The impact of mono-ethylene glycol and kinetic inhibitors on methane hydrate formation

2021 ◽  
pp. 131531
Author(s):  
Vincent W.S. Lim ◽  
Peter J. Metaxas ◽  
Michael L. Johns ◽  
Zachary M. Aman ◽  
Eric F. May
2015 ◽  
Vol 204 ◽  
pp. 236-242 ◽  
Author(s):  
Marziyeh Zare ◽  
Ali Haghtalab ◽  
Amir Naser Ahmadi ◽  
Khodadad Nazari ◽  
Ali Mehdizadeh

2018 ◽  
Vol 56 ◽  
pp. 134-140 ◽  
Author(s):  
Zhen Long ◽  
Xuebing Zhou ◽  
Yong He ◽  
Dongliang Li ◽  
Deqing Liang

2011 ◽  
Vol 2011 ◽  
pp. 1-15 ◽  
Author(s):  
Emily V. L. Rees ◽  
Timothy J. Kneafsey ◽  
Yongkoo Seol

To study physical properties of methane gas hydrate-bearing sediments, it is necessary to synthesize laboratory samples due to the limited availability of cores from natural deposits. X-ray computed tomography (CT) and other observations have shown gas hydrate to occur in a number of morphologies over a variety of sediment types. To aid in understanding formation and growth patterns of hydrate in sediments, methane hydrate was repeatedly formed in laboratory-packed sand samples and in a natural sediment core from the Mount Elbert Stratigraphic Test Well. CT scanning was performed during hydrate formation and decomposition steps, and periodically while the hydrate samples remained under stable conditions for up to 60 days. The investigation revealed the impact of water saturation on location and morphology of hydrate in both laboratory and natural sediments during repeated hydrate formations. Significant redistribution of hydrate and water in the samples was observed over both the short and long term.


Author(s):  
Xuejian Liu ◽  
Quan Cao ◽  
Dongyan Xu ◽  
Shengjun Luo ◽  
Rongbo Guo

2021 ◽  
Vol 35 (6) ◽  
pp. 5264-5270
Author(s):  
Yong He ◽  
Zhen Long ◽  
Jingsheng Lu ◽  
Lingli Shi ◽  
Wen Yan ◽  
...  

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