Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters

Abstract Seismic bottom simulating reflections (BSR) analysis and seismic inversion are commonly used for gas hydrate reservoir interpretation. The relationship between gas hydrate saturation and elastic parameters can be influenced by gas hydrate occurrence state (e.g. pore-filling type gas hydrate...

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Published in:Journal of Geophysics and Engineering
Main Authors: Wu, Cunzhi, Han, Lei, Zhang, Feng, Liu, Junzhou, Chen, Haifeng, Di, Bangrang
Other Authors: National Natural Science Foundation of China, Foundation of Sinopec Key Laboratory of Seismic Elastic Wave Technology, CNPC
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2023
Subjects:
Rho
Online Access:http://dx.doi.org/10.1093/jge/gxac100
https://academic.oup.com/jge/article-pdf/20/1/117/48758593/gxac100.pdf
id croxfordunivpr:10.1093/jge/gxac100
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spelling croxfordunivpr:10.1093/jge/gxac100 2023-05-15T17:58:22+02:00 Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters Wu, Cunzhi Han, Lei Zhang, Feng Liu, Junzhou Chen, Haifeng Di, Bangrang National Natural Science Foundation of China Foundation of Sinopec Key Laboratory of Seismic Elastic Wave Technology CNPC 2023 http://dx.doi.org/10.1093/jge/gxac100 https://academic.oup.com/jge/article-pdf/20/1/117/48758593/gxac100.pdf en eng Oxford University Press (OUP) https://creativecommons.org/licenses/by/4.0/ CC-BY Journal of Geophysics and Engineering volume 20, issue 1, page 117-127 ISSN 1742-2132 1742-2140 Management, Monitoring, Policy and Law Industrial and Manufacturing Engineering Geology Geophysics journal-article 2023 croxfordunivpr https://doi.org/10.1093/jge/gxac100 2023-01-20T11:05:20Z Abstract Seismic bottom simulating reflections (BSR) analysis and seismic inversion are commonly used for gas hydrate reservoir interpretation. The relationship between gas hydrate saturation and elastic parameters can be influenced by gas hydrate occurrence state (e.g. pore-filling type gas hydrate or load-bearing type gas hydrate), and this may cause inaccurate interpretation. We first used the simplified three-phase Biot equation (STPBE) to model a formation containing two types of gas hydrate at the same time. Then the effects of occurrence state and authigenic minerals on the relationship between saturation and varied elastic parameters are analysed. Results show that bulk modulus (K), shear modulus ($\mu $), P-wave velocity (${V}_p$), S-wave velocity (${V}_s$), velocity ratio (${V}_p/{V}_s$), Poisson's ratio (v) and $\mu \rho $ increase at different rates with gas hydrate saturation, ${V}_p/{V}_s$ and v show relative higher sensitivity to occurrence state. Ratios of elastic parameter increments are further used to highlight the anomalies caused by gas hydrate. Four attributes ($\Delta K/\Delta \mu $, $\Delta {V}_p/\Delta {V}_s$, $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $) show good sensitivity to both gas hydrate saturation and occurrence state. $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $ can be used to distinguish gas hydrate with varied occurrence states from authigenic minerals (limestone, opal, pyrite and others). Two selected sensitive attributes $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $ are applied to well logs, four gas hydrate-bearing intervals in well 2L-38 from Mallik permafrost area in Canada and one gas hydrate-bearing interval in well A from Shenhu area in South China Sea are identified. These results are consistent with the interpreted result from the resistivity log using Archie's formula. This investigation may provide effective tools for the seismic interpretation of gas hydrate reservoirs. Article in Journal/Newspaper permafrost Oxford University Press (via Crossref) Canada Lambda ENVELOPE(-62.983,-62.983,-64.300,-64.300) Rho ENVELOPE(-63.000,-63.000,-64.300,-64.300) Journal of Geophysics and Engineering 20 1 117 127
institution Open Polar
collection Oxford University Press (via Crossref)
op_collection_id croxfordunivpr
language English
topic Management, Monitoring, Policy and Law
Industrial and Manufacturing Engineering
Geology
Geophysics
spellingShingle Management, Monitoring, Policy and Law
Industrial and Manufacturing Engineering
Geology
Geophysics
Wu, Cunzhi
Han, Lei
Zhang, Feng
Liu, Junzhou
Chen, Haifeng
Di, Bangrang
Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
topic_facet Management, Monitoring, Policy and Law
Industrial and Manufacturing Engineering
Geology
Geophysics
description Abstract Seismic bottom simulating reflections (BSR) analysis and seismic inversion are commonly used for gas hydrate reservoir interpretation. The relationship between gas hydrate saturation and elastic parameters can be influenced by gas hydrate occurrence state (e.g. pore-filling type gas hydrate or load-bearing type gas hydrate), and this may cause inaccurate interpretation. We first used the simplified three-phase Biot equation (STPBE) to model a formation containing two types of gas hydrate at the same time. Then the effects of occurrence state and authigenic minerals on the relationship between saturation and varied elastic parameters are analysed. Results show that bulk modulus (K), shear modulus ($\mu $), P-wave velocity (${V}_p$), S-wave velocity (${V}_s$), velocity ratio (${V}_p/{V}_s$), Poisson's ratio (v) and $\mu \rho $ increase at different rates with gas hydrate saturation, ${V}_p/{V}_s$ and v show relative higher sensitivity to occurrence state. Ratios of elastic parameter increments are further used to highlight the anomalies caused by gas hydrate. Four attributes ($\Delta K/\Delta \mu $, $\Delta {V}_p/\Delta {V}_s$, $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $) show good sensitivity to both gas hydrate saturation and occurrence state. $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $ can be used to distinguish gas hydrate with varied occurrence states from authigenic minerals (limestone, opal, pyrite and others). Two selected sensitive attributes $\Delta ({V}_p/{V}_s)/\Delta u $ and $\Delta \lambda \rho /\Delta \mu \rho $ are applied to well logs, four gas hydrate-bearing intervals in well 2L-38 from Mallik permafrost area in Canada and one gas hydrate-bearing interval in well A from Shenhu area in South China Sea are identified. These results are consistent with the interpreted result from the resistivity log using Archie's formula. This investigation may provide effective tools for the seismic interpretation of gas hydrate reservoirs.
author2 National Natural Science Foundation of China
Foundation of Sinopec Key Laboratory of Seismic Elastic Wave Technology
CNPC
format Article in Journal/Newspaper
author Wu, Cunzhi
Han, Lei
Zhang, Feng
Liu, Junzhou
Chen, Haifeng
Di, Bangrang
author_facet Wu, Cunzhi
Han, Lei
Zhang, Feng
Liu, Junzhou
Chen, Haifeng
Di, Bangrang
author_sort Wu, Cunzhi
title Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
title_short Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
title_full Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
title_fullStr Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
title_full_unstemmed Gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
title_sort gas hydrate reservoir identification based on rock physics modelling and sensitive elastic parameters
publisher Oxford University Press (OUP)
publishDate 2023
url http://dx.doi.org/10.1093/jge/gxac100
https://academic.oup.com/jge/article-pdf/20/1/117/48758593/gxac100.pdf
long_lat ENVELOPE(-62.983,-62.983,-64.300,-64.300)
ENVELOPE(-63.000,-63.000,-64.300,-64.300)
geographic Canada
Lambda
Rho
geographic_facet Canada
Lambda
Rho
genre permafrost
genre_facet permafrost
op_source Journal of Geophysics and Engineering
volume 20, issue 1, page 117-127
ISSN 1742-2132 1742-2140
op_rights https://creativecommons.org/licenses/by/4.0/
op_rightsnorm CC-BY
op_doi https://doi.org/10.1093/jge/gxac100
container_title Journal of Geophysics and Engineering
container_volume 20
container_issue 1
container_start_page 117
op_container_end_page 127
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