Methane Hydrate Dissociation Rates at 0.1 MPa and Temperatures above 272 K
Annals of the New York Academy of Sciences
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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 | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Methane Hydrate Dissociation Rates at 0.1 MPa and Temperatures above 272 K |
| Series title | Annals of the New York Academy of Sciences |
| DOI | 10.1111/j.1749-6632.2000.tb06809.x |
| Volume | 912 |
| Issue | 1 |
| Year Published | 2000 |
| Language | English |
| Publisher | The New York Academy of Science |
| Contributing office(s) | Earthquake Science Center |
| Description | 12 p. |
| First page | 544 |
| Last page | 555 |
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