Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization

A series of tri-axial shear tests were carried out to determine the stress and strain characteristics, as well as the volume deformation of methane hydrate-bearing sediments during gas hydrate dissociation. An innovative type of depressurization was adopted with a high-pressure and low-temperature t...

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Published in:Energies
Main Authors: Li, Dongliang, Wu, Qi, Wang, Zhe, Lu, Jingsheng, Liang, Deqing, Li, Xiaosen
Format: Report
Language:English
Published: MDPI 2018
Subjects:
Online Access:http://ir.gig.ac.cn/handle/344008/39555
https://doi.org/10.3390/en11071819
id ftchacadscgigcas:oai:ir.gig.ac.cn:344008/39555
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spelling ftchacadscgigcas:oai:ir.gig.ac.cn:344008/39555 2023-05-15T17:11:39+02:00 Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization Li, Dongliang Wu, Qi Wang, Zhe Lu, Jingsheng Liang, Deqing Li, Xiaosen 2018-07-01 http://ir.gig.ac.cn/handle/344008/39555 https://doi.org/10.3390/en11071819 英语 eng MDPI ENERGIES http://ir.gig.ac.cn/handle/344008/39555 doi:10.3390/en11071819 Energy & Fuels tri-axial shear test hydrate-bearing sediments depressurization hydrate disassociation METHANE HYDRATE MECHANICAL-PROPERTIES SAND PRESSURE STRENGTH BEHAVIOR 期刊论文 2018 ftchacadscgigcas https://doi.org/10.3390/en11071819 2020-12-22T07:21:32Z A series of tri-axial shear tests were carried out to determine the stress and strain characteristics, as well as the volume deformation of methane hydrate-bearing sediments during gas hydrate dissociation. An innovative type of depressurization was adopted with a high-pressure and low-temperature tri-axial apparatus. Results show that: (1) decrease in pore pressure during the shear process may result in the failure of hydrate-bearing sediments, but they did not collapse completely due to high effective confining pressure; (2) depressurization leads to the contraction of volumetric strain and the ultimate deformation shows no difference compared to that prior depressurization; (3) high saturation hydrate-bearing sediments were more sensitive to depressurization, which could be due to the methane hydrate acting as a skeleton structure at some sites when the pore hydrates' saturation is high. Report Methane hydrate Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) Energies 11 7 1819
institution Open Polar
collection Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences)
op_collection_id ftchacadscgigcas
language English
topic Energy & Fuels
tri-axial shear test
hydrate-bearing sediments
depressurization
hydrate disassociation
METHANE HYDRATE
MECHANICAL-PROPERTIES
SAND
PRESSURE
STRENGTH
BEHAVIOR
spellingShingle Energy & Fuels
tri-axial shear test
hydrate-bearing sediments
depressurization
hydrate disassociation
METHANE HYDRATE
MECHANICAL-PROPERTIES
SAND
PRESSURE
STRENGTH
BEHAVIOR
Li, Dongliang
Wu, Qi
Wang, Zhe
Lu, Jingsheng
Liang, Deqing
Li, Xiaosen
Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
topic_facet Energy & Fuels
tri-axial shear test
hydrate-bearing sediments
depressurization
hydrate disassociation
METHANE HYDRATE
MECHANICAL-PROPERTIES
SAND
PRESSURE
STRENGTH
BEHAVIOR
description A series of tri-axial shear tests were carried out to determine the stress and strain characteristics, as well as the volume deformation of methane hydrate-bearing sediments during gas hydrate dissociation. An innovative type of depressurization was adopted with a high-pressure and low-temperature tri-axial apparatus. Results show that: (1) decrease in pore pressure during the shear process may result in the failure of hydrate-bearing sediments, but they did not collapse completely due to high effective confining pressure; (2) depressurization leads to the contraction of volumetric strain and the ultimate deformation shows no difference compared to that prior depressurization; (3) high saturation hydrate-bearing sediments were more sensitive to depressurization, which could be due to the methane hydrate acting as a skeleton structure at some sites when the pore hydrates' saturation is high.
format Report
author Li, Dongliang
Wu, Qi
Wang, Zhe
Lu, Jingsheng
Liang, Deqing
Li, Xiaosen
author_facet Li, Dongliang
Wu, Qi
Wang, Zhe
Lu, Jingsheng
Liang, Deqing
Li, Xiaosen
author_sort Li, Dongliang
title Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
title_short Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
title_full Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
title_fullStr Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
title_full_unstemmed Tri-Axial Shear Tests on Hydrate-Bearing Sediments during Hydrate Dissociation with Depressurization
title_sort tri-axial shear tests on hydrate-bearing sediments during hydrate dissociation with depressurization
publisher MDPI
publishDate 2018
url http://ir.gig.ac.cn/handle/344008/39555
https://doi.org/10.3390/en11071819
genre Methane hydrate
genre_facet Methane hydrate
op_relation ENERGIES
http://ir.gig.ac.cn/handle/344008/39555
doi:10.3390/en11071819
op_doi https://doi.org/10.3390/en11071819
container_title Energies
container_volume 11
container_issue 7
container_start_page 1819
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