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Simulation of N 2 O emissions from a urine‐affected pasture in New Zealand with the ecosystem model DayCent
Author(s) -
Stehfest Elke,
Müller Christoph
Publication year - 2004
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2003jd004261
Subject(s) - nitrification , pasture , nitrous oxide , soil water , water content , ammonium , environmental science , denitrification , nitrate , environmental chemistry , evapotranspiration , hydrology (agriculture) , nitrogen , atmospheric sciences , chemistry , zoology , soil science , ecology , forestry , geology , geography , geotechnical engineering , organic chemistry , biology
We used the trace gas model DayCent to simulate emissions of nitrous oxide (N 2 O) from a urine‐affected pasture in New Zealand. The data set for this site contained year‐round daily emissions of nitrification‐N 2 O (N 2 O nit ) and denitrification‐N 2 O (N 2 O den ), meteorological data, soil moisture, and at least weekly data on soil ammonium (NH 4 + ) and nitrate (NO 3 − ) content. Evapotranspiration, soil temperature, and most of the soil moisture data were reasonably well represented. Observed and simulated soil NH 4 + concentrations agreed well, but DayCent underestimated the NO 3 − concentrations, due possibly to an insufficient nitrification rate. Modeled N 2 O emissions (18.4 kg N 2 O‐N ha −1 yr −1 ) showed a similar pattern but exceeded observed emissions (4.4 kg N 2 O‐N ha −1 yr −1 ) by more than 3 times. Modeled and observed N 2 O emissions were dominated by peaks following N‐application and heavy rainfall events and were favored under high soil temperatures. The contribution of N 2 O den was simulated well except for a 4‐week period when water‐filled pore space was overestimated and caused high N 2 O emissions which accounted for one third of the simulated annual N 2 O emissions. N 2 O nit fluxes were overestimated with DayCent because they are calculated as a fixed proportion of NH 4 + converted to NO 3 − , while the data suggest that significant rates of nitrification can occur without inducing significant N 2 O emissions. The comprehensive data set made it possible to explain discrepancies between modeled and observed values. In‐depth model validations with detailed data sets are essential for a better understanding of the internal model behavior and for deriving possible model improvements.

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