Formation temperatures of thermogenic and biogenic methane

Author:

Stolper D. A.1,Lawson M.2,Davis C. L.2,Ferreira A. A.3,Neto E. V. Santos3,Ellis G. S.4,Lewan M. D.4,Martini A. M.5,Tang Y.6,Schoell M.7,Sessions A. L.1,Eiler J. M.1

Affiliation:

1. Division of Geological and Planetary Sciences, California Institute of Technology, 1200 East California Boulevard, Pasadena, CA 91125, USA.

2. ExxonMobil Upstream Research Company, Houston, TX, USA.

3. Division of Geochemistry, Petrobras Research and Development Center (CENPES), Rio de Janeiro, RJ, Brazil.

4. U.S. Geological Survey, Denver Federal Center, Denver, CO, USA.

5. Department of Geology, Amherst College, Amherst, MA, USA.

6. Power, Environmental, and Energy Research Institute, Covina, CA, USA.

7. GasConsult International Inc, Berkeley, CA, USA.

Abstract

Making of methane deep underground Technologies such as hydraulic fracturing, or “fracking,” can now extract natural gas from underground reservoirs. Within the gas, the ratio of certain isotopes holds clues to its origins. Stolper et al. analyzed a wide range of natural gas, including samples from some of the most active fracking sites in the United States. Using a “clumped isotope” technique, the authors could estimate the high temperatures at which methane formed deep underground, as well as the lower temperatures at which ancient microbes produced methane. The approach can help to distinguish the degree of mixing of gas from both sources. Science , this issue p. 1500

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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