Turbulent dispersion of pollutants in urban-type canopies under stable stratification conditions. (May 2017)

• Record Type: Journal Article
• Authors: Shen, Zhi; Cui, Guixiang; Zhang, Zhaoshun
• Is Part Of: Atmospheric environment. Volume 156(2017)
• Page Start: 1
• Page End: 14
• Publication Date: 2017-05
• Subjects: Urban dispersion -- Stable stratification -- Large eddy simulation -- Flow pattern; Air -- Pollution -- Periodicals; Air -- Pollution -- Meteorological aspects -- Periodicals; 551.51
• DOI: 10.1016/j.atmosenv.2017.02.017
• Languages: English
• ISSNs: 1352-2310

Abstract

Abstract: Large eddy simulation is performed for the dispersion of a passive scalar in the turbulent boundary layer over an urban-like roughness surface under neutral and stable stratification. Square arrays of cubical obstacles are used to model the urban canopy with a ground level point source located in front of the obstacle. We design cases for varying building intervals to investigate the relationship between flow patterns and dispersion processes for different plan area densities λ p . It has been found (Shen et al. 2015) that flow patterns in a three-dimensional urban canopy can be classified into five basic regimes in neutral stratification: isolated roughness, external wake interference, internal wake interference, skimming flow and streets network. This classification still holds in the presence of moderately stable stratification. In area with large λ p, the material released from the point source tends to be trapped by the leeward recirculation and is well-mixed inside the canopy. The mean concentration level within roughness canopies is high due to the reduced advection velocity. In area with small λ p, the great part of the material is entrained into the horseshoe vortex wrapping around the obstacle and carried downwind. The material is concentrated in the lower region of the canopy with a relatively higher temporal fluctuation. In the presence of stable stratification, the spread of the plume is reduced and the temporal fluctuation is suppressed as well. For area of large λ p, the advective part of the scalar flux is responsible for carrying the material at ground level aloft into the urban canopy layer. Highlights: Development of a LES method is applicable to stably stratified turbulent flow. Patterns of the urban canopy flow are classified with varying plan area densities. Flow patterns inside the canopy are similar between neutral and stable conditions. Evolution of pollutant plumes are found to be affected by the stable stratification. Proportion of advection and diffusion in scalar flux depend on packaging densities.