Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales

Summary: Unlike the conceptual models, the natural hydrate spatial distribution in sediments is multitype and presents different coalescence degrees. In this study, we present pore-scale triaxial test results for hydrate-bearing sediments with different hydrate spatial distributions for the first ti...

Full description

Bibliographic Details
Main Authors: Yanghui Li, Peng Wu, Xiang Sun, Weiguo Liu, Yongchen Song
Format: Article
Language:English
Published: Elsevier 2021-05-01
Series:iScience
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2589004221004168
id doaj-6c34430354304fb18e38e637d669c82e
record_format Article
spelling doaj-6c34430354304fb18e38e637d669c82e2021-05-28T05:03:46ZengElsevieriScience2589-00422021-05-01245102448Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscalesYanghui Li0Peng Wu1Xiang Sun2Weiguo Liu3Yongchen Song4Key Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian, 116024, P. R. ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian, 116024, P. R. China; Corresponding authorKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian, 116024, P. R. ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian, 116024, P. R. ChinaKey Laboratory of Ocean Energy Utilization and Energy Conservation of Ministry of Education, Dalian University of Technology, Dalian, 116024, P. R. ChinaSummary: Unlike the conceptual models, the natural hydrate spatial distribution in sediments is multitype and presents different coalescence degrees. In this study, we present pore-scale triaxial test results for hydrate-bearing sediments with different hydrate spatial distributions for the first time. It shows that the specimen with a more dispersed hydrate distribution yields later and exhibits larger peak strength. Correspondingly, the localized deformation develops more slowly, and the shear band is steeper and thinner. The cementation failure in the specimen with a more dispersed hydrate distribution develops more slowly. However, the changing rate of the pore space characteristic does not seem to be affected by the hydrate spatial distribution. Moreover, the specimen with a more dispersed hydrate distribution has a larger hydrate-sand interfacial area, and further axial loading would increase it rapidly firstly, and then the increasing rate would be slowed down since the cementation structure failure.http://www.sciencedirect.com/science/article/pii/S2589004221004168Sediment GeochemistryMechanical PropertyMicrostructurePorous Material
collection DOAJ
language English
format Article
sources DOAJ
author Yanghui Li
Peng Wu
Xiang Sun
Weiguo Liu
Yongchen Song
spellingShingle Yanghui Li
Peng Wu
Xiang Sun
Weiguo Liu
Yongchen Song
Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
iScience
Sediment Geochemistry
Mechanical Property
Microstructure
Porous Material
author_facet Yanghui Li
Peng Wu
Xiang Sun
Weiguo Liu
Yongchen Song
author_sort Yanghui Li
title Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
title_short Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
title_full Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
title_fullStr Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
title_full_unstemmed Mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
title_sort mechanical behaviors of hydrate-bearing sediment with different cementation spatial distributions at microscales
publisher Elsevier
series iScience
issn 2589-0042
publishDate 2021-05-01
description Summary: Unlike the conceptual models, the natural hydrate spatial distribution in sediments is multitype and presents different coalescence degrees. In this study, we present pore-scale triaxial test results for hydrate-bearing sediments with different hydrate spatial distributions for the first time. It shows that the specimen with a more dispersed hydrate distribution yields later and exhibits larger peak strength. Correspondingly, the localized deformation develops more slowly, and the shear band is steeper and thinner. The cementation failure in the specimen with a more dispersed hydrate distribution develops more slowly. However, the changing rate of the pore space characteristic does not seem to be affected by the hydrate spatial distribution. Moreover, the specimen with a more dispersed hydrate distribution has a larger hydrate-sand interfacial area, and further axial loading would increase it rapidly firstly, and then the increasing rate would be slowed down since the cementation structure failure.
topic Sediment Geochemistry
Mechanical Property
Microstructure
Porous Material
url http://www.sciencedirect.com/science/article/pii/S2589004221004168
work_keys_str_mv AT yanghuili mechanicalbehaviorsofhydratebearingsedimentwithdifferentcementationspatialdistributionsatmicroscales
AT pengwu mechanicalbehaviorsofhydratebearingsedimentwithdifferentcementationspatialdistributionsatmicroscales
AT xiangsun mechanicalbehaviorsofhydratebearingsedimentwithdifferentcementationspatialdistributionsatmicroscales
AT weiguoliu mechanicalbehaviorsofhydratebearingsedimentwithdifferentcementationspatialdistributionsatmicroscales
AT yongchensong mechanicalbehaviorsofhydratebearingsedimentwithdifferentcementationspatialdistributionsatmicroscales
_version_ 1721424550713884672