The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application
Over recent years, there has been a growing interest in producing methane gas from hydrate-bearing sands (MHBS) located below the permafrost in arctic regions and offshore within continental margins. Geotechnical stability of production wellbores is one of the significant challenges during the gas e...
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ftpubmed:oai:pubmedcentral.nih.gov:8586339 2023-05-15T15:13:31+02:00 The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application Rake, Lior Pinkert, Shmulik 2021-11-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8586339/ http://www.ncbi.nlm.nih.gov/pubmed/34764309 https://doi.org/10.1038/s41598-021-00777-7 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8586339/ http://www.ncbi.nlm.nih.gov/pubmed/34764309 http://dx.doi.org/10.1038/s41598-021-00777-7 © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open AccessThis 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . CC-BY Sci Rep Article Text 2021 ftpubmed https://doi.org/10.1038/s41598-021-00777-7 2021-11-21T01:37:10Z Over recent years, there has been a growing interest in producing methane gas from hydrate-bearing sands (MHBS) located below the permafrost in arctic regions and offshore within continental margins. Geotechnical stability of production wellbores is one of the significant challenges during the gas extraction process. The vast majority of geotechnical investigations of MHBS have been conducted on laboratory-formed samples due to the complex procedure of undisturbed sample extraction. One of the most commonly used hydrate laboratory-formation methods is the excess-gas method. This work investigates fundamental aspects in the excess-gas formation of MHBS that are affecting the geotechnical interpretation and modeling. The work finds that (1) the measured temperature in the experimental system may be quite different from the in-sample temperature, and can reach 4 [Formula: see text] C difference during thermodynamic processes. This potential difference must be considered in investigation of hydrate formation or dissociation, (2) various calculation approaches may yield different hydrate saturation values of up to tens of percentages difference in high hydrate saturations. The calculation formulas are specified together with the fundamental difference between them, (3) the water mixture method during the sample assembling is critical for homogeneous MHBS laboratory formation, in which a maximum initial water content threshold of 9.1 to 1.3 % are obtained for a minimal fraction size of 0.01 to 0.8 mm, respectively, (4) the hydrate formation duration may influence the MHBS properties, and should be rigorously estimated according to the real-time gas consumption convergence. The outcomes of this work may contribute to the integration of data sets derived from various experiments for the study of MHBS mechanical behavior. Text Arctic Methane hydrate permafrost PubMed Central (PMC) Arctic Scientific Reports 11 1 |
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Article Rake, Lior Pinkert, Shmulik The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
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Article |
description |
Over recent years, there has been a growing interest in producing methane gas from hydrate-bearing sands (MHBS) located below the permafrost in arctic regions and offshore within continental margins. Geotechnical stability of production wellbores is one of the significant challenges during the gas extraction process. The vast majority of geotechnical investigations of MHBS have been conducted on laboratory-formed samples due to the complex procedure of undisturbed sample extraction. One of the most commonly used hydrate laboratory-formation methods is the excess-gas method. This work investigates fundamental aspects in the excess-gas formation of MHBS that are affecting the geotechnical interpretation and modeling. The work finds that (1) the measured temperature in the experimental system may be quite different from the in-sample temperature, and can reach 4 [Formula: see text] C difference during thermodynamic processes. This potential difference must be considered in investigation of hydrate formation or dissociation, (2) various calculation approaches may yield different hydrate saturation values of up to tens of percentages difference in high hydrate saturations. The calculation formulas are specified together with the fundamental difference between them, (3) the water mixture method during the sample assembling is critical for homogeneous MHBS laboratory formation, in which a maximum initial water content threshold of 9.1 to 1.3 % are obtained for a minimal fraction size of 0.01 to 0.8 mm, respectively, (4) the hydrate formation duration may influence the MHBS properties, and should be rigorously estimated according to the real-time gas consumption convergence. The outcomes of this work may contribute to the integration of data sets derived from various experiments for the study of MHBS mechanical behavior. |
format |
Text |
author |
Rake, Lior Pinkert, Shmulik |
author_facet |
Rake, Lior Pinkert, Shmulik |
author_sort |
Rake, Lior |
title |
The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
title_short |
The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
title_full |
The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
title_fullStr |
The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
title_full_unstemmed |
The ‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
title_sort |
‘excess gas’ method for laboratory formation of methane hydrate-bearing sand: geotechnical application |
publisher |
Nature Publishing Group UK |
publishDate |
2021 |
url |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8586339/ http://www.ncbi.nlm.nih.gov/pubmed/34764309 https://doi.org/10.1038/s41598-021-00777-7 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Methane hydrate permafrost |
genre_facet |
Arctic Methane hydrate permafrost |
op_source |
Sci Rep |
op_relation |
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC8586339/ http://www.ncbi.nlm.nih.gov/pubmed/34764309 http://dx.doi.org/10.1038/s41598-021-00777-7 |
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© The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open AccessThis 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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . |
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CC-BY |
op_doi |
https://doi.org/10.1038/s41598-021-00777-7 |
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