Volume 43, Issue 25 pp. 3310-3313
Communication

The Coexistence of Two Different Methane Hydrate Phases under Moderate Pressure and Temperature Conditions: Kinetic versus Thermodynamic Products

Judith M. Schicks Dr.

Judith M. Schicks Dr.

GeoForschungsZentrum Potsdam Telegrafenberg, 14473 Potsdam, Germany, Fax: (+49) 331-288-1436

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John A. Ripmeester Dr.

John A. Ripmeester Dr.

Ripmeester Steacie Institute for Molecular Science National Research Council Ottawa Canada

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First published: 16 June 2004
Citations: 140

The Geotechnologien program of BMBF and DFG provided funding of this work through the Research Grant G0555A. This is publication no. GEOTECH-61 of the Geotechnologien program.

Graphical Abstract

The unexpected coexistence of structure I (s I) and structure II (s II) methane hydrates under conditions where only s I hydrates should be stable (see picture) suggests that the initial product is determined by kinetics. The state of coexistence as well as the transformation of the kinetic product into the thermodynamically stable s I hydrate was documented by microscopic visual observation as well as Raman spectroscopy.

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