Three-dimensional characterization of the ammonia plume from a beef cattle feedlot
In Canada approximately 45% of ammonia (NH 3) emissions are attributed to dairy and beef cattle industries. The present study focused on NH 3 emissions from a beef feedlot with a one-time capacity of 17,220 head. The aim was to improve the Canadian NH 3 emission inventories and air quality forecasti...
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Veröffentlicht in: | Atmospheric environment (1994) 2009-12, Vol.43 (38), p.6091-6099 |
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Sprache: | eng |
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Zusammenfassung: | In Canada approximately 45% of ammonia (NH
3) emissions are attributed to dairy and beef cattle industries. The present study focused on NH
3 emissions from a beef feedlot with a one-time capacity of 17,220 head. The aim was to improve the Canadian NH
3 emission inventories and air quality forecasting capabilities. A Cessna 207, equipped with a fast-response NH
3/NO
y detector and a quadrupole aerosol mass spectrometer, was flown in a grid pattern covering an area of 8 × 8 km centered on a feedlot (800 × 800 m) at altitudes ranging from 30 to 300 m above ground. Stationary ground measurements of NH
3 concentration and turbulence parameters were made downwind of the feedlot. Three flights were conducted under varying meteorological conditions, ranging from very calm to windy with near-neutral stratification. NH
3 mixing ratios up to 100 ppbv were recorded on the calm day, up to 300 m above ground. An average feedlot NH
3 emission rate of 76 ± 4 μg m
−2 s
−1 (equivalent to 10.2 g head
−1 h
−1) was estimated. Characteristics of the measured NH
3 plume were compared to those predicted by a Lagrangian dispersion model. The spatially integrated pattern of NH
3 concentrations predicted and measured agreed but the measured was often more complex than the predicted spatial distribution. The study suggests that the export of NH
3 through advection accounted for about 90% of the emissions from the feedlot, chemical transformation was insignificant, and dry deposition accounted for the remaining 10%. |
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ISSN: | 1352-2310 1873-2844 |
DOI: | 10.1016/j.atmosenv.2009.08.045 |