Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration

4-D seismic techniques rely on measuring changes in velocity over time in order to detect changes during activities such as CO[subscript 2] flooding and storage in a reservoir. Wang et al. [1998] detail a laboratory study of the seismic detectability of CO[subscript 2] flooding in a series of carbon...

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Main Author: Brown, Stephen
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Language:en_US
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2014
Subjects:
Online Access:http://hdl.handle.net/1721.1/90449
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author Brown, Stephen
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
Brown, Stephen
author_sort Brown, Stephen
collection MIT
description 4-D seismic techniques rely on measuring changes in velocity over time in order to detect changes during activities such as CO[subscript 2] flooding and storage in a reservoir. Wang et al. [1998] detail a laboratory study of the seismic detectability of CO[subscript 2] flooding in a series of carbonate reservoir rocks taken from the McElroy field, West Texas. The basic findings of the paper suggest that while “ . . . laboratory results show that the largest V[subscript P] and V[subscript S] changes caused by CO[subscript 2] injection are associated with high-porosity, high-permeability rocks, . . . ” velocity changes in low-porosity (< 10%) and low-permeability carbonates are less than 1% and are undetectable using traditional 4-D seismic techniques.
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spelling mit-1721.1/904492019-04-10T21:28:31Z Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration Brown, Stephen Massachusetts Institute of Technology. Earth Resources Laboratory AVO CO2 Fluid flow 4-D seismic techniques rely on measuring changes in velocity over time in order to detect changes during activities such as CO[subscript 2] flooding and storage in a reservoir. Wang et al. [1998] detail a laboratory study of the seismic detectability of CO[subscript 2] flooding in a series of carbonate reservoir rocks taken from the McElroy field, West Texas. The basic findings of the paper suggest that while “ . . . laboratory results show that the largest V[subscript P] and V[subscript S] changes caused by CO[subscript 2] injection are associated with high-porosity, high-permeability rocks, . . . ” velocity changes in low-porosity (< 10%) and low-permeability carbonates are less than 1% and are undetectable using traditional 4-D seismic techniques. 2014-09-29T19:26:28Z 2014-09-29T19:26:28Z 2011 Technical Report http://hdl.handle.net/1721.1/90449 en_US Earth Resources Laboratory Industry Consortia Annual Report;2011-09 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle AVO
CO2
Fluid flow
Brown, Stephen
Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title_full Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title_fullStr Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title_full_unstemmed Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title_short Geophysical Monitoring of Multiple Phase Saturation of Rocks: Application to CO[subscript 2] Sequestration
title_sort geophysical monitoring of multiple phase saturation of rocks application to co subscript 2 sequestration
topic AVO
CO2
Fluid flow
url http://hdl.handle.net/1721.1/90449
work_keys_str_mv AT brownstephen geophysicalmonitoringofmultiplephasesaturationofrocksapplicationtocosubscript2sequestration