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δ13C patterns of CO2 and CH4 in peatlands: The role of diffusion/advection vs. microbial reactions

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Non-CO2 Greenhouse Gases: Scientific Understanding, Control and Implementation

Abstract

Atmospheric methane acts as a strong greenhouse gas and possibly played a key role in past and present climate changes. This study aims at a better understanding of the mechanisms of methane production in wetlands, which represent an important source of atmospheric methane.

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References

  • Steinmann P. and Shotyk W. (1997) Chemical composition, pH, and redox state of S and Fe in complete vertical pore water profiles from two Sphagnum peat bogs, Jura Mountains, Switzerland. Geochim. Cosmochim. Acta 61, 1143–1163.

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© 2000 Springer Science+Business Media Dordrecht

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Steinmann, P., Eilrich, B., Burns, S.J. (2000). δ13C patterns of CO2 and CH4 in peatlands: The role of diffusion/advection vs. microbial reactions. In: van Ham, J., Baede, A.P.M., Meyer, L.A., Ybema, R. (eds) Non-CO2 Greenhouse Gases: Scientific Understanding, Control and Implementation. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-9343-4_19

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  • DOI: https://doi.org/10.1007/978-94-015-9343-4_19

  • Publisher Name: Springer, Dordrecht

  • Print ISBN: 978-90-481-5409-8

  • Online ISBN: 978-94-015-9343-4

  • eBook Packages: Springer Book Archive

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