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Volume 14, issue 3
Biogeosciences, 14, 703–710, 2017
https://doi.org/10.5194/bg-14-703-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 14, 703–710, 2017
https://doi.org/10.5194/bg-14-703-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Feb 2017

Research article | 10 Feb 2017

Interactions among temperature, moisture, and oxygen concentrations in controlling decomposition rates in a boreal forest soil

Carlos A. Sierra et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (24 Jan 2017) by Jens-Arne Subke
AR by Carlos Sierra on behalf of the Authors (24 Jan 2017)  Author's response    Manuscript
ED: Publish as is (27 Jan 2017) by Jens-Arne Subke
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Short summary
Temperature, moisture, and oxygen are interacting variables that control the rates of soil organic matter decomposition. With a well-replicated experiment, the authors show that decomposition rates in a boreal forest soil are not limited at high temperatures in the presence of enough water and oxygen. Similarly, at high humidity, oxygen is the main limiting factor for decomposition. The authors conclude that interactions among the three variables are the main determinants of decomposition rates.
Temperature, moisture, and oxygen are interacting variables that control the rates of soil...
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