Non-Co2 Greenhouse Gases: Why and How to Control? 1994
DOI: 10.1007/978-94-011-0982-6_14
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Nitrous Oxide Emission out of Grassland

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Cited by 12 publications
(5 citation statements)
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“…Thus, at certain pH and Eh values, high NO -3 activity enhances its transformation to N2O. Although these results contradict with those obtained by Kroese et al (1989) who found that N2O production is independent on the initial NO -3 content, they appear to fit the observations of many authors (Eichner, 1990;1991;Kralova et al, 1992;Van Cleemput, 1994;Van Cleemput et al, 1994;DeGroot et al, 1994 andVermoesen et al, 1996). Hence, the stability diagrams of nitrate developed in this study support the hypothesis that agricultural soils are responsible for most of N2O in air which attacks the ozone layer as concluded by Mosier and Schinel (1991).…”
Section: Resultsmentioning
confidence: 51%
“…Thus, at certain pH and Eh values, high NO -3 activity enhances its transformation to N2O. Although these results contradict with those obtained by Kroese et al (1989) who found that N2O production is independent on the initial NO -3 content, they appear to fit the observations of many authors (Eichner, 1990;1991;Kralova et al, 1992;Van Cleemput, 1994;Van Cleemput et al, 1994;DeGroot et al, 1994 andVermoesen et al, 1996). Hence, the stability diagrams of nitrate developed in this study support the hypothesis that agricultural soils are responsible for most of N2O in air which attacks the ozone layer as concluded by Mosier and Schinel (1991).…”
Section: Resultsmentioning
confidence: 51%
“…Adding a nitrification inhibitor reduced N 2 O emission from urea, but an urease inhibitor did not reduce N 2 O emissions relative to CAN.A study byHarty et al (2016) in Ireland evaluated the impact of switching fertilizer formulation from CAN to urea based products on grassland (urea, urea + urease inhibitor N-(n-butyl) thiophosphoric triamide (NBPT), and urea + nitrification inhibitor dicyandiamide; DCD). The results showed thatN 2 O emissions were highest for CAN, also when the indirect N 2 O emission from ammonia was 6 References: Abbasi and Adams (2000); Ambus et al (2001); Anger et al (2003); Arah et al (1991); Ball et al (2000); Burford et al (1981); Chadwick et al (2000); Christensen (1983), Clayton et al (1994); Clayton et al (1997); Clemens et al (1997);Colbourn and Harper (1987);Colbourn et al (1984);Conrad et al (1983);Dobbie and Smith (2003a);Dobbie et al (1999);Eggington and Smith (1986);Ellis et al (1998);Glatzel and Stahr (2001);Goossens et al (2001);Hénault et al (1998a);Jambert et al (1997);Jørgensen et al (1997);Kaiser et al (1996);Kaiser et al (1998b);Kamp et al (1998);;Misselbrook et al (1998);Mogge et al (1999);Petersen (1999);Rodhe et al (2006);Ryden (1981);Seiler and Conrad (1981);Skiba et al (1992);Skiba et al (1998);Slemr et al (1984);Smith et al (1998a, b);Van Cleemput et al (1994);Webster and Dowdell (1982);Weslien et al (1998);Wulf et al (2002); Yamulki and Jarvis…”
mentioning
confidence: 99%
“…Here, we consider issues relating to the statistical analysis of spatially heterogenous cumulative N 2 O flux estimates. This spatial variability has been considered log‐normal at different scales, from plot to paddock to farm to landscape (Oenema, Velthof, Yamulki, & Jarvis, 1997; van Cleemput, Vermoesen, de Groot, & van Ryckeghem, 1994), although normal distributions have also been reported (Petersen, 1999).…”
Section: Statistical Considerations For Heterogeneous Datamentioning
confidence: 99%