Ammonia (NH3) fluxes were estimated by three inverse modelling methods over a sorghum field following the application of 240 kg N ha(-1) of urea pills under a semi-arid Mediterranean climate. Ammonia volatilisation started following irrigation, which coincided with the third urea application. The maximum volatilisation rate was reached 7 days after irrigation. A clear dependence of the NH3 volatilisation on irrigation and rainfall events was observed. The NH3 fluxes ranged from 2.5 to 45 mu g NH3 m(-2) s(-1). The canopy compensation point jumped from 9 mu g NH3 m(-3) before urea hydrolysis to 131 mu g NH3 m-3 afterwards, while the soil compensation point varied in the meantime from 24 to 800 mu g NH3 m-3 on average. The soil-dominated observed NH3 emissions were reasonably well reproduced by a two-layer resistance model. Overall, between 10% and 14% of the total nitrogen applied was volatilised. (C)

Ammonia volatilisation following urea fertilisation in an irrigated sorghum crop in Italy

Di Tommasi P;Magliulo V;
2014

Abstract

Ammonia (NH3) fluxes were estimated by three inverse modelling methods over a sorghum field following the application of 240 kg N ha(-1) of urea pills under a semi-arid Mediterranean climate. Ammonia volatilisation started following irrigation, which coincided with the third urea application. The maximum volatilisation rate was reached 7 days after irrigation. A clear dependence of the NH3 volatilisation on irrigation and rainfall events was observed. The NH3 fluxes ranged from 2.5 to 45 mu g NH3 m(-2) s(-1). The canopy compensation point jumped from 9 mu g NH3 m(-3) before urea hydrolysis to 131 mu g NH3 m-3 afterwards, while the soil compensation point varied in the meantime from 24 to 800 mu g NH3 m-3 on average. The soil-dominated observed NH3 emissions were reasonably well reproduced by a two-layer resistance model. Overall, between 10% and 14% of the total nitrogen applied was volatilised. (C)
2014
Istituto per i Sistemi Agricoli e Forestali del Mediterraneo - ISAFOM
Inglese
195
179
191
13
http://www.sciencedirect.com/science/article/pii/S0168192314001270
Sì, ma tipo non specificato
Inverse modelling
QC-TILDAS
Emission factor
Resistance model
10
info:eu-repo/semantics/article
262
Ferrara, R M; Loubet, B; Decuq, C; Palumbo, A D; Di Tommasi, P; Magliulo, V; Masson, S; Personne, E; Cellier, P; Rana, G
01 Contributo su Rivista::01.01 Articolo in rivista
restricted
   Integrated Carbon Observation System
   ICOS
   FP7
   211574

   The nitrogen cycle and its influence on the European greenhouse gas balance
   NITROEUROPE IP
   FP6
   17841
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/271474
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