AmmoniaDeposition of atmospheric ammonia to moorlands
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Cited by (83)
Nitrogen fertilisers with urease inhibitors reduce nitrous oxide and ammonia losses, while retaining yield in temperate grassland
2020, Science of the Total EnvironmentCitation Excerpt :Gaseous losses of reactive N following fertilisation are predominantly of nitrous oxide (N2O) and ammonia (NH3). Nitrous oxide is a potent greenhouse gas (GHG) and ozone-destroying substance (Ravishankara et al., 2009), while NH3 is an air pollutant contributing to eutrophication and acidification of terrestrial and aquatic ecosystems, and an indirect source of N2O (Sutton et al., 1992). Global N2O and NH3 emissions from fertiliser N are estimated to be approximately 4 and 10–12 Tg N yr−1, respectively (Beusen et al., 2008; Reay et al., 2012).
Coupling atmospheric ammonia exchange process over a rice paddy field with a multi-layer atmosphere-soil-vegetation model
2013, Agricultural and Forest MeteorologyCitation Excerpt :Based on field observations, Jitto et al. (2007) reported that mean values of Vd for SO2 was 1.5–2.5 cm s−1 during the daytime over a paddy field in the tropical region in summer, similar to the results obtained in the present study (Fig. 10b). For NH3, Vd values ranging from 0.65 to 6.0 cm s−1 over various surfaces were obtained from the literature (Andersen et al., 1999; Asman et al., 1998; Duyzer et al., 1992; Shahin et al., 1999; Sutton et al., 1992; Valigura, 1995; Wyers et al., 1992). The calculated Vd during both fallow and cropping periods in this study (Fig. 10a and c) were within this range.
Atmospheric deposition of nitrogen, sulfur and chloride in Thessaloniki, Greece
2007, Atmospheric ResearchConcentration-dependent NH<inf>3</inf> deposition processes for mixed moorland semi-natural vegetation
2007, Atmospheric Environment