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Modeling reactive pollutant dispersion in an urban street canyon
Institution:1. School of Earth and Environmental Sciences, Seoul National University, Seoul 151-742, Republic of Korea;2. Numerical Weather Prediction Division, Korea Meteorological Administration, Seoul 156-720, Republic of Korea;1. Department of Environmental Engineering and Energy, Myongji University, Yongin, Gyunggi, Republic of Korea;2. School of Earth and Environmental Sciences, Seoul National University, Seoul, Republic of Korea;3. Department of Environmental Atmospheric Sciences, Pukyong National University, Busan, Republic of Korea;4. Department of Environmental Engineering, Sunchon National University, Suncheon, Jeonnam, Republic of Korea;5. Air Quality Forecasting Center, Climate and Air Quality Research Department, National Institute of Environmental Research, Incheon, Republic of Korea
Abstract:Reactive pollutant dispersion in an urban street canyon with a street aspect ratio of one is numerically investigated using a computational fluid dynamics (CFD) model. The CFD model developed is a Reynolds-averaged Navier–Stokes equations (RANS) model with the renormalization group (RNG) k–ε turbulence model and includes transport equations for NO, NO2, and O3 with simple photochemistry. An area emission source of NO and NO2 is considered in the presence of background O3 and street bottom heating (ΔT=5 °C) with an ambient wind perpendicular to the along-canyon direction. A primary vortex is formed in the street canyon and the line connecting the centers of cross-sectional vortices meanders over time and in the canyon space. The cross-canyon-averaged temperature and reactive pollutant concentrations oscillate with a period of about 15 min. The averaged temperature is found to be in phase with NO and NO2 concentrations but out of phase with O3 concentration. The photostationary state defect is small in the street canyon except for near the roof level and the upper downwind region of the canyon and its local minimum is observed near the center of the primary vortex. The budget analysis of NO (NO2) concentration shows that the magnitude of the advection or turbulent diffusion term is much larger (larger) than that of the chemical reaction term and that the advection term is largely balanced by the turbulent diffusion term. On the other hand, the budget analysis of O3 concentration shows that the magnitude of the chemical reaction term is comparable to that of the advection or turbulent diffusion term. The inhomogeneous temperature distribution itself affects O3 concentration to some extent due to the temperature-dependent photolysis rate and reaction rate constant.
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