Influence of temperature on methane hydrate formation

During gas hydrate formation process, a phase transition of liquid water exists naturally, implying that temperature has an important influence on hydrate formation. In this study, methane hydrate was formed within the same media. The experimental system was kept at 1.45, 6.49, and 12.91 °C respecti...

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Published in:Scientific Reports
Main Authors: Zhang, Peng, Wu, Qingbai, Mu, Cuicui
Format: Text
Language:English
Published: Nature Publishing Group UK 2017
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5554230/
http://www.ncbi.nlm.nih.gov/pubmed/28801566
https://doi.org/10.1038/s41598-017-08430-y
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spelling ftpubmed:oai:pubmedcentral.nih.gov:5554230 2023-05-15T17:11:50+02:00 Influence of temperature on methane hydrate formation Zhang, Peng Wu, Qingbai Mu, Cuicui 2017-08-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5554230/ http://www.ncbi.nlm.nih.gov/pubmed/28801566 https://doi.org/10.1038/s41598-017-08430-y en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5554230/ http://www.ncbi.nlm.nih.gov/pubmed/28801566 http://dx.doi.org/10.1038/s41598-017-08430-y © The Author(s) 2017 Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/. CC-BY Article Text 2017 ftpubmed https://doi.org/10.1038/s41598-017-08430-y 2017-08-20T00:13:45Z During gas hydrate formation process, a phase transition of liquid water exists naturally, implying that temperature has an important influence on hydrate formation. In this study, methane hydrate was formed within the same media. The experimental system was kept at 1.45, 6.49, and 12.91 °C respectively, and then different pressurization modes were applied in steps. We proposed a new indicator, namely the slope of the gas flow rates against time (dν g /dt), to represent the intrinsic driving force for hydrate formation. The driving force was calculated as a fixed value at the different stages of formation, including initial nucleation/growth, secondary nucleation/growth, and decay. The amounts of gas consumed at each stage were also calculated. The results show that the driving force during each stage follows an inverse relation with temperature, whereas the amount of consumed gas is proportional to temperature. This opposite trend indicates that the influences of temperature on the specific formation processes and final amounts of gas contained in hydrate should be considered separately. Our results also suggest that the specific ambient temperature under which hydrate is formed should be taken into consideration, when explaining the formation of different configurations and saturations of gas hydrates in natural reservoirs. Text Methane hydrate PubMed Central (PMC) Scientific Reports 7 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Zhang, Peng
Wu, Qingbai
Mu, Cuicui
Influence of temperature on methane hydrate formation
topic_facet Article
description During gas hydrate formation process, a phase transition of liquid water exists naturally, implying that temperature has an important influence on hydrate formation. In this study, methane hydrate was formed within the same media. The experimental system was kept at 1.45, 6.49, and 12.91 °C respectively, and then different pressurization modes were applied in steps. We proposed a new indicator, namely the slope of the gas flow rates against time (dν g /dt), to represent the intrinsic driving force for hydrate formation. The driving force was calculated as a fixed value at the different stages of formation, including initial nucleation/growth, secondary nucleation/growth, and decay. The amounts of gas consumed at each stage were also calculated. The results show that the driving force during each stage follows an inverse relation with temperature, whereas the amount of consumed gas is proportional to temperature. This opposite trend indicates that the influences of temperature on the specific formation processes and final amounts of gas contained in hydrate should be considered separately. Our results also suggest that the specific ambient temperature under which hydrate is formed should be taken into consideration, when explaining the formation of different configurations and saturations of gas hydrates in natural reservoirs.
format Text
author Zhang, Peng
Wu, Qingbai
Mu, Cuicui
author_facet Zhang, Peng
Wu, Qingbai
Mu, Cuicui
author_sort Zhang, Peng
title Influence of temperature on methane hydrate formation
title_short Influence of temperature on methane hydrate formation
title_full Influence of temperature on methane hydrate formation
title_fullStr Influence of temperature on methane hydrate formation
title_full_unstemmed Influence of temperature on methane hydrate formation
title_sort influence of temperature on methane hydrate formation
publisher Nature Publishing Group UK
publishDate 2017
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5554230/
http://www.ncbi.nlm.nih.gov/pubmed/28801566
https://doi.org/10.1038/s41598-017-08430-y
genre Methane hydrate
genre_facet Methane hydrate
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC5554230/
http://www.ncbi.nlm.nih.gov/pubmed/28801566
http://dx.doi.org/10.1038/s41598-017-08430-y
op_rights © The Author(s) 2017
Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.
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