018
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spelling curtin-20.500.11937-747962019-02-19T04:18:04Z Direct laboratory observation of velocity-saturation relation transition during rocks saturation Lebedev, Maxim Gurevich, Boris Toms, J. Clennel, B. Pervukhina, Marina Mueller, T. Copyright © (2008) by the Society of Exploration Geophysicists All rights reserved. Ultrasonic velocities and fluid saturations are measured simultaneously during water injection into sandstone core samples. The experimental results obtained on low-permeability samples show that at low saturation values the velocity-saturation dependence can be described by the Gassmann-Wood relationship. However, with increasing saturation a sharp increase of P-wave velocity is observed, eventually approaching the Gassmann-Hill relationship. We relate this transition behavior to the change of the fluid distribution characteristics inferred from CT scans. In particular, we show that for relatively large fluid injection rate this transition occurs at smaller degrees of saturation as compared with high injection rate. 2018 Conference Paper http://hdl.handle.net/20.500.11937/74796 restricted
spellingShingle Lebedev, Maxim
Gurevich, Boris
Toms, J.
Clennel, B.
Pervukhina, Marina
Mueller, T.
Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title_full Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title_fullStr Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title_full_unstemmed Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title_short Direct laboratory observation of velocity-saturation relation transition during rocks saturation
title_sort direct laboratory observation of velocity-saturation relation transition during rocks saturation
url http://hdl.handle.net/20.500.11937/74796