Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests

In this work, we validate a coupled flow-geomechanics simulator for gas hydrate deposits, named T+M AM , performing two meter-scale laboratory experiments of gas hydrates for production by depressurization, replicating the gas hydrate deposit in the Ulleung Basin, East Sea, South Korea. The first ex...

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Published in:International Journal of Rock Mechanics and Mining Sciences
Main Authors: Kim, Jihoon, Lee, Joo Yong, Ahn, Tae Woong, Yoon, Hyun Chul, Lee, Jaehyung, Yoon, Sangcheol, Moridis, George J.
Language:unknown
Published: 2023
Subjects:
Online Access:http://www.osti.gov/servlets/purl/1925178
https://www.osti.gov/biblio/1925178
https://doi.org/10.1016/j.ijrmms.2021.104958
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spelling ftosti:oai:osti.gov:1925178 2023-07-30T04:06:18+02:00 Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests Kim, Jihoon Lee, Joo Yong Ahn, Tae Woong Yoon, Hyun Chul Lee, Jaehyung Yoon, Sangcheol Moridis, George J. 2023-02-22 application/pdf http://www.osti.gov/servlets/purl/1925178 https://www.osti.gov/biblio/1925178 https://doi.org/10.1016/j.ijrmms.2021.104958 unknown http://www.osti.gov/servlets/purl/1925178 https://www.osti.gov/biblio/1925178 https://doi.org/10.1016/j.ijrmms.2021.104958 doi:10.1016/j.ijrmms.2021.104958 03 NATURAL GAS 02 PETROLEUM 58 GEOSCIENCES 2023 ftosti https://doi.org/10.1016/j.ijrmms.2021.104958 2023-07-11T10:19:46Z In this work, we validate a coupled flow-geomechanics simulator for gas hydrate deposits, named T+M AM , performing two meter-scale laboratory experiments of gas hydrates for production by depressurization, replicating the gas hydrate deposit in the Ulleung Basin, East Sea, South Korea. The first experiment with a sand-only specimen is a 1D 1 m-scale depressurization test based on the excess gas method, which represents the grain coating hydrate growth. On the other hand, the second is a 3D 1.5 m-scale test with the excess water method for a sand-mud alternating layer system, representing the pore filling hydrate growth. We measure production and displacement at the top with different depressurization levels. In particular, the 3D test exhibits high coupling strength of substantial deformation induced by incompressibility of water and high deformability of the specimen. For validation, we match pressure, flow rate, and displacement between the experimental data and numerical results. Thus, we identify that T+M AM is a reliable simulator, which can be applied to fields in both permafrost and deep oceanic hydrate deposits of strongly coupled flow and geomechanics systems. This validation also implies that other coupled simulators based on the same coupling formulation as T+M AM can be validated when individual flow and geomechanics simulators are stable and reliable. Other/Unknown Material permafrost SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) International Journal of Rock Mechanics and Mining Sciences 149 104958
institution Open Polar
collection SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy)
op_collection_id ftosti
language unknown
topic 03 NATURAL GAS
02 PETROLEUM
58 GEOSCIENCES
spellingShingle 03 NATURAL GAS
02 PETROLEUM
58 GEOSCIENCES
Kim, Jihoon
Lee, Joo Yong
Ahn, Tae Woong
Yoon, Hyun Chul
Lee, Jaehyung
Yoon, Sangcheol
Moridis, George J.
Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
topic_facet 03 NATURAL GAS
02 PETROLEUM
58 GEOSCIENCES
description In this work, we validate a coupled flow-geomechanics simulator for gas hydrate deposits, named T+M AM , performing two meter-scale laboratory experiments of gas hydrates for production by depressurization, replicating the gas hydrate deposit in the Ulleung Basin, East Sea, South Korea. The first experiment with a sand-only specimen is a 1D 1 m-scale depressurization test based on the excess gas method, which represents the grain coating hydrate growth. On the other hand, the second is a 3D 1.5 m-scale test with the excess water method for a sand-mud alternating layer system, representing the pore filling hydrate growth. We measure production and displacement at the top with different depressurization levels. In particular, the 3D test exhibits high coupling strength of substantial deformation induced by incompressibility of water and high deformability of the specimen. For validation, we match pressure, flow rate, and displacement between the experimental data and numerical results. Thus, we identify that T+M AM is a reliable simulator, which can be applied to fields in both permafrost and deep oceanic hydrate deposits of strongly coupled flow and geomechanics systems. This validation also implies that other coupled simulators based on the same coupling formulation as T+M AM can be validated when individual flow and geomechanics simulators are stable and reliable.
author Kim, Jihoon
Lee, Joo Yong
Ahn, Tae Woong
Yoon, Hyun Chul
Lee, Jaehyung
Yoon, Sangcheol
Moridis, George J.
author_facet Kim, Jihoon
Lee, Joo Yong
Ahn, Tae Woong
Yoon, Hyun Chul
Lee, Jaehyung
Yoon, Sangcheol
Moridis, George J.
author_sort Kim, Jihoon
title Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
title_short Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
title_full Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
title_fullStr Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
title_full_unstemmed Validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
title_sort validation of strongly coupled geomechanics and gas hydrate reservoir simulation with multiscale laboratory tests
publishDate 2023
url http://www.osti.gov/servlets/purl/1925178
https://www.osti.gov/biblio/1925178
https://doi.org/10.1016/j.ijrmms.2021.104958
genre permafrost
genre_facet permafrost
op_relation http://www.osti.gov/servlets/purl/1925178
https://www.osti.gov/biblio/1925178
https://doi.org/10.1016/j.ijrmms.2021.104958
doi:10.1016/j.ijrmms.2021.104958
op_doi https://doi.org/10.1016/j.ijrmms.2021.104958
container_title International Journal of Rock Mechanics and Mining Sciences
container_volume 149
container_start_page 104958
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