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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Format: | Technical Report |
Language: | en_US |
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Massachusetts Institute of Technology. Earth Resources Laboratory
2014
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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. |
first_indexed | 2024-09-23T13:14:16Z |
format | Technical Report |
id | mit-1721.1/90449 |
institution | Massachusetts Institute of Technology |
language | en_US |
last_indexed | 2024-09-23T13:14:16Z |
publishDate | 2014 |
publisher | Massachusetts Institute of Technology. Earth Resources Laboratory |
record_format | dspace |
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 |