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Crosswell monitoring using virtual sources and horizontal wells

Authors
Byun, JoongmooYu, JeongminSeol, Soon Jee
Issue Date
May-2010
Publisher
Society of Exploration Geophysicists
Citation
Geophysics, v.75, no.3, pp SA37 - SA43
Indexed
SCI
SCIE
SCOPUS
Journal Title
Geophysics
Volume
75
Number
3
Start Page
SA37
End Page
SA43
URI
https://scholarworks.bwise.kr/hanyang/handle/2021.sw.hanyang/175037
DOI
10.1190/1.3427175
ISSN
0016-8033
1942-2156
Abstract
Time-lapse crosswell seismic provides an efficient way to monitor the migration of a CO(2) plume or its leakage after CO(2) injection into a geologic formation. Recently, crosswell seismic has become a powerful tool for monitoring underground variations, using the concept of a virtual source, with virtual sources positioned at the receivers installed in the well and thus the positions of sources and receivers can be invariant during monitoring. However, time-lapse crosswell seismic using vertical wells and virtual sources has difficulty in describing the front of a CO(2) plume, which usually is parallel to the vertical wells, and in obtaining sufficient ray coverage for the first-arrival tomography. These problems arise because of the theoretical downward-illumination-directivity limitation of the virtual source. We have developed an effective monitoring method that uses virtual sources and two horizontal wells: one above and one below the CO(2) sequestration reservoir. In our method, we redatum the traces that are recorded at geophones in horizontal wells from sources on the surface. The redatumed traces then become virtual traces recorded at geophones in the lower well and sent from virtual sources at the positions of the geophones in the upper well. The geometry of our method has advantages for locating the front of the CO(2) plume, which is normal to the horizontal wells, compared with either real or virtual sources. The method also is advantageous in acquiring full ray coverage between the wells, and that coverage is superior to coverage acquired using vertical crosswell seismic with virtual sources. In addition, we can avoid problems related to any potential change in the medium above the reservoir and in the source and receiver positions. The results of applying our method to synthetic data that simulate CO(2)-sequestration monitoring show that the front of a CO(2) plume in the reservoir is depicted accurately in a velocity tomogram. The new method also can be used to monitor a reservoir during production of heavy oil.
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