Journal article

Processes leading to N2O emissions in grassland soil during freezing and thawing


Authors listMüller, C; Martin, M; Stevens, RJ; Laughlin, RJ; Kammann, C; Ottow, JCG; Jäger, HJ

Publication year2002

Pages1325-1331

JournalSoil Biology and Biochemistry

Volume number34

Issue number9

ISSN0038-0717

DOI Linkhttps://doi.org/10.1016/S0038-0717(02)00076-7

PublisherElsevier


Abstract
Nitrous oxide (N2O) emissions during periods of freezing-thawing can amount to more than 70% of the total annual N2O loss from soil in temperate climates. In this study, N-15-labelled grassland soil was subjected to freezing-thawing conditions to characterise the nitrogen transformation processes operating in soils under these conditions. Nitrogen transformations during a freezing-thawing event were separated into three stages: freezing, thawing and post-thawing. Ammonium (NH4+) and nitrate (NO3-) concentrations increased during the freezing period and the N-15 excess in the NH4+ and NO3- pools increased by approximately 4 and 2.5 at.% in treatments where either the NH4+ or NO3- pool had been labelled. This suggests that reviously unavailable N (characterised by high N-15 excess values) must have been either fixed on soil colloids or immobilised by the microbial biomass shortly after fertilizer application. A tracing model was developed to quantify the N transformation rates. The thawing period was characterised by high gross mineralisation (31.2 mug N g(-1) d(-1)) and low net nitrification (0.1 mug N g(-1) d(-1)) rates. During the post-thawing period the mineralisation rate decreased and the nitrification rate increased substantially to values of 3.8 and 11.4 mug N g(-1) d(-1), respectively. The enrichment of the nitrous oxide (N2O) increased during the thawing period to peak values of 9.3, 5.6 and 17.3 at.% N-15 in the three treatments where either NO3-, NH4+ or both NH4+ and NO3- had been labelled. The is enrichment of the N2O corresponded to the enrichment of the NO3 that appeared during the freezing. This indicated that the burst of N associated with reduction of NO3 which became available during the freeze-thaw episode. (C) 2002 Elsevier Science Ltd. All rights reserved.



Citation Styles

Harvard Citation styleMüller, C., Martin, M., Stevens, R., Laughlin, R., Kammann, C., Ottow, J., et al. (2002) Processes leading to N2O emissions in grassland soil during freezing and thawing, Soil Biology and Biochemistry, 34(9), pp. 1325-1331. https://doi.org/10.1016/S0038-0717(02)00076-7

APA Citation styleMüller, C., Martin, M., Stevens, R., Laughlin, R., Kammann, C., Ottow, J., & Jäger, H. (2002). Processes leading to N2O emissions in grassland soil during freezing and thawing. Soil Biology and Biochemistry. 34(9), 1325-1331. https://doi.org/10.1016/S0038-0717(02)00076-7


Last updated on 2025-21-05 at 15:17