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...
Main Authors: | , , |
---|---|
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 |