Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation

Natural gas hydrate could be regarded as an alternative energy source in the future. Therefore, the investigation of the gas production from hydrate reservoirs is attracting extensive attention. In this work, a novel set-up was built to investigate sand production and sediment deformation during hyd...

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Main Authors: Yi Wang, Lei Zhan, Jing-Chun Feng, Xiao-Sen Li
Format: Article in Journal/Newspaper
Language:unknown
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Online Access:https://www.mdpi.com/1996-1073/12/22/4227/pdf
https://www.mdpi.com/1996-1073/12/22/4227/
id ftrepec:oai:RePEc:gam:jeners:v:12:y:2019:i:22:p:4227-:d:283988
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spelling ftrepec:oai:RePEc:gam:jeners:v:12:y:2019:i:22:p:4227-:d:283988 2024-04-14T08:14:52+00:00 Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation Yi Wang Lei Zhan Jing-Chun Feng Xiao-Sen Li https://www.mdpi.com/1996-1073/12/22/4227/pdf https://www.mdpi.com/1996-1073/12/22/4227/ unknown https://www.mdpi.com/1996-1073/12/22/4227/pdf https://www.mdpi.com/1996-1073/12/22/4227/ article ftrepec 2024-03-19T10:27:44Z Natural gas hydrate could be regarded as an alternative energy source in the future. Therefore, the investigation of the gas production from hydrate reservoirs is attracting extensive attention. In this work, a novel set-up was built to investigate sand production and sediment deformation during hydrate dissociation by heat stimulation. The influence of the particle sizes on the hydrate dissociation and sediment deformation was first investigated experimentally. The experimental results indicated that the rate of hydrate decomposition by heat stimulation was in proportion to the particle size of the sediment. The heat transfer rate and the energy efficiency decreased with the decrease of the particle size of the sediment. This was because higher permeability might lead to a larger sweep area of the fluid flow, which was beneficial for the supply of heat for hydrate dissociation. The sand production was found during hydrate dissociation by heat stimulation. The particle migration was due to the hydrodynamics of the water injection. The sand sediment expanded under the drive force from water injection and hydrate dissociation. Additionally, the smaller permeability led to the larger pressure difference leading to the larger sediment deformation. Because the sediment became loose after hydrate dissociation, small particle migration due to the hydrodynamics of the water injection could happen during the experiments. However, the sand production in the sediment with the larger particle size was more difficult, because the larger particles were harder to move due to the hydrodynamics, and the larger particles were harder to move across the holes on the production well with a diameter of 1 mm. Therefore, the sediment deformation during hydrate dissociation by heat stimulation should not be ignored. methane hydrate; thermal stimulation; sediment deformation; sandy sediment; particle size; sand production Article in Journal/Newspaper Methane hydrate RePEc (Research Papers in Economics)
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Natural gas hydrate could be regarded as an alternative energy source in the future. Therefore, the investigation of the gas production from hydrate reservoirs is attracting extensive attention. In this work, a novel set-up was built to investigate sand production and sediment deformation during hydrate dissociation by heat stimulation. The influence of the particle sizes on the hydrate dissociation and sediment deformation was first investigated experimentally. The experimental results indicated that the rate of hydrate decomposition by heat stimulation was in proportion to the particle size of the sediment. The heat transfer rate and the energy efficiency decreased with the decrease of the particle size of the sediment. This was because higher permeability might lead to a larger sweep area of the fluid flow, which was beneficial for the supply of heat for hydrate dissociation. The sand production was found during hydrate dissociation by heat stimulation. The particle migration was due to the hydrodynamics of the water injection. The sand sediment expanded under the drive force from water injection and hydrate dissociation. Additionally, the smaller permeability led to the larger pressure difference leading to the larger sediment deformation. Because the sediment became loose after hydrate dissociation, small particle migration due to the hydrodynamics of the water injection could happen during the experiments. However, the sand production in the sediment with the larger particle size was more difficult, because the larger particles were harder to move due to the hydrodynamics, and the larger particles were harder to move across the holes on the production well with a diameter of 1 mm. Therefore, the sediment deformation during hydrate dissociation by heat stimulation should not be ignored. methane hydrate; thermal stimulation; sediment deformation; sandy sediment; particle size; sand production
format Article in Journal/Newspaper
author Yi Wang
Lei Zhan
Jing-Chun Feng
Xiao-Sen Li
spellingShingle Yi Wang
Lei Zhan
Jing-Chun Feng
Xiao-Sen Li
Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
author_facet Yi Wang
Lei Zhan
Jing-Chun Feng
Xiao-Sen Li
author_sort Yi Wang
title Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
title_short Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
title_full Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
title_fullStr Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
title_full_unstemmed Influence of the Particle Size of Sandy Sediments on Heat and Mass Transfer Characteristics during Methane Hydrate Dissociation by Thermal Stimulation
title_sort influence of the particle size of sandy sediments on heat and mass transfer characteristics during methane hydrate dissociation by thermal stimulation
url https://www.mdpi.com/1996-1073/12/22/4227/pdf
https://www.mdpi.com/1996-1073/12/22/4227/
genre Methane hydrate
genre_facet Methane hydrate
op_relation https://www.mdpi.com/1996-1073/12/22/4227/pdf
https://www.mdpi.com/1996-1073/12/22/4227/
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