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Gas Hydrates: From Laboratory Curiosity to Potential Global Powerhouse
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Abstract
Clathrates are a nonstoichiometric class of compounds that consist of a three-dimensional host molecule lattice and voids in the lattice that can be occupied by guest molecules, particularly common gases (e.g. methane, CH4). Where the host crystal structure is water the clathrate is termed a hydrate; these are the focus of increasing research. Methane (natural gas) hydrates are now recognized to occur in huge volumes in deep marine sediments and permafrost. These naturally occurring hydrates may constitute the next major energy resource of the planet and could provide the basis for the transition from our present petroleum economy to one based on methane.
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This article has been cited by 2 ACS Journal articles (2 most recent appear below).

Structures of the I-, II- and H-Methane Clathrates and the Ice−Methane Clathrate Phase Transition from Quantum-Chemical Modeling with Force-Field Thermal Corrections
Annika Lenz and Lars OjamäeThe Journal of Physical Chemistry A2011 115 (23), 6169-6176Structures of the I-, II- and H-Methane Clathrates and the Ice−Methane Clathrate Phase Transition from Quantum-Chemical Modeling with Force-Field Thermal Corrections
Annika Lenz and Lars OjamäeThe Journal of Physical Chemistry A2011 115 (23), 6169-6176Methane hydrates with the three clathrate structures I, II, and H are studied by quantum-chemical methods. Hybrid density-functional theory B3LYP computations using periodic boundary conditions are combined with force-field methods for the thermal energy ...

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- Received: August 03, 2009
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