Methane hydrate dissociation rates at 0.1 MPa and temperatures above 272 K
By: S. Circone, L.A. Stern, S. H. Kirby, J.C. Pinkston, and W. B. Durham
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Abstract
We performed rapid depressurization experiments on methane hydrate under isothermal conditions above 272 K to determine the amount and rate of methane evolution. Sample temperatures rapidly drop below 273 K and stabilize near 272.5 K during dissociation. This thermal anomaly and the persistence of methane hydrate are consistent with the reported recovery of partially dissociated methane hydrate from ocean drilling cores.
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | Methane hydrate dissociation rates at 0.1 MPa and temperatures above 272 K |
| Volume | 912 |
| Year Published | 2000 |
| Language | English |
| Larger Work Title | Annals of the New York Academy of Sciences |
| First page | 544 |
| Last page | 555 |
| Google Analytic Metrics | Metrics page |