Methane hydrate cement induced anisotropy in granular sediments
Methane hydrate cement induced anisotropy in granular sediments
Gas hydrate dissociation is one of the factors that is considered to contribute towards initiation of submarine landslides and failure of hydrate reservoir, which may be linked to the reduction in stiffness and associated strength of sediments. Stiffness or wave velocity plays an important role in evaluating the stability of hydrate reservoirs, which is usually affected by the particle characteristics of sediment matrix. This article presents an experimental study to evaluate the loss of hydrate cement effect on stiffness for a range of granular materials with differing particle characteristics. Given similar effective stress and hydrate saturation, the stiffness of hydrate cemented granular soils not only depend on particle size of host sands, but also on size and shape of finer particles within the matrix. The results show that the presence of cemented hydrates induces anisotropy in the sediments, exhibited by increase in the horizontal stiffness, reduction in Poisson's ratio. The magnitude of anisotropy is governed by particle characteristics, where granular soils with lower specific surface and platy fines show greater degree of influence.
Luo, Tingting
60d5de9e-f7b0-41f3-b7f9-f2d977c6e615
Bangalore Narasimha Murthy, Madhusudhan
e139e3d3-2992-4579-b3f0-4eec3ddae98c
Song, Yongchen
c77e399a-c9dc-4402-b643-a4693c1f17cc
Luo, Tingting
60d5de9e-f7b0-41f3-b7f9-f2d977c6e615
Bangalore Narasimha Murthy, Madhusudhan
e139e3d3-2992-4579-b3f0-4eec3ddae98c
Song, Yongchen
c77e399a-c9dc-4402-b643-a4693c1f17cc
Luo, Tingting, Bangalore Narasimha Murthy, Madhusudhan and Song, Yongchen
(2021)
Methane hydrate cement induced anisotropy in granular sediments.
Journal of Geophysical Research: Solid Earth, [2021JB022609].
(Submitted)
Abstract
Gas hydrate dissociation is one of the factors that is considered to contribute towards initiation of submarine landslides and failure of hydrate reservoir, which may be linked to the reduction in stiffness and associated strength of sediments. Stiffness or wave velocity plays an important role in evaluating the stability of hydrate reservoirs, which is usually affected by the particle characteristics of sediment matrix. This article presents an experimental study to evaluate the loss of hydrate cement effect on stiffness for a range of granular materials with differing particle characteristics. Given similar effective stress and hydrate saturation, the stiffness of hydrate cemented granular soils not only depend on particle size of host sands, but also on size and shape of finer particles within the matrix. The results show that the presence of cemented hydrates induces anisotropy in the sediments, exhibited by increase in the horizontal stiffness, reduction in Poisson's ratio. The magnitude of anisotropy is governed by particle characteristics, where granular soils with lower specific surface and platy fines show greater degree of influence.
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Submitted date: 23 June 2021
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Local EPrints ID: 450014
URI: http://eprints.soton.ac.uk/id/eprint/450014
ISSN: 2169-9356
PURE UUID: 9bb7b7ba-6762-4ed6-bbb3-d8b04d9c71ce
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Date deposited: 05 Jul 2021 16:30
Last modified: 28 Feb 2024 02:53
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Author:
Tingting Luo
Author:
Yongchen Song
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