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Biogeosciences An interactive open-access journal of the European Geosciences Union
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Volume 14, issue 3
Volume 14, issue 3
Biogeosciences, 14, 711–732, 2017
https://doi.org/10.5194/bg-14-711-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 14, 711–732, 2017
https://doi.org/10.5194/bg-14-711-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Volume 14, issue 3

Research article 14 Feb 2017

Research article | 14 Feb 2017

Quantifying N2O reduction to N2 based on N2O isotopocules – validation with independent methods (helium incubation and 15N gas flux method)

Dominika Lewicka-Szczebak et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (Editor review) (05 Dec 2016) by Yakov Kuzyakov
AR by Dominika Lewicka-Szczebak on behalf of the Authors (19 Jan 2017)  Author's response    Manuscript
ED: Publish as is (19 Jan 2017) by Yakov Kuzyakov
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Short summary
The consumption of the greenhouse gas nitrous oxide (N2O) by its reduction to dinitrogen via microbial denitrification in soil is poorly quantified. This precludes improvements in nitrogen (N) efficiency in agricultural ecosystems and mitigation of N losses to the environment including N2O fluxes. We present a laboratory evaluation for the determination of N2O reduction based on stable isotope values of soil-emitted N2O as a new approach to determine N2O reduction in the field studies.
The consumption of the greenhouse gas nitrous oxide (N2O) by its reduction to dinitrogen via...
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Biogeosciences

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