Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate

Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): B04106, doi:10.1029/2006JB004484. The mechanical b...

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Published in:Journal of Geophysical Research: Solid Earth
Main Authors: Yun, Tae Sup, Santamarina, J. Carlos, Ruppel, Carolyn D.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2007
Subjects:
Online Access:https://hdl.handle.net/1912/3809
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author Yun, Tae Sup
Santamarina, J. Carlos
Ruppel, Carolyn D.
author_facet Yun, Tae Sup
Santamarina, J. Carlos
Ruppel, Carolyn D.
author_sort Yun, Tae Sup
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
container_issue B4
container_title Journal of Geophysical Research: Solid Earth
container_volume 112
description Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): B04106, doi:10.1029/2006JB004484. The mechanical behavior of hydrate-bearing sediments subjected to large strains has relevance for the stability of the seafloor and submarine slopes, drilling and coring operations, and the analysis of certain small-strain properties of these sediments (for example, seismic velocities). This study reports on the results of comprehensive axial compression triaxial tests conducted at up to 1 MPa confining pressure on sand, crushed silt, precipitated silt, and clay specimens with closely controlled concentrations of synthetic hydrate. The results show that the stress-strain behavior of hydrate-bearing sediments is a complex function of particle size, confining pressure, and hydrate concentration. The mechanical properties of hydrate-bearing sediments at low hydrate concentration (probably < 40% of pore space) appear to be determined by stress-dependent soil stiffness and strength. At high hydrate concentrations (>50% of pore space), the behavior becomes more independent of stress because the hydrates control both stiffness and strength and possibly the dilative tendency of sediments by effectively increasing interparticle coordination, cementing particles together, and filling the pore space. The cementation contribution to the shear strength of hydrate-bearing sediments decreases with increasing specific surface of soil minerals. The lower the effective confining stress, the greater the impact of hydrate formation on normalized strength. This research was sponsored by a contract to C.R. and J.C.S. from the Joint Industry Project for Methane Hydrate, administered by ChevronTexaco with funding from award DE-FC26- 01NT41330 from DOE’s National Energy Technology Laboratory. The Goizueta Foundation at Georgia Tech also provided ...
format Article in Journal/Newspaper
genre Methane hydrate
genre_facet Methane hydrate
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Journal of Geophysical Research 112 (2007): B04106
https://hdl.handle.net/1912/3809
doi:10.1029/2006JB004484
op_source Journal of Geophysical Research 112 (2007): B04106
doi:10.1029/2006JB004484
publishDate 2007
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/3809 2025-01-16T23:05:10+00:00 Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate Yun, Tae Sup Santamarina, J. Carlos Ruppel, Carolyn D. 2007-04-17 application/pdf https://hdl.handle.net/1912/3809 en_US eng American Geophysical Union https://doi.org/10.1029/2006JB004484 Journal of Geophysical Research 112 (2007): B04106 https://hdl.handle.net/1912/3809 doi:10.1029/2006JB004484 Journal of Geophysical Research 112 (2007): B04106 doi:10.1029/2006JB004484 Gas hydrate Sediment strength Elasticity Mechanical behavior Stiffness Article 2007 ftwhoas https://doi.org/10.1029/2006JB004484 2022-05-28T22:58:04Z Author Posting. © American Geophysical Union, 2007. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research 112 (2007): B04106, doi:10.1029/2006JB004484. The mechanical behavior of hydrate-bearing sediments subjected to large strains has relevance for the stability of the seafloor and submarine slopes, drilling and coring operations, and the analysis of certain small-strain properties of these sediments (for example, seismic velocities). This study reports on the results of comprehensive axial compression triaxial tests conducted at up to 1 MPa confining pressure on sand, crushed silt, precipitated silt, and clay specimens with closely controlled concentrations of synthetic hydrate. The results show that the stress-strain behavior of hydrate-bearing sediments is a complex function of particle size, confining pressure, and hydrate concentration. The mechanical properties of hydrate-bearing sediments at low hydrate concentration (probably < 40% of pore space) appear to be determined by stress-dependent soil stiffness and strength. At high hydrate concentrations (>50% of pore space), the behavior becomes more independent of stress because the hydrates control both stiffness and strength and possibly the dilative tendency of sediments by effectively increasing interparticle coordination, cementing particles together, and filling the pore space. The cementation contribution to the shear strength of hydrate-bearing sediments decreases with increasing specific surface of soil minerals. The lower the effective confining stress, the greater the impact of hydrate formation on normalized strength. This research was sponsored by a contract to C.R. and J.C.S. from the Joint Industry Project for Methane Hydrate, administered by ChevronTexaco with funding from award DE-FC26- 01NT41330 from DOE’s National Energy Technology Laboratory. The Goizueta Foundation at Georgia Tech also provided ... Article in Journal/Newspaper Methane hydrate Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Journal of Geophysical Research: Solid Earth 112 B4
spellingShingle Gas hydrate
Sediment strength
Elasticity
Mechanical behavior
Stiffness
Yun, Tae Sup
Santamarina, J. Carlos
Ruppel, Carolyn D.
Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title_full Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title_fullStr Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title_full_unstemmed Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title_short Mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
title_sort mechanical properties of sand, silt, and clay containing tetrahydrofuran hydrate
topic Gas hydrate
Sediment strength
Elasticity
Mechanical behavior
Stiffness
topic_facet Gas hydrate
Sediment strength
Elasticity
Mechanical behavior
Stiffness
url https://hdl.handle.net/1912/3809