A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments
Laboratory acoustic measurements of hydrate-bearing sediments serve as an important reference for the geological interpretation of seismic exploration data. Tetrahydrofuran (THF) hydrates are relatively easy to form with precise control of hydrate saturation, and they overcome the long time it takes...
Published in: | Journal of Marine Science and Engineering |
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Main Authors: | , , , , , , |
Format: | Text |
Language: | English |
Published: |
Multidisciplinary Digital Publishing Institute
2024
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Subjects: | |
Online Access: | https://doi.org/10.3390/jmse12122239 |
_version_ | 1821581205477261312 |
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author | Wengao Zhao Qingtao Bu Zihao Wang Tong Liu Qingguo Meng Yapeng Zhao Gaowei Hu |
author_facet | Wengao Zhao Qingtao Bu Zihao Wang Tong Liu Qingguo Meng Yapeng Zhao Gaowei Hu |
author_sort | Wengao Zhao |
collection | MDPI Open Access Publishing |
container_issue | 12 |
container_start_page | 2239 |
container_title | Journal of Marine Science and Engineering |
container_volume | 12 |
description | Laboratory acoustic measurements of hydrate-bearing sediments serve as an important reference for the geological interpretation of seismic exploration data. Tetrahydrofuran (THF) hydrates are relatively easy to form with precise control of hydrate saturation, and they overcome the long time it takes for methane in sediments to form hydrate. However, when THF hydrates are used as a substitute for methane hydrate, their acoustic properties yield different results. This study reports the results of a series of laboratory experiments on the formation of methane and THF hydrate in quartz sand and the evaluation of their acoustic properties. It compares the experimental results with the results of calculations from micro-distribution models of the four hydrates using effective medium theory (EMT). Methane hydrate formed by the excess gas method has higher acoustic velocities than THF hydrate at 0–80% saturation, but at 80–100% saturation, the situation reverses, with THF hydrate having a higher wave velocity. The methane hydrate synthesis process follows a mixed micro-distribution, with grain coating predominating at low saturations, the pore-filling mixing mode dominating at medium saturations, and grain coating dominating at high saturations. In addition, THF hydrate has a slow-velocity growth at low saturation and is dominated by a pore-filling model and a load-bearing model at high saturation. We compared our experimental data with a compilation of similar published results to confirm their reliability and support our conclusions. Both hydrate types exhibit distinct micro-distributions across different saturations. Therefore, when testing the elastic characteristics of hydrate sediments, the distinct hydrate synthesis methods and micro-distribution should be considered, especially when using THF hydrate as an alternative to methane hydrate. |
format | Text |
genre | Methane hydrate |
genre_facet | Methane hydrate |
id | ftmdpi:oai:mdpi.com:/2077-1312/12/12/2239/ |
institution | Open Polar |
language | English |
op_collection_id | ftmdpi |
op_coverage | agris |
op_doi | https://doi.org/10.3390/jmse12122239 |
op_relation | Geological Oceanography https://dx.doi.org/10.3390/jmse12122239 |
op_rights | https://creativecommons.org/licenses/by/4.0/ |
op_source | Journal of Marine Science and Engineering Volume 12 Issue 12 Pages: 2239 |
publishDate | 2024 |
publisher | Multidisciplinary Digital Publishing Institute |
record_format | openpolar |
spelling | ftmdpi:oai:mdpi.com:/2077-1312/12/12/2239/ 2025-01-16T23:04:30+00:00 A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments Wengao Zhao Qingtao Bu Zihao Wang Tong Liu Qingguo Meng Yapeng Zhao Gaowei Hu agris 2024-12-05 application/pdf https://doi.org/10.3390/jmse12122239 eng eng Multidisciplinary Digital Publishing Institute Geological Oceanography https://dx.doi.org/10.3390/jmse12122239 https://creativecommons.org/licenses/by/4.0/ Journal of Marine Science and Engineering Volume 12 Issue 12 Pages: 2239 methane hydrate THF hydrate acoustic characteristics hydrate saturation Text 2024 ftmdpi https://doi.org/10.3390/jmse12122239 2024-12-13T01:06:16Z Laboratory acoustic measurements of hydrate-bearing sediments serve as an important reference for the geological interpretation of seismic exploration data. Tetrahydrofuran (THF) hydrates are relatively easy to form with precise control of hydrate saturation, and they overcome the long time it takes for methane in sediments to form hydrate. However, when THF hydrates are used as a substitute for methane hydrate, their acoustic properties yield different results. This study reports the results of a series of laboratory experiments on the formation of methane and THF hydrate in quartz sand and the evaluation of their acoustic properties. It compares the experimental results with the results of calculations from micro-distribution models of the four hydrates using effective medium theory (EMT). Methane hydrate formed by the excess gas method has higher acoustic velocities than THF hydrate at 0–80% saturation, but at 80–100% saturation, the situation reverses, with THF hydrate having a higher wave velocity. The methane hydrate synthesis process follows a mixed micro-distribution, with grain coating predominating at low saturations, the pore-filling mixing mode dominating at medium saturations, and grain coating dominating at high saturations. In addition, THF hydrate has a slow-velocity growth at low saturation and is dominated by a pore-filling model and a load-bearing model at high saturation. We compared our experimental data with a compilation of similar published results to confirm their reliability and support our conclusions. Both hydrate types exhibit distinct micro-distributions across different saturations. Therefore, when testing the elastic characteristics of hydrate sediments, the distinct hydrate synthesis methods and micro-distribution should be considered, especially when using THF hydrate as an alternative to methane hydrate. Text Methane hydrate MDPI Open Access Publishing Journal of Marine Science and Engineering 12 12 2239 |
spellingShingle | methane hydrate THF hydrate acoustic characteristics hydrate saturation Wengao Zhao Qingtao Bu Zihao Wang Tong Liu Qingguo Meng Yapeng Zhao Gaowei Hu A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title | A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title_full | A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title_fullStr | A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title_full_unstemmed | A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title_short | A Comparative Study on Acoustic Characteristics of Methane and Tetrahydrofuran Hydrate-Bearing Sediments |
title_sort | comparative study on acoustic characteristics of methane and tetrahydrofuran hydrate-bearing sediments |
topic | methane hydrate THF hydrate acoustic characteristics hydrate saturation |
topic_facet | methane hydrate THF hydrate acoustic characteristics hydrate saturation |
url | https://doi.org/10.3390/jmse12122239 |