Publications—Fact Sheet 2007-3041

Thermal Properties of Methane Gas Hydrates

By William F. Waite

U.S. Geological Survey Fact Sheet 2007-3041

The body of the report is available in PDF Format (361 KB)

To read this report using a Mac computer, open it in Adobe Acrobat only.

Introduction

Gas hydrates are crystalline solids in which molecules of a “guest” species occupy and stabilize cages formed by water molecules. Similar to ice in appearance (fig. 1), gas hydrates are stable at high pressures and temperatures above freezing (0°C). Methane is the most common naturally occurring hydrate guest species. Methane hydrates, also called simply “gas hydrates,” are extremely concentrated stores of methane and are found in shallow permafrost and continental margin sediments worldwide. Brought to sea-level conditions, methane hydrate breaks down and releases up to 160 times its own volume in methane gas.
The methane stored in gas hydrates is of interest and concern to policy makers as a potential alternative energy resource and as a potent greenhouse gas that could be released from sediments to the atmosphere and ocean during global warming. In continental margin settings, methane release from gas hydrates also is a potential geohazard and could cause submarine landslides that endanger offshore infrastructure.
Gas hydrate stability is sensitive to temperature changes. To understand methane release from gas hydrate, the U.S. Geological Survey (USGS) conducted a laboratory investigation of pure methane hydrate thermal properties at conditions relevant to accumulations of naturally occurring methane hydrate. Prior to this work, thermal properties for gas hydrates generally were measured on analog systems such as ice and non-methane hydrates or at temperatures below freezing; these conditions limit direct comparisons to methane hydrates in marine and permafrost sediment.
Three thermal properties, defined succinctly by Briaud and Chaouch (1997), are estimated from the experiments described here:

Thermal conductivity, λ: if λ is high, heat travels easily through the material.

Thermal diffusivity, κ: if κ is high, it takes little time for the temperature to rise in the material.

Specific heat, cp: if cp is high, it takes a great deal of heat to raise the temperature of the material.

Suggested Citation

Waite, W.F, Thermal Properties of Methane Gas Hydrates: U.S. Geological Survey Fact Sheet 2007-3041, 2 p., Online Only


If you have Adobe® Acrobat® or Adobe® Acrobat® Reader® installed on your computer, you may view and print the PDF version of this report. Acrobat Reader, is a free download from Adobe Systems, Inc. Users with disabilities can view information concerning accessibility at access.Adobe.com .


For further information, contact:

William C. Schwab
Chief Scientist
United States Geological Survey
Woods Hole Science Center
384 Woods Hole Road
Quissett Campus
Woods Hole, MA 02543-1598

U.S. Department of Interior
> U.S. Geological Survey > Coastal and Marine Geology Program > Woods Hole Science Center


Accessibility FOIA Privacy Policies and Notices

Take Pride in America home page. FirstGov button U.S. Department of the Interior | U.S. Geological Survey
URL: http://pubs.usgs.gov/fs/2007/3041/
Page Contact Information: USGS Publishing Network
Page Last Modified: Tuesday, 08-Jan-2013 20:21:47 EST