Methane hydrate dissociation rates as 0.1 MPa and temperatures above 272K
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 m...
Main Authors: | , , , , |
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Other Authors: | |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Lawrence Livermore National Laboratory
1999
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Subjects: | |
Online Access: | http://digital.library.unt.edu/ark:/67531/metadc623609/ |
Summary: | 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. |
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