Biology of the Nitrogen Cycle 2007
DOI: 10.1016/b978-044452857-5.50024-2
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Denitrification in Wetlands

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Cited by 12 publications
(15 citation statements)
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References 25 publications
(22 reference statements)
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“…Furthermore, the algorithms only attempt to represent in-river uptake of N by algal growth and take no account of macrophytes (which are an important feature of the river Axe) in the river channel which might reduce river nitrogen concentrations during the spring and summer. Finally, data limitations meant that it was not possible to locate and simulate wetlands within SWAT which might be important local sinks of nitrogen [60][61][62]. Furthermore, in the process of building a model several adjustments of the parameters need to be made in order to improve simulations.…”
Section: Discussionmentioning
confidence: 99%
“…Furthermore, the algorithms only attempt to represent in-river uptake of N by algal growth and take no account of macrophytes (which are an important feature of the river Axe) in the river channel which might reduce river nitrogen concentrations during the spring and summer. Finally, data limitations meant that it was not possible to locate and simulate wetlands within SWAT which might be important local sinks of nitrogen [60][61][62]. Furthermore, in the process of building a model several adjustments of the parameters need to be made in order to improve simulations.…”
Section: Discussionmentioning
confidence: 99%
“…In natural wetlands the direct loss of ammonia gas is negligible (Hemond 1983), and denitrification rates in global natural temperate wetlands on average is 4 kg N ha -1 year -1 (Van Cleemput et al 2007). However, in cultivated wetlands, such as rice paddies, N emissions can be much higher.…”
Section: Evidence Of Denitrification In Cultivated Cranberry Bedsmentioning
confidence: 99%
“…This flux is illustrated by high volume of water percolation losses (Table 6). As a result, the N-NO3 -formed in oxidizing zones are spread into soil profile (Aulakh and Bijay-Singh, 1996; and it triggers denitrification processes due to nitrate movement into anaerobic sites (Van Cleemput et al, 2007;. CF, SS, AWDL, AWDS might have low 15 N recovery compared to NF explained by it.…”
Section: The Isotopic Efficiencymentioning
confidence: 99%
“…Under continuous flooding the soil remains in a reduced anaerobic state and ammonium nitrification is restricted to a few oxidation sites, thus becoming negligible (Reddy et al, 1984;Van Cleemput et al, 2007). However, varying water regimes or high percolation rates can trigger nitrification and expose N to loss pathways such denitrification and leaching (Aulakh and Bijay-Singh, 1996;.…”
Section: Introductionmentioning
confidence: 99%
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