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...
Published in: | Journal of Marine Science and Engineering |
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Main Authors: | , , , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2023
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Subjects: | |
Online Access: | https://doi.org/10.3390/jmse11040766 |
_version_ | 1821581458966315008 |
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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. |
format | Text |
genre | Methane hydrate |
genre_facet | Methane hydrate |
id | ftmdpi:oai:mdpi.com:/2077-1312/11/4/766/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
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 |
publishDate | 2023 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
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 |