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N2O, NO N2 and CO2 emissions from tropical savanna and grassland of northern Australia: an incubation experiment with intact soil cores

Werner, C., Reiser, K., Dannenmann, M., Hutley, L.B., Jacobeit, J. and Butterbach-Bahl, K. (2014). N2O, NO N2 and CO2 emissions from tropical savanna and grassland of northern Australia: an incubation experiment with intact soil cores. Biogeosciences,11(21):6047-6065.

Document type: Journal Article
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IRMA ID 84376995xPUB97
Title N2O, NO N2 and CO2 emissions from tropical savanna and grassland of northern Australia: an incubation experiment with intact soil cores
Author Werner, C.
Reiser, K.
Dannenmann, M.
Hutley, L.B.
Jacobeit, J.
Butterbach-Bahl, K.
Journal Name Biogeosciences
Publication Date 2014
Volume Number 11
Issue Number 21
ISSN 1726-4170   (check CDU catalogue open catalogue search in new window)
Scopus ID 2-s2.0-84908610737
Start Page 6047
End Page 6065
Total Pages 19
Place of Publication Germany
Publisher Copernicus GmbH
HERDC Category C1 - Journal Article (DIISR)
Abstract Strong seasonal variability of hygric and thermal soil conditions are a defining environmental feature in northern Australia. However, how such changes affect the soil–atmosphere exchange of nitrous oxide (N2O), nitric oxide (NO) and dinitrogen (N2) is still not well explored. By incubating intact soil cores from four sites (three savanna, one pasture) under controlled soil temperatures (ST) and soil moisture (SM) we investigated the release of the trace gas fluxes of N2O, NO and carbon dioxide (CO2). Furthermore, the release of N2 due to denitrification was measured using the helium gas flow soil core technique. Under dry pre-incubation conditions NO and N2O emissions were very low (<7.0 ± 5.0 μg NO-N m−2 h−1; <0.0 ± 1.4 μg N2O-N m−2 h−1) or in the case of N2O, even a net soil uptake was observed. Substantial NO (max: 306.5 μg N m−2 h−1) and relatively small N2O pulse emissions (max: 5.8 ± 5.0 μg N m−2 h−1) were recorded following soil wetting, but these pulses were short lived, lasting only up to 3 days. The total atmospheric loss of nitrogen was generally dominated by N2 emissions (82.4–99.3% of total N lost), although NO emissions contributed almost 43.2% to the total atmospheric nitrogen loss at 50% SM and 30 °C ST incubation settings (the contribution of N2 at these soil conditions was only 53.2%). N2O emissions were systematically higher for 3 of 12 sample locations, which indicates substantial spatial variability at site level, but on average soils acted as weak N2O sources or even sinks. By using a conservative upscale approach we estimate total annual emissions from savanna soils to average 0.12 kg N ha−1 yr−1 (N2O), 0.68 kg N ha−1 yr−1 (NO) and 6.65 kg N ha−1 yr−1 (N2). The analysis of long-term SM and ST records makes it clear that extreme soil saturation that can lead to high N2O and N2 emissions only occurs a few days per year and thus has little impact on the annual total. The potential contribution of nitrogen released due to pulse events compared to the total annual emissions was found to be of importance for NO emissions (contribution to total: 5–22%), but not for N2O emissions. Our results indicate that the total gaseous release of nitrogen from these soils is low and clearly dominated by loss in the form of inert nitrogen. Effects of seasonally varying soil temperature and moisture were detected, but were found to be low due to the small amounts of available nitrogen in the soils (total nitrogen <0.1%).

DOI http://dx.doi.org/10.5194/bg-11-6047-2014   (check subscription with CDU E-Gateway service for CDU Staff and Students  check subscription with CDU E-Gateway in new window)
Additional Notes This is an Open Access article distributed under the terms of the Creative Commons Attribution License 3.0, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


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