Articles | Volume 13, issue 7
https://doi.org/10.5194/bg-13-2111-2016
https://doi.org/10.5194/bg-13-2111-2016
Research article
 | 
11 Apr 2016
Research article |  | 11 Apr 2016

An inversion approach for determining distribution of production and temperature sensitivity of soil respiration

Robyn N. C. Latimer and David A. Risk

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Cited articles

Cerling, T. E.: The stable isotopic composition of modern soil carbonate and its relationship to climate, Earth Planet. Sc. Lett., 71, 229–240, 1984.
Davidson, E. A., Belk, E., and Boone, R. D.: Soil water content and temperature as independent or confound factors controlling soil respiration in a temperate mixed hardwood forest, Glob. Change Biol., 4, 217–227, 1998.
Davidson, E. A., Janssens, I. A., and Luo, Y.: On the variability of respiration in terrestrial ecosystems: Moving beyond Q10, Glob. Change Biol., 12, 154–164, https://doi.org/10.1111/j.1365-2486.2005.01065.x, 2006.
Graf, A., Weihermüller, L., Huisman, J. A., Herbst, M., Bauer, J., and Vereecken, H.: Measurement depth effects on the apparent temperature sensitivity of soil respiration in field studies, Biogeosciences, 5, 1175–1188, https://doi.org/10.5194/bg-5-1175-2008, 2008.
Hanson, P. J., Edwards, N. T., Garten, C. T., and Andrews, J. A.: Separating root and soil microbial contributions to soil respiration: A review of methods and observations, Biogeochemistry, 48, 115–146, 2000.
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Short summary
This study examines an inversion approach for estimating Q10 and depth of production using a physically based soil model, constrained by observed high-frequency surface fluxes and/or five concentrations. Inversions using exclusively surface flux measurements were successful, but using multiple shallow subsurface CO2 measurements yielded the best results. This work is a first step toward building a reliable computing framework for removing physical artefacts from high-frequency soil CO2 data.
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