Stability Condition of Methane Hydrate in Fine-Grained Sediment

Stability condition is of critical importance for methane hydrate exploitation, transportation, and reserves. This study measured the stability conditions of methane hydrate in fine-grained sediment with different dry densities (ρd = 1.40, 1.50 and 1.60 g/cm3) and various initial water saturations b...

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Published in:Journal of Marine Science and Engineering
Main Authors: Di Lu, Qin Tang, Dehuan Yang, Rongtao Yan, Yun Chen, Shuai Tao
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/jmse11010196
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spelling ftmdpi:oai:mdpi.com:/2077-1312/11/1/196/ 2023-08-20T04:07:56+02:00 Stability Condition of Methane Hydrate in Fine-Grained Sediment Di Lu Qin Tang Dehuan Yang Rongtao Yan Yun Chen Shuai Tao agris 2023-01-12 application/pdf https://doi.org/10.3390/jmse11010196 EN eng Multidisciplinary Digital Publishing Institute Marine Energy https://dx.doi.org/10.3390/jmse11010196 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering; Volume 11; Issue 1; Pages: 196 fine-grained sediment methane hydrate stability conditions nuclear magnetic resonance phase equilibrium model Text 2023 ftmdpi https://doi.org/10.3390/jmse11010196 2023-08-01T08:16:16Z Stability condition is of critical importance for methane hydrate exploitation, transportation, and reserves. This study measured the stability conditions of methane hydrate in fine-grained sediment with different dry densities (ρd = 1.40, 1.50 and 1.60 g/cm3) and various initial water saturations by the multi-step heating method. The experimental result showed that the methane hydrate formation in fine-grained sediment required lower temperature and/or higher pressure compared to that in bulk state. At the same time, it is found that the deviation degree of P–T conditions of methane hydrate in fine-grained sediment with different dry density and initial water saturation are completely different from that in pure water. In addition, according to the nuclear magnetic resonance technique (NMR), the changes in NMR signal intensity during the formation and decomposition of methane hydrate in silt were analyzed. Regardless of formation and dissociation stages, liquid water always distributes in the small sediment pores. An empirical formula is developed to address the capillary suction of water and hydrate with respect to the unhydrated water within sediment. Furthermore, a phase equilibrium model is proposed to predict the stability conditions of hydrate-bearing fine-grained sediment. Text Methane hydrate MDPI Open Access Publishing Journal of Marine Science and Engineering 11 1 196
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic fine-grained sediment
methane hydrate
stability conditions
nuclear magnetic resonance
phase equilibrium model
spellingShingle fine-grained sediment
methane hydrate
stability conditions
nuclear magnetic resonance
phase equilibrium model
Di Lu
Qin Tang
Dehuan Yang
Rongtao Yan
Yun Chen
Shuai Tao
Stability Condition of Methane Hydrate in Fine-Grained Sediment
topic_facet fine-grained sediment
methane hydrate
stability conditions
nuclear magnetic resonance
phase equilibrium model
description Stability condition is of critical importance for methane hydrate exploitation, transportation, and reserves. This study measured the stability conditions of methane hydrate in fine-grained sediment with different dry densities (ρd = 1.40, 1.50 and 1.60 g/cm3) and various initial water saturations by the multi-step heating method. The experimental result showed that the methane hydrate formation in fine-grained sediment required lower temperature and/or higher pressure compared to that in bulk state. At the same time, it is found that the deviation degree of P–T conditions of methane hydrate in fine-grained sediment with different dry density and initial water saturation are completely different from that in pure water. In addition, according to the nuclear magnetic resonance technique (NMR), the changes in NMR signal intensity during the formation and decomposition of methane hydrate in silt were analyzed. Regardless of formation and dissociation stages, liquid water always distributes in the small sediment pores. An empirical formula is developed to address the capillary suction of water and hydrate with respect to the unhydrated water within sediment. Furthermore, a phase equilibrium model is proposed to predict the stability conditions of hydrate-bearing fine-grained sediment.
format Text
author Di Lu
Qin Tang
Dehuan Yang
Rongtao Yan
Yun Chen
Shuai Tao
author_facet Di Lu
Qin Tang
Dehuan Yang
Rongtao Yan
Yun Chen
Shuai Tao
author_sort Di Lu
title Stability Condition of Methane Hydrate in Fine-Grained Sediment
title_short Stability Condition of Methane Hydrate in Fine-Grained Sediment
title_full Stability Condition of Methane Hydrate in Fine-Grained Sediment
title_fullStr Stability Condition of Methane Hydrate in Fine-Grained Sediment
title_full_unstemmed Stability Condition of Methane Hydrate in Fine-Grained Sediment
title_sort stability condition of methane hydrate in fine-grained sediment
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/jmse11010196
op_coverage agris
genre Methane hydrate
genre_facet Methane hydrate
op_source Journal of Marine Science and Engineering; Volume 11; Issue 1; Pages: 196
op_relation Marine Energy
https://dx.doi.org/10.3390/jmse11010196
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/jmse11010196
container_title Journal of Marine Science and Engineering
container_volume 11
container_issue 1
container_start_page 196
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