Observation of Interstitial Molecular Hydrogen in Clathrate Hydrates

The current knowledge and description of guest molecules within clathrate hydrates only accounts for occupancy within regular polyhedral water cages. Experimental measurements and simulations, examining the tert‐butylamine+H2+H2O hydrate system, now suggest that H2 can also be incorporated within hy...

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Published in:Angewandte Chemie International Edition Vol. 53; no. 40; pp. 10710 - 10713
Main Authors: Grim, R. Gary, Barnes, Brian C., Lafond, Patrick G., Kockelmann, Winfred A., Keen, David A., Soper, Alan K., Hiratsuka, Masaki, Yasuoka, Kenji, Koh, Carolyn A., Sum, Amadeu K.
Format: Journal Article
Language:English
Published: Weinheim WILEY-VCH Verlag 26-09-2014
WILEY‐VCH Verlag
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Edition:International ed. in English
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Summary:The current knowledge and description of guest molecules within clathrate hydrates only accounts for occupancy within regular polyhedral water cages. Experimental measurements and simulations, examining the tert‐butylamine+H2+H2O hydrate system, now suggest that H2 can also be incorporated within hydrate crystal structures by occupying interstitial sites, that is, locations other than the interior of regular polyhedral water cages. Specifically, H2 is found within the shared heptagonal faces of the large (43596273) cage and in cavities formed from the disruption of smaller (4454) water cages. The ability of H2 to occupy these interstitial sites and fluctuate position in the crystal lattice demonstrates the dynamic behavior of H2 in solids and reveals new insight into guest–guest and guest–host interactions in clathrate hydrates, with potential implications in increasing overall energy storage properties. Breaking the boundaries: In the presence of molecular hydrogen, interstitial occupancy is observed in the type VI clathrate hydrate (see picture; tBuNH2 in interstices (red) with H2 (green)). This observation revises the definition of clathrate hydrate guest occupancy that assumes all guests are contained within the interior of the host water lattice.
Bibliography:We acknowledge the financial support of this work by the U.S. Department of Energy, Office of Basic Energy Sciences, Division of Materials Sciences and Engineering (DOE-BES award DE-FG02-05ER46242). We also acknowledge Dr. Tim Strobel (Carnegie Institute of Washington) and Dr. John Ripmeester (formerly at National Research Council of Canada) for helpful discussions. Thanks also to the ISIS Facility, Rutherford Appleton Laboratory for neutron beam time, and to Chris Goodway and his team for technical and engineering assistance for the measurements.
U.S. Department of Energy, Office of Basic Energy Sciences, Division of Materials Sciences and Engineering - No. DE-FG02-05ER46242
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ArticleID:ANIE201406546
We acknowledge the financial support of this work by the U.S. Department of Energy, Office of Basic Energy Sciences, Division of Materials Sciences and Engineering (DOE‐BES award DE‐FG02‐05ER46242). We also acknowledge Dr. Tim Strobel (Carnegie Institute of Washington) and Dr. John Ripmeester (formerly at National Research Council of Canada) for helpful discussions. Thanks also to the ISIS Facility, Rutherford Appleton Laboratory for neutron beam time, and to Chris Goodway and his team for technical and engineering assistance for the measurements.
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ISSN:1433-7851
1521-3773
DOI:10.1002/anie.201406546