Articles | Volume 15, issue 22
Atmos. Chem. Phys., 15, 13003–13021, 2015
https://doi.org/10.5194/acp-15-13003-2015
Atmos. Chem. Phys., 15, 13003–13021, 2015
https://doi.org/10.5194/acp-15-13003-2015

Research article 24 Nov 2015

Research article | 24 Nov 2015

Isotopic signatures of production and uptake of H2 by soil

Q. Chen et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Qianjie Chen on behalf of the Authors (28 Oct 2015)  Author's response    Manuscript
ED: Reconsider after minor revisions (Editor review) (11 Nov 2015) by Jan Kaiser
AR by Qianjie Chen on behalf of the Authors (11 Nov 2015)  Author's response    Manuscript
ED: Publish subject to technical corrections (12 Nov 2015) by Jan Kaiser
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Short summary
We investigated soil production and uptake of H2 and associated isotope effects. Uptake and emission of H2 occurred simultaneously at all sampling sites, with strongest emission where N2 fixing legume was present. The fractionation constant during soil uptake was about 0.945 and it did not show positive correlation with deposition velocity. The isotopic composition of H2 emitted from soil with legume was about -530‰, which is less deuterium-depleted than isotope equilibrium between H2O and H2.
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