DOI | Resolve DOI: https://doi.org/10.1021/jp9839854 |
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Author | Search for: Moudrakovski, Igor L.1; Search for: Ratcliffe, Christopher I.1; Search for: McLaurin, Graham E.1; Search for: Simard, Benoit1; Search for: Ripmeester, John A.1 |
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Affiliation | - National Research Council of Canada. NRC Steacie Institute for Molecular Sciences
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Format | Text, Article |
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Subject | superheated ice; microimaging; hydrate layers |
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Abstract | Recent observations on the interaction of methane gas with ice surfaces have led to the suggestion that the resulting hydrate layer prevents the encapsulated ice from melting at its usual temperature. This would require ice to exist in a “superheated” state.1 We have examined the product of the gas−solid reaction with 1H NMR imaging. The imaging experiments show that the hydrate-encapsulated ice is able to melt at its usual melting point. As a possible alternative model, we suggest that a considerable amount of ice inside the hydrate layer can be converted to hydrate and liquid water under isothermal and constant volume conditions, the hydrate layer acting as an insulating, semipermeable layer that insulates processes inside the hydrate layer from external bulk temperature and pressure measurements. |
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Publication date | 1999-07-01 |
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In | |
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Language | English |
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Peer reviewed | Yes |
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NRC number | NRCC 42178 |
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NPARC number | 21275384 |
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Export citation | Export as RIS |
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Report a correction | Report a correction (opens in a new tab) |
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Record identifier | 2b0c5c6d-e0e0-4e41-86f2-54a6c0aef81f |
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Record created | 2015-06-24 |
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Record modified | 2020-03-20 |
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