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. 2018 Nov 16;9:2794. doi: 10.3389/fmicb.2018.02794

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Copyright © 2018 Arce, von Schiller, Bengtsson, Hinze, Jung, Alves, Urich and Singer.

This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.

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(A) Fluxes of N₂O from sediments before microcosms drainage (microcosms with a surface water column; t = –3 days), immediately after drainage (t = 0 days) and several times after drainage and drying. (B) Accumulated fluxes of N₂O following 24 h under the effects of variable RMs (0, 4, and 21 mm) after the different DPDs. (C) and (D) Fluxes of N₂O before (t = –2 h), immediately (t = 0 h) and following rainfall events (t = 2, 6, and 24 h) after 6 and 9 weeks of drying, respectively. Values are means ± SE (n = 3).