Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations

The kinetics of methane hydrate formation in marine sediments with different water saturations are important to assess the feasibility of the hydrate production and understand the process of the secondary hydrate formation in the gas production from hydrate reservoir. In this paper, the behaviors of...

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Published in:Energies
Main Authors: Zhang, Yu, Li, Xiaosen, Wang, Yi, Chen, Zhaoyang, Li, Gang
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
BED
Online Access:http://ir.giec.ac.cn/handle/344007/14113
https://doi.org/10.3390/en10040561
id ftchacadsciegiec:oai:ir.giec.ac.cn:344007/14113
record_format openpolar
spelling ftchacadsciegiec:oai:ir.giec.ac.cn:344007/14113 2023-05-15T17:11:43+02:00 Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations Zhang, Yu Li, Xiaosen Wang, Yi Chen, Zhaoyang Li, Gang 2017-04-01 http://ir.giec.ac.cn/handle/344007/14113 https://doi.org/10.3390/en10040561 英语 eng ENERGIES http://ir.giec.ac.cn/handle/344007/14113 doi:10.3390/en10040561 Marine Sediments Methane Hydrate Formation Behavior Water Saturation Science & Technology Technology Energy & Fuels POROUS-MEDIA GAS-PRODUCTION DISSOCIATION BEHAVIOR DEPRESSURIZATION DEPOSITS GROWTH SIZES BED Article 期刊论文 2017 ftchacadsciegiec https://doi.org/10.3390/en10040561 2022-09-23T14:12:47Z The kinetics of methane hydrate formation in marine sediments with different water saturations are important to assess the feasibility of the hydrate production and understand the process of the secondary hydrate formation in the gas production from hydrate reservoir. In this paper, the behaviors of methane hydrate formation in marine sediments from the South China Sea at different water saturation levels were experimentally studied in isobaric conditions. The marine sediments used in the experiments have the mean pore diameter of 12.178 nm, total pore volume of 4.997 x 10(-2) mL/g and surface area of 16.412 m(2)/g. The volume fraction of water in the marine sediments ranges from 30% to 50%. The hydrate formation rate and the final water conversion increase with the decrease of the formation temperature at the water saturation of 40%. At the same experimental conditions, the hydrate formation rate decreases with the increase of the water saturation from 40% to 50% due to the reduction of the gas diffusion speed. At the water saturation of 30%, the hydrate formation rate is lower than that at the water saturation of 40% due to the effect of the equilibrium hydrate formation pressure, which increases with the decrease of the water saturation. The final water conversion is shown to increase with the increase of the water saturation, even the formation process at higher water did not end. The experiments at low water saturation show a better repeatability than that at high water saturation. Article in Journal/Newspaper Methane hydrate Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences: GIEC OpenIR Energies 10 4 561
institution Open Polar
collection Guangzhou Institute of Energy Conversion, Chinese Academy of Sciences: GIEC OpenIR
op_collection_id ftchacadsciegiec
language English
topic Marine Sediments
Methane Hydrate
Formation Behavior
Water Saturation
Science & Technology
Technology
Energy & Fuels
POROUS-MEDIA
GAS-PRODUCTION
DISSOCIATION BEHAVIOR
DEPRESSURIZATION
DEPOSITS
GROWTH
SIZES
BED
spellingShingle Marine Sediments
Methane Hydrate
Formation Behavior
Water Saturation
Science & Technology
Technology
Energy & Fuels
POROUS-MEDIA
GAS-PRODUCTION
DISSOCIATION BEHAVIOR
DEPRESSURIZATION
DEPOSITS
GROWTH
SIZES
BED
Zhang, Yu
Li, Xiaosen
Wang, Yi
Chen, Zhaoyang
Li, Gang
Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
topic_facet Marine Sediments
Methane Hydrate
Formation Behavior
Water Saturation
Science & Technology
Technology
Energy & Fuels
POROUS-MEDIA
GAS-PRODUCTION
DISSOCIATION BEHAVIOR
DEPRESSURIZATION
DEPOSITS
GROWTH
SIZES
BED
description The kinetics of methane hydrate formation in marine sediments with different water saturations are important to assess the feasibility of the hydrate production and understand the process of the secondary hydrate formation in the gas production from hydrate reservoir. In this paper, the behaviors of methane hydrate formation in marine sediments from the South China Sea at different water saturation levels were experimentally studied in isobaric conditions. The marine sediments used in the experiments have the mean pore diameter of 12.178 nm, total pore volume of 4.997 x 10(-2) mL/g and surface area of 16.412 m(2)/g. The volume fraction of water in the marine sediments ranges from 30% to 50%. The hydrate formation rate and the final water conversion increase with the decrease of the formation temperature at the water saturation of 40%. At the same experimental conditions, the hydrate formation rate decreases with the increase of the water saturation from 40% to 50% due to the reduction of the gas diffusion speed. At the water saturation of 30%, the hydrate formation rate is lower than that at the water saturation of 40% due to the effect of the equilibrium hydrate formation pressure, which increases with the decrease of the water saturation. The final water conversion is shown to increase with the increase of the water saturation, even the formation process at higher water did not end. The experiments at low water saturation show a better repeatability than that at high water saturation.
format Article in Journal/Newspaper
author Zhang, Yu
Li, Xiaosen
Wang, Yi
Chen, Zhaoyang
Li, Gang
author_facet Zhang, Yu
Li, Xiaosen
Wang, Yi
Chen, Zhaoyang
Li, Gang
author_sort Zhang, Yu
title Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
title_short Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
title_full Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
title_fullStr Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
title_full_unstemmed Methane Hydrate Formation in Marine Sediment from South China Sea with Different Water Saturations
title_sort methane hydrate formation in marine sediment from south china sea with different water saturations
publishDate 2017
url http://ir.giec.ac.cn/handle/344007/14113
https://doi.org/10.3390/en10040561
genre Methane hydrate
genre_facet Methane hydrate
op_relation ENERGIES
http://ir.giec.ac.cn/handle/344007/14113
doi:10.3390/en10040561
op_doi https://doi.org/10.3390/en10040561
container_title Energies
container_volume 10
container_issue 4
container_start_page 561
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