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...
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croxfordunivpr:10.1093/gji/ggaa452 2024-04-28T08:38:08+00:00 Time-lapse CSEM: how important is survey repeatability? Shantsev, Daniil V Nerland, Elias A Gelius, Leiv-J 2020 http://dx.doi.org/10.1093/gji/ggaa452 http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggaa452/33792244/ggaa452.pdf http://academic.oup.com/gji/article-pdf/223/3/2133/33885692/ggaa452.pdf en eng Oxford University Press (OUP) https://academic.oup.com/journals/pages/open_access/funder_policies/chorus/standard_publication_model Geophysical Journal International volume 223, issue 3, page 2133-2147 ISSN 0956-540X 1365-246X Geochemistry and Petrology Geophysics journal-article 2020 croxfordunivpr https://doi.org/10.1093/gji/ggaa452 2024-04-02T08:02:14Z 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 Oxford University Press Geophysical Journal International 223 3 2133 2147 |
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Open Polar |
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Oxford University Press |
op_collection_id |
croxfordunivpr |
language |
English |
topic |
Geochemistry and Petrology Geophysics |
spellingShingle |
Geochemistry and Petrology Geophysics Shantsev, Daniil V Nerland, Elias A Gelius, Leiv-J Time-lapse CSEM: how important is survey repeatability? |
topic_facet |
Geochemistry and Petrology Geophysics |
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 V Nerland, Elias A Gelius, Leiv-J |
author_facet |
Shantsev, Daniil V Nerland, Elias A Gelius, Leiv-J |
author_sort |
Shantsev, Daniil V |
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? |
publisher |
Oxford University Press (OUP) |
publishDate |
2020 |
url |
http://dx.doi.org/10.1093/gji/ggaa452 http://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggaa452/33792244/ggaa452.pdf http://academic.oup.com/gji/article-pdf/223/3/2133/33885692/ggaa452.pdf |
genre |
Snøhvit |
genre_facet |
Snøhvit |
op_source |
Geophysical Journal International volume 223, issue 3, page 2133-2147 ISSN 0956-540X 1365-246X |
op_rights |
https://academic.oup.com/journals/pages/open_access/funder_policies/chorus/standard_publication_model |
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 |
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1797569310570315776 |