Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations
We performed a sequence of tests on a partially water-saturated sand sample contained in an x-ray transparent aluminum pressure vessel that is conducive to x-ray computed tomography (CT) observation. These tests were performed to gather data for estimation of thermal properties of the sand/water/gas...
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ftcdlib:qt3771s0xv 2023-05-15T17:12:00+02:00 Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations Kneafsey, Timothy J. Tomutsa, Liviu Moridis, George J. Seol, Yongkoo Freifeld, Barry Taylor, Charles E. Gupta, Arvind 2005-03-01 application/pdf http://www.escholarship.org/uc/item/3771s0xv english eng eScholarship, University of California qt3771s0xv http://www.escholarship.org/uc/item/3771s0xv public Kneafsey, Timothy J.; Tomutsa, Liviu; Moridis, George J.; Seol, Yongkoo; Freifeld, Barry; Taylor, Charles E.; et al.(2005). Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations. Lawrence Berkeley National Laboratory. Lawrence Berkeley National Laboratory: Lawrence Berkeley National Laboratory. Retrieved from: http://www.escholarship.org/uc/item/3771s0xv Earth Sciences Hydrate formation dissociation porous medium thermal stimulation depressurization x-ray computed tomography capillary pressure article 2005 ftcdlib 2016-04-02T18:32:31Z We performed a sequence of tests on a partially water-saturated sand sample contained in an x-ray transparent aluminum pressure vessel that is conducive to x-ray computed tomography (CT) observation. These tests were performed to gather data for estimation of thermal properties of the sand/water/gas system and the sand/hydrate/water/gas systems, as well as data to evaluate the kinetic nature of hydrate dissociation. The tests included mild thermal perturbations for the estimation of the thermal properties of the sand/water/gas system, hydrate formation, thermal perturbations with hydrate in the stability zone, hydrate dissociation through thermal stimulation, additional hydrate formation, and hydrate dissociation through depressurization with thermal stimulation. Density changes throughout the sample were observed as a result of hydrate formation and dissociation, and these processes induced capillary pressure changes that altered local water saturation. Article in Journal/Newspaper Methane hydrate University of California: eScholarship |
institution |
Open Polar |
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University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
English |
topic |
Earth Sciences Hydrate formation dissociation porous medium thermal stimulation depressurization x-ray computed tomography capillary pressure |
spellingShingle |
Earth Sciences Hydrate formation dissociation porous medium thermal stimulation depressurization x-ray computed tomography capillary pressure Kneafsey, Timothy J. Tomutsa, Liviu Moridis, George J. Seol, Yongkoo Freifeld, Barry Taylor, Charles E. Gupta, Arvind Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
topic_facet |
Earth Sciences Hydrate formation dissociation porous medium thermal stimulation depressurization x-ray computed tomography capillary pressure |
description |
We performed a sequence of tests on a partially water-saturated sand sample contained in an x-ray transparent aluminum pressure vessel that is conducive to x-ray computed tomography (CT) observation. These tests were performed to gather data for estimation of thermal properties of the sand/water/gas system and the sand/hydrate/water/gas systems, as well as data to evaluate the kinetic nature of hydrate dissociation. The tests included mild thermal perturbations for the estimation of the thermal properties of the sand/water/gas system, hydrate formation, thermal perturbations with hydrate in the stability zone, hydrate dissociation through thermal stimulation, additional hydrate formation, and hydrate dissociation through depressurization with thermal stimulation. Density changes throughout the sample were observed as a result of hydrate formation and dissociation, and these processes induced capillary pressure changes that altered local water saturation. |
format |
Article in Journal/Newspaper |
author |
Kneafsey, Timothy J. Tomutsa, Liviu Moridis, George J. Seol, Yongkoo Freifeld, Barry Taylor, Charles E. Gupta, Arvind |
author_facet |
Kneafsey, Timothy J. Tomutsa, Liviu Moridis, George J. Seol, Yongkoo Freifeld, Barry Taylor, Charles E. Gupta, Arvind |
author_sort |
Kneafsey, Timothy J. |
title |
Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
title_short |
Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
title_full |
Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
title_fullStr |
Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
title_full_unstemmed |
Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations |
title_sort |
methane hydrate formation and dissocation in a partially saturated sand--measurements and observations |
publisher |
eScholarship, University of California |
publishDate |
2005 |
url |
http://www.escholarship.org/uc/item/3771s0xv |
genre |
Methane hydrate |
genre_facet |
Methane hydrate |
op_source |
Kneafsey, Timothy J.; Tomutsa, Liviu; Moridis, George J.; Seol, Yongkoo; Freifeld, Barry; Taylor, Charles E.; et al.(2005). Methane Hydrate Formation and Dissocation in a Partially Saturated Sand--Measurements and Observations. Lawrence Berkeley National Laboratory. Lawrence Berkeley National Laboratory: Lawrence Berkeley National Laboratory. Retrieved from: http://www.escholarship.org/uc/item/3771s0xv |
op_relation |
qt3771s0xv http://www.escholarship.org/uc/item/3771s0xv |
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public |
_version_ |
1766068753268736000 |