SIMULATING SULFUR-DIOXIDE PLUME DISPERSION AND SUBSEQUENT DEPOSITION DOWNWIND FROM A STATIONARY POINT-SOURCE - A MODEL

Citation
Cpa. Bourque et Pa. Arp, SIMULATING SULFUR-DIOXIDE PLUME DISPERSION AND SUBSEQUENT DEPOSITION DOWNWIND FROM A STATIONARY POINT-SOURCE - A MODEL, Environmental pollution, 91(3), 1996, pp. 363-380
Citations number
32
Categorie Soggetti
Environmental Sciences
Journal title
ISSN journal
02697491
Volume
91
Issue
3
Year of publication
1996
Pages
363 - 380
Database
ISI
SICI code
0269-7491(1996)91:3<363:SSPDAS>2.0.ZU;2-0
Abstract
Dispersion and subsequent deposition of SO2 downwind from a stationary point source are affected by several transport processes: buoyancy at the source, advection, and air turbulence en route from the source to the area of impact. In this paper, SO2 transport processes are simula ted by way of Lagrangian air parcel trajectory simulations. In these s imulations, the source releases air parcels in puffs. The calculations cover both daytime and night-time conditions and take into account: ( i) solar geometry, (ii) diurnal variations of wind speed and air turbu lence, (iii) resistance to the transfer of SO2 from the air to the lan d, and (iv) flat terrain. Deposition to the forest is determined by ca lculating the rate of SO2 flux from individual air parcels to the land according to the parcel's velocity and an assumed air-to-surface SO2 transfer coefficient. Daily cumulative SO2 deposition rates are calcul ated by summing the simulated diffusional fluxes of SO2 from air to la nd over each simulated time step. Daily cumulative SO2 amounts are cal culated for downwind distances from 0 to 42 km, for smokestack heights from 30 to 200 m, and for each day of the year according to historica l year-round and local weather patterns representative of days with ne utral conditions and days with transitions from stable to unstable con ditions. Annual per hectare rates of SO2 deposition are calculated by way of Monte Carlo simulations, according to historical patterns for d aily wind, atmospheric stability, and precipitation. These simulations are calibrated for the area surrounding a coal-burning power generato r at Grand Lake in south-central New Brunswick, Canada. Calculated con centrations for SO2 were similar to those obtained with a mobile SO2 d etection unit and a SO2-monitoring unit 42 km NE from the emission sou rce. Cumulative SO2 deposition rates were reasonably similar to those obtained with PbO2 sulfation plates. A detailed comparison revealed to pography was an important factor in modifying actual cumulative SO2 de position rates.