期刊
ENERGIES
卷 5, 期 2, 页码 518-530出版社
MDPI
DOI: 10.3390/en5020518
关键词
methane hydrate; depressurization; saturation; dissociation pressure; porous sediments
资金
- National Natural Science Foundation of China [51076155]
- Science & Technology Program of Guangdong Province [2009B050600006]
Based on currently available data from site measurements in the Shenhu Area of the South China Sea, methane hydrate dissociation behavior by depressurization is studied in a one-dimensional experimental apparatus. According to time variation of temperature, resistance and gas production, the hydrate dissociation process is divided into three stages: free gas release, rapid dissociation and gradual dissociation. The experimental results show that as the hydrate saturation increases the proportion of hydrate decomposed decreases in the rapid dissociation stage. The hydrate dissociation rate and the dissociation heat increase as the dissociation pressure decreases. Furthermore, the decrease of the dissociation pressure works against the secondary formation of the hydrate.
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