Time-Lapse Monitoring of Subsurface Fluid Flow using Parsimonious Seismic Interferometry

Handle URI:
http://hdl.handle.net/10754/625238
Title:
Time-Lapse Monitoring of Subsurface Fluid Flow using Parsimonious Seismic Interferometry
Authors:
Hanafy, Sherif; Li, Jing ( 0000-0002-7960-176X ) ; Schuster, Gerard T. ( 0000-0001-7532-1587 )
Abstract:
A typical small-scale seismic survey (such as 240 shot gathers) takes at least 16 working hours to be completed, which is a major obstacle in case of time-lapse monitoring experiments. This is especially true if the subject that needs to be monitored is rapidly changing. In this work, we will discuss how to decrease the recording time from 16 working hours to less than one hour of recording. Here, the virtual data has the same accuracy as the conventional data. We validate the efficacy of parsimonious seismic interferometry with the time-lapse mentoring idea with field examples, where we were able to record 30 different data sets within a 2-hour period. The recorded data are then processed to generate 30 snapshots that shows the spread of water from the ground surface down to a few meters.
KAUST Department:
KAUST
Citation:
Hanafy S, Li J, Schuster G (2017) TIME-LAPSE MONITORING OF SUBSURFACE FLUID FLOW USING PARSIMONIOUS SEISMIC INTERFEROMETRY. Symposium on the Application of Geophysics to Engineering and Environmental Problems 2017. Available: http://dx.doi.org/10.4133/sageep.30-047.
Publisher:
Society of Exploration Geophysicists and Environment and Engineering Geophysical Society
Journal:
Symposium on the Application of Geophysics to Engineering and Environmental Problems 2017
Issue Date:
21-Apr-2017
DOI:
10.4133/sageep.30-047
Type:
Conference Paper
Additional Links:
http://library.seg.org/doi/10.4133/SAGEEP.30-047
Appears in Collections:
Conference Papers

Full metadata record

DC FieldValue Language
dc.contributor.authorHanafy, Sherifen
dc.contributor.authorLi, Jingen
dc.contributor.authorSchuster, Gerard T.en
dc.date.accessioned2017-07-19T10:45:07Z-
dc.date.available2017-07-19T10:45:07Z-
dc.date.issued2017-04-21en
dc.identifier.citationHanafy S, Li J, Schuster G (2017) TIME-LAPSE MONITORING OF SUBSURFACE FLUID FLOW USING PARSIMONIOUS SEISMIC INTERFEROMETRY. Symposium on the Application of Geophysics to Engineering and Environmental Problems 2017. Available: http://dx.doi.org/10.4133/sageep.30-047.en
dc.identifier.doi10.4133/sageep.30-047en
dc.identifier.urihttp://hdl.handle.net/10754/625238-
dc.description.abstractA typical small-scale seismic survey (such as 240 shot gathers) takes at least 16 working hours to be completed, which is a major obstacle in case of time-lapse monitoring experiments. This is especially true if the subject that needs to be monitored is rapidly changing. In this work, we will discuss how to decrease the recording time from 16 working hours to less than one hour of recording. Here, the virtual data has the same accuracy as the conventional data. We validate the efficacy of parsimonious seismic interferometry with the time-lapse mentoring idea with field examples, where we were able to record 30 different data sets within a 2-hour period. The recorded data are then processed to generate 30 snapshots that shows the spread of water from the ground surface down to a few meters.en
dc.publisherSociety of Exploration Geophysicists and Environment and Engineering Geophysical Societyen
dc.relation.urlhttp://library.seg.org/doi/10.4133/SAGEEP.30-047en
dc.rightsArchived with thanks to Symposium on the Application of Geophysics to Engineering and Environmental Problems 2017en
dc.subjectRefractionen
dc.subjectInterferometryen
dc.subjectAcquisitionen
dc.subjectField Dataen
dc.titleTime-Lapse Monitoring of Subsurface Fluid Flow using Parsimonious Seismic Interferometryen
dc.typeConference Paperen
dc.contributor.departmentKAUSTen
dc.identifier.journalSymposium on the Application of Geophysics to Engineering and Environmental Problems 2017en
dc.eprint.versionPublisher's Version/PDFen
kaust.authorHanafy, Sherifen
kaust.authorLi, Jingen
kaust.authorSchuster, Gerard T.en
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