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Large-eddy simulation for flow and dispersion in urban streets
Authors:Zheng-Tong Xie  Ian P Castro
Institution:1. CENSAM, Singapore-MIT Alliance for Research and Technology, Singapore;2. Department of Urban Studies and Planning, Massachusetts Institute of Technology, Cambridge, MA, USA;3. Department of Architecture, Massachusetts Institute of Technology, Cambridge, MA, USA;1. Department of Atmospheric Sciences, School of Environmental Science and Engineering of Sun Yat-Sen University, Guangzhou, P. R. China;2. Department of Mechanical Engineering, The University of Hong Kong, Pokfulam, Hong Kong;3. School of Construction Management and Engineering, University of Reading, Reading, UK;4. Laboratory of Ventilation and Air Quality, University of Gävle, SE-80176 Gävle, Sweden;1. Department of Civil and Environmental Engineering, Shantou University, 243 Daxue Road, Shantou, 515063, Guangdong province, China;2. President, Tokyo Polytechnic University, 1583 Iiyama, Atsugi, 243-0297, Kanagawa, Japan
Abstract:Large-eddy simulations (LES) with our recently developed inflow approach (Xie, Z.-T., Castro, I.P., 2008a. Efficient generation of inflow conditions for large-eddy simulation of street-scale flows. Flow Turbul. Combust., vol. 81(3), pp. 449–470.) have been used for flow and dispersion within a genuine city area – the DAPPLE site, located at the intersection of Marylebone Rd and Gloucester Pl in Central London. Numerical results up to second-order statistics are reported for a computational domain of 1.2 km (streamwise) × 0.8 km (lateral) × 0.2 km (in full scale), with a resolution down to approximately one meter in space and one second in time. They are in reasonable agreement with the experimental data. Such a comprehensive urban geometry is often, as here, composed of staggered, aligned, square arrays of blocks with non-uniform height and non-uniform base, street canyons and intersections. Both the integrative and local effect of flow and dispersion to these geometrical patterns were investigated. For example, it was found that the peaks of spatially averaged urms, vrms, wrms and <uw′> occurred neither at the mean height nor at the maximum height, but at the height of large and tall buildings. It was also found that the mean and fluctuating concentrations in the near-source field is highly dependent on the source location and the local geometry pattern, whereas in the far field (e.g. >0.1 km) they are not. In summary, it is demonstrated that full-scale resolution of around one meter is sufficient to yield accurate prediction of the flow and mean dispersion characteristics and to provide reasonable estimation of concentration fluctuations.
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