Influence of temperature on methane hydrate formation

Abstract 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...

Full description

Bibliographic Details
Main Authors: Peng Zhang, Qingbai Wu, Cuicui Mu
Format: Article
Language:English
Published: Nature Publishing Group 2017-08-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-08430-y
id doaj-07e2ba43fb0d42e4bb332fb334a2a8a8
record_format Article
spelling doaj-07e2ba43fb0d42e4bb332fb334a2a8a82020-12-08T03:19:51ZengNature Publishing GroupScientific Reports2045-23222017-08-017111310.1038/s41598-017-08430-yInfluence of temperature on methane hydrate formationPeng Zhang0Qingbai Wu1Cuicui Mu2State Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesState Key Laboratory of Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of SciencesKey Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou UniversityAbstract 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.https://doi.org/10.1038/s41598-017-08430-y
collection DOAJ
language English
format Article
sources DOAJ
author Peng Zhang
Qingbai Wu
Cuicui Mu
spellingShingle Peng Zhang
Qingbai Wu
Cuicui Mu
Influence of temperature on methane hydrate formation
Scientific Reports
author_facet Peng Zhang
Qingbai Wu
Cuicui Mu
author_sort Peng Zhang
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
series Scientific Reports
issn 2045-2322
publishDate 2017-08-01
description Abstract 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.
url https://doi.org/10.1038/s41598-017-08430-y
work_keys_str_mv AT pengzhang influenceoftemperatureonmethanehydrateformation
AT qingbaiwu influenceoftemperatureonmethanehydrateformation
AT cuicuimu influenceoftemperatureonmethanehydrateformation
_version_ 1724392616071528448