Time-lapse CSEM: how important is survey repeatability?

SUMMARY An important concern for time-lapse studies using the controlled-source electromagnetic (CSEM) method is repeatability of acquisition parameters for the base and monitoring surveys. We consider a challenging case when variations in source and receiver positions, conductivity of seawater, etc...

Full description

Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Shantsev, Daniil, Nerland, Elias A, Gelius, Leiv-J
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Online Access:http://hdl.handle.net/10852/84067
http://urn.nb.no/URN:NBN:no-86824
https://doi.org/10.1093/gji/ggaa452
id ftoslouniv:oai:www.duo.uio.no:10852/84067
record_format openpolar
spelling ftoslouniv:oai:www.duo.uio.no:10852/84067 2023-05-15T18:20:13+02:00 Time-lapse CSEM: how important is survey repeatability? Shantsev, Daniil Nerland, Elias A Gelius, Leiv-J 2020-10-06T17:21:51Z http://hdl.handle.net/10852/84067 http://urn.nb.no/URN:NBN:no-86824 https://doi.org/10.1093/gji/ggaa452 EN eng http://urn.nb.no/URN:NBN:no-86824 Shantsev, Daniil Nerland, Elias A Gelius, Leiv-J . Time-lapse CSEM: how important is survey repeatability?. Geophysical Journal International. 2020, 223(3), 2133-2147 http://hdl.handle.net/10852/84067 1837705 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical Journal International&rft.volume=223&rft.spage=2133&rft.date=2020 Geophysical Journal International 223 3 2133 2147 https://doi.org/10.1093/gji/ggaa452 URN:NBN:no-86824 Fulltext https://www.duo.uio.no/bitstream/handle/10852/84067/1/ggaa452.pdf 0956-540X Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2020 ftoslouniv https://doi.org/10.1093/gji/ggaa452 2021-03-17T23:31:02Z SUMMARY An important concern for time-lapse studies using the controlled-source electromagnetic (CSEM) method is repeatability of acquisition parameters for the base and monitoring surveys. We consider a challenging case when variations in source and receiver positions, conductivity of seawater, etc. will lead to differences in the recorded EM fields that exceed EM response due to production-induced changes in the reservoir resistivity. We show that even in that case, 4-D response can often be clearly resolved if the base and monitor EM data sets are inverted to produce 3-D resistivity distributions. More precisely, for a synthetic model of the Snøhvit gas field, changes in the inverted resistivity maps caused by such non-repeatability will be at least 10 times smaller than the time-lapse differences in the reservoir resistivity. By contrast, measurement errors and poor knowledge of background resistivity may reduce the resolution of 4-D CSEM to a much stronger degree. Analysis of field CSEM data from the Wisting oil field supports our conclusion about strongly relaxed repeatability requirements when 4-D effects are established by examining inverted resistivity volumes rather than by looking at raw EM data. Article in Journal/Newspaper Snøhvit Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Geophysical Journal International 223 3 2133 2147
institution Open Polar
collection Universitet i Oslo: Digitale utgivelser ved UiO (DUO)
op_collection_id ftoslouniv
language English
description SUMMARY An important concern for time-lapse studies using the controlled-source electromagnetic (CSEM) method is repeatability of acquisition parameters for the base and monitoring surveys. We consider a challenging case when variations in source and receiver positions, conductivity of seawater, etc. will lead to differences in the recorded EM fields that exceed EM response due to production-induced changes in the reservoir resistivity. We show that even in that case, 4-D response can often be clearly resolved if the base and monitor EM data sets are inverted to produce 3-D resistivity distributions. More precisely, for a synthetic model of the Snøhvit gas field, changes in the inverted resistivity maps caused by such non-repeatability will be at least 10 times smaller than the time-lapse differences in the reservoir resistivity. By contrast, measurement errors and poor knowledge of background resistivity may reduce the resolution of 4-D CSEM to a much stronger degree. Analysis of field CSEM data from the Wisting oil field supports our conclusion about strongly relaxed repeatability requirements when 4-D effects are established by examining inverted resistivity volumes rather than by looking at raw EM data.
format Article in Journal/Newspaper
author Shantsev, Daniil
Nerland, Elias A
Gelius, Leiv-J
spellingShingle Shantsev, Daniil
Nerland, Elias A
Gelius, Leiv-J
Time-lapse CSEM: how important is survey repeatability?
author_facet Shantsev, Daniil
Nerland, Elias A
Gelius, Leiv-J
author_sort Shantsev, Daniil
title Time-lapse CSEM: how important is survey repeatability?
title_short Time-lapse CSEM: how important is survey repeatability?
title_full Time-lapse CSEM: how important is survey repeatability?
title_fullStr Time-lapse CSEM: how important is survey repeatability?
title_full_unstemmed Time-lapse CSEM: how important is survey repeatability?
title_sort time-lapse csem: how important is survey repeatability?
publishDate 2020
url http://hdl.handle.net/10852/84067
http://urn.nb.no/URN:NBN:no-86824
https://doi.org/10.1093/gji/ggaa452
genre Snøhvit
genre_facet Snøhvit
op_source 0956-540X
op_relation http://urn.nb.no/URN:NBN:no-86824
Shantsev, Daniil Nerland, Elias A Gelius, Leiv-J . Time-lapse CSEM: how important is survey repeatability?. Geophysical Journal International. 2020, 223(3), 2133-2147
http://hdl.handle.net/10852/84067
1837705
info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Geophysical Journal International&rft.volume=223&rft.spage=2133&rft.date=2020
Geophysical Journal International
223
3
2133
2147
https://doi.org/10.1093/gji/ggaa452
URN:NBN:no-86824
Fulltext https://www.duo.uio.no/bitstream/handle/10852/84067/1/ggaa452.pdf
op_doi https://doi.org/10.1093/gji/ggaa452
container_title Geophysical Journal International
container_volume 223
container_issue 3
container_start_page 2133
op_container_end_page 2147
_version_ 1766197704309866496