Denitrification across landscapes and waterscapes: a synthesis.

By S. Seitzinger, J. Harrison, J. Böhlke, A. Bouwman, R. Lowrance, B. Peterson, C. Tobias, G. Drecht. Ecological Applications, 2006

1,634 citations recorded by the source corpus.

Subfields: Environmental Chemistry, Geochemistry and Petrology, Pollution

View Paper: https://www.semanticscholar.org/paper/2e0794a107fe729370484701d28829eae2ca9494

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Citations in the corpus

Stoichiometry constrains microbial response to root exudation- insights from a model and a field experiment in a temperate forest (2012, background): “, 2003), denitrification (Potter et al., 1996; Seitzinger et al., 2006), NH3 volatilization (Schlesinger and Peterjohn, 1991; Bouwman et al.”
Beyond carbon and nitrogen: how the microbial energy economy couples elemental cycles in diverse ecosystems (2011, background): “For example, anaerobic respiration based on NO3 − reduction to dinitrogen (N2; denitrification) is the most important sink (removal process) for reactive N, helping to remove excess NO3 − resulting from human activities (Seitzinger et al. 2006).”
The nitrogen legacy: emerging evidence of nitrogen accumulation in anthropogenic landscapes (2016, background): “The existence of such a balance, however, is based on an assumption of steady-state dynamics for terrestrial N reservoirs, with all anthropogenically and naturally fixed NR being denitrified and returned to the atmosphere on an annual timescale [22].”
Mycorrhizal effects on nutrient cycling, nutrient leaching and N2O production in experimental grassland (2015, neutral): “…of N losses via denitri ﬁ cation, when nitrate is transformed to N 2 O and N 2 , are very variable and can range from 0 to more than 300 kg N ha (cid:1) 1 yr (cid:1) 1 lost from agricultural soils (Jambert et al., 1997; Hofstra and Bouwman, 2005; Seitzinger et al., 2006; van der Salm et al., 2007).”
Mainstreaming ecosystem services into EU policy (2013, methodology): “used a model that accounts for differences between rivers, lakes, and wetlands in their capacity to retain nitrogen based on their hydrological and geomorphological properties [30].”
Global Nutrient Export from WaterSheds 2 (NEWS 2): Model development and implementation (2010, background): “The unified formulation for dissolved forms includes explicit sources to the watershed (imports of external origin, recycling, and mobilization or transformation to reactive forms within the watershed); explicit and parameterized land-based sinks from the watershed; inputs to streams from both…”
Nitrous oxide emission from denitrification in stream and river networks (2010, background): “, indirect denitrification following organic N mineralization and nitrification), which can be the dominant source of NO3 − supporting denitrification when stream water NO3 − concentration is low (<140 μg N·L) (25).”
An Earth-system perspective of the global nitrogen cycle (2008, background): “Nearly half of global terrestrial denitrification occurs in freshwater system”