1996
DOI: 10.1007/bf00011298
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Laboratory measurements and simulations of ammonia volatilization from urea applied to calcareous Chinese loess soils

Abstract: Ammonia volatilization is the major pathway for mineral nitrogen loss in the calcareous soils of the Chinese loess plateau, with maximum losses reaching 50% of the fertilizer-N applied. A volatilization-diffusion experiment was carried out in the laboratory using a forced-draft system and soil columns of 15.5 cm depth. Urea was surface applied at rates of 210 kg N ha-I to a soil with 10% CaCO3 and a pH of 7.7. The amount of ammonia volatilized as well as the concentration profiles of ammoniacal-nitrogen and so… Show more

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Cited by 25 publications
(12 citation statements)
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“…Bouwman et al (2002) summarized NH 3 volatilization data following the application of N sources to agricultural soils and estimated that NH 3 losses from incorporated N were on average 50% lower than those from surface application. However, studies under field conditions typical of dryland agriculture yielded highly variable results with NH 3 volatilization 1.6 to 1.9 (Palma et al, 1998), 1 to 9 (Roelcke et al, 1996), and 7 (Prasertsak et al, 2002) times lower for incorporated than for surface‐applied urea.…”
mentioning
confidence: 99%
“…Bouwman et al (2002) summarized NH 3 volatilization data following the application of N sources to agricultural soils and estimated that NH 3 losses from incorporated N were on average 50% lower than those from surface application. However, studies under field conditions typical of dryland agriculture yielded highly variable results with NH 3 volatilization 1.6 to 1.9 (Palma et al, 1998), 1 to 9 (Roelcke et al, 1996), and 7 (Prasertsak et al, 2002) times lower for incorporated than for surface‐applied urea.…”
mentioning
confidence: 99%
“…Likewise, the effect of NH $ _4^+ $ adsorption on NH 3 losses was less important compared to initial soil pH and soil pH buffer capacity in the sensitivity analysis of the DUPAV model by Singh and Nye (1986c). As described by Singh and Nye (1986a, 1986b) and Roelcke et al (1996), the soil pH rises in the first few days following urea application due to hydrolysis and thereafter decreases again due to protons (H + ) remaining at the immediate soil surface during the volatilization of NH 3 . This rise and decline in pH was also described by the HERMES model, though there were differences in magnitude in the study of Roelcke et al (1996), in which surface CaCO 3 content was high (10%), which buffered pH change.…”
Section: Discussionmentioning
confidence: 86%
“…As described by Singh and Nye (1986a, 1986b) and Roelcke et al (1996), the soil pH rises in the first few days following urea application due to hydrolysis and thereafter decreases again due to protons (H + ) remaining at the immediate soil surface during the volatilization of NH 3 . This rise and decline in pH was also described by the HERMES model, though there were differences in magnitude in the study of Roelcke et al (1996), in which surface CaCO 3 content was high (10%), which buffered pH change. This suggests that this magnitude may have been overestimated since soil pH buffer capacity, clay and CaCO 3 content, and CO 2 loss was not taken into account.…”
Section: Discussionmentioning
confidence: 86%
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“…Effective use of urea and ammonium sulfate on crop requiring surface fertilizer application is limited by high ammonia NH 3 loss. Approximately 10-40% of N as urea and ammonium sulfate applied to soils is volatilized during the growing season, especially N from alkaline and calcareous soils (Gezgin and Bayrakll, 1995;Roelcke et al, 1996). Many studies have evaluated the effect of N source on wheat production.…”
Section: Introductionmentioning
confidence: 99%