A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice

The ice generation is one of the challenges facing the methane hydrate depressurization, which, however, has not been fully addressed by existing numerical models for hydrate-bearing sediments (HBS). In this study, we develop a high-fidelity, fully coupled thermo-hydro-mechanical-chemical numerical...

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Published in:Journal of Marine Science and Engineering
Main Authors: Fanbao Cheng, Xiang Sun, Peng Wu, Zhixiang Chen, Tao Yu, Weiguo Liu, Xin Ju, Yanghui Li
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/jmse11040766
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author Fanbao Cheng
Xiang Sun
Peng Wu
Zhixiang Chen
Tao Yu
Weiguo Liu
Xin Ju
Yanghui Li
author_facet Fanbao Cheng
Xiang Sun
Peng Wu
Zhixiang Chen
Tao Yu
Weiguo Liu
Xin Ju
Yanghui Li
author_sort Fanbao Cheng
collection MDPI Open Access Publishing
container_issue 4
container_start_page 766
container_title Journal of Marine Science and Engineering
container_volume 11
description The ice generation is one of the challenges facing the methane hydrate depressurization, which, however, has not been fully addressed by existing numerical models for hydrate-bearing sediments (HBS). In this study, we develop a high-fidelity, fully coupled thermo-hydro-mechanical-chemical numerical model that incorporates the effect of ice. The model, developed using COMSOL, takes into account water–ice phase change, thermally induced cryogenic suction and constitutive relation in HBS. It is verified well against the temperature, pressure and cumulative gas production of Masuda’s experiment. The model is then employed to investigate multiphysical responses and gas/water production when ice generation is induced by setting a low outlet pressure. The results reveal that ice forms near the outlet boundary of the specimen center, leading to a reduction in intrinsic permeability and fluid velocity and an increase in the bulk modulus of ice-HBS. This enhanced bulk modulus results in higher porosity under axial load. Although the exothermic effect of ice generation promotes the hydrate dissociation, the effect on cumulative gas production is negligible after the ice melts. A negative correlation between ice saturation and water production rate is observed, indicating that a higher gas–water ratio can be achieved by adjusting the ice duration during hydrate production. The developed coupled model proves to be crucial for understanding the effect of ice on hydrate exploitation.
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genre Methane hydrate
genre_facet Methane hydrate
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op_doi https://doi.org/10.3390/jmse11040766
op_relation Marine Energy
https://dx.doi.org/10.3390/jmse11040766
op_rights https://creativecommons.org/licenses/by/4.0/
op_source Journal of Marine Science and Engineering; Volume 11; Issue 4; Pages: 766
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spelling ftmdpi:oai:mdpi.com:/2077-1312/11/4/766/ 2025-01-16T23:04:50+00:00 A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice Fanbao Cheng Xiang Sun Peng Wu Zhixiang Chen Tao Yu Weiguo Liu Xin Ju Yanghui Li agris 2023-03-31 application/pdf https://doi.org/10.3390/jmse11040766 EN eng Multidisciplinary Digital Publishing Institute Marine Energy https://dx.doi.org/10.3390/jmse11040766 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 11; Issue 4; Pages: 766 ice-hydrate-bearing sediments coupled thermo-hydro-mechanical-chemical (THMC) model water–ice phase change compaction numerical simulation Text 2023 ftmdpi https://doi.org/10.3390/jmse11040766 2023-08-01T09:31:45Z The ice generation is one of the challenges facing the methane hydrate depressurization, which, however, has not been fully addressed by existing numerical models for hydrate-bearing sediments (HBS). In this study, we develop a high-fidelity, fully coupled thermo-hydro-mechanical-chemical numerical model that incorporates the effect of ice. The model, developed using COMSOL, takes into account water–ice phase change, thermally induced cryogenic suction and constitutive relation in HBS. It is verified well against the temperature, pressure and cumulative gas production of Masuda’s experiment. The model is then employed to investigate multiphysical responses and gas/water production when ice generation is induced by setting a low outlet pressure. The results reveal that ice forms near the outlet boundary of the specimen center, leading to a reduction in intrinsic permeability and fluid velocity and an increase in the bulk modulus of ice-HBS. This enhanced bulk modulus results in higher porosity under axial load. Although the exothermic effect of ice generation promotes the hydrate dissociation, the effect on cumulative gas production is negligible after the ice melts. A negative correlation between ice saturation and water production rate is observed, indicating that a higher gas–water ratio can be achieved by adjusting the ice duration during hydrate production. The developed coupled model proves to be crucial for understanding the effect of ice on hydrate exploitation. Text Methane hydrate MDPI Open Access Publishing Journal of Marine Science and Engineering 11 4 766
spellingShingle ice-hydrate-bearing sediments
coupled thermo-hydro-mechanical-chemical (THMC) model
water–ice phase change
compaction
numerical simulation
Fanbao Cheng
Xiang Sun
Peng Wu
Zhixiang Chen
Tao Yu
Weiguo Liu
Xin Ju
Yanghui Li
A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title_full A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title_fullStr A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title_full_unstemmed A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title_short A Fully Coupled Thermo-Hydro-Mechanical-Chemical Model for Methane Hydrate Bearing Sediments Considering the Effect of Ice
title_sort fully coupled thermo-hydro-mechanical-chemical model for methane hydrate bearing sediments considering the effect of ice
topic ice-hydrate-bearing sediments
coupled thermo-hydro-mechanical-chemical (THMC) model
water–ice phase change
compaction
numerical simulation
topic_facet ice-hydrate-bearing sediments
coupled thermo-hydro-mechanical-chemical (THMC) model
water–ice phase change
compaction
numerical simulation
url https://doi.org/10.3390/jmse11040766