Abstract
Efficiency of gas production from naturally occurring methane clathrate hydrate is governed by processes of fluid and heat transports as well as kinetics of the hydrate dissociation. Past numerical and laboratory studies on gas hydrate dissociation have revealed critical parameters to the dissociation processes. Field studies have been done for data acquisition and verification of production techniques. According to the results of those studies, natural gas hydrate deposit can be dissociated continuously by simple depressurization under a certain condition.
| Original language | English |
|---|---|
| Title of host publication | Poromechanics IV - 4th Biot Conference on Poromechanics |
| Publisher | DEStech Publications |
| Pages | 947-952 |
| Number of pages | 6 |
| ISBN (Print) | 9781605950068 |
| Publication status | Published - 2009 |
| Externally published | Yes |
| Event | 4th Biot Conference on Poromechanics - New York, United States Duration: 2009 Jun 8 → 2009 Jun 10 |
Other
| Other | 4th Biot Conference on Poromechanics |
|---|---|
| Country | United States |
| City | New York |
| Period | 09/6/8 → 09/6/10 |
ASJC Scopus subject areas
- Acoustics and Ultrasonics
- Condensed Matter Physics
- Mechanics of Materials
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Cite this
Yamamoto, K., & Kurihara, M. (2009). Gas hydrate production from geological formations as transport phenomena. In Poromechanics IV - 4th Biot Conference on Poromechanics (pp. 947-952). DEStech Publications.