2000
DOI: 10.1002/1522-2624(200006)163:3<249::aid-jpln249>3.0.co;2-z
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Nitrous oxide emissions from arable soils in Germany — An evaluation of six long-term field experiments

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Cited by 116 publications
(76 citation statements)
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“…This confirms that the fertilizer sources affect N 2 O flux. Kaiser and Ruser (2000) reported that organically fertilized soil is characterised by higher N 2 O emissions compared to mineral fertilizer-treated plots. It is due to higher microbiological activities and the accessibility of C suitable for mineralization.…”
Section: Resultsmentioning
confidence: 99%
“…This confirms that the fertilizer sources affect N 2 O flux. Kaiser and Ruser (2000) reported that organically fertilized soil is characterised by higher N 2 O emissions compared to mineral fertilizer-treated plots. It is due to higher microbiological activities and the accessibility of C suitable for mineralization.…”
Section: Resultsmentioning
confidence: 99%
“…However, the implementation of anaerobic digestion plants also enables a use of the residues otherwise incorporated directly into the soil (crop residues, green manure crops like cover crops or clover-grass-leys) leading to a substantial decrease of soilborne N 2 O emissions as indicated by few studies presented in Effects of anaerobic digestion on soil C, N, and biological activity Stinner 2009;Nadeem et al 2012). The harvest and anaerobic digestion of clover/grass leys, crop residues, and cover crops in autumn results in the removal of large amounts of N and its storage in "closed" stores during winter Gunnarsson et al 2011;Nadeem et al 2012), a period with substantial N 2 O losses which might account for 50 % or even more of the annual N 2 O flux (Flessa et al 1995;Kaiser and Ruser 2000). Whole-year inventories indicated that most soil N 2 O fluxes occurred within 20-40 days after fertilization Möller and Stinner 2009;Chantigny et al 2010).…”
Section: Cropping System Change-based Impacts On Field N 2 O Emissionsmentioning
confidence: 96%
“…Surprisingly the BMED values for N 2 O for tropical climates are similar to those in temperate and lower than in subtropical climates. Although not significantly different, the BMED for continental temperate climates is higher than for oceanic temperate climates, reflecting the higher winter emissions due to temporary accumulation of soil N due to freezethaw cycles (Kaiser and Ruser 2000). The length of the experiment is the only measurement-related factor with a significant influence on N 2 O emissions ( Table 1).…”
Section: Agricultural Fieldsmentioning
confidence: 99%