School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK.
School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK.
Environ Pollut. 2020 Nov;266(Pt 3):115223. doi: 10.1016/j.envpol.2020.115223. Epub 2020 Jul 20.
Traffic-generated ultrafine particles (UFPs) in the urban atmosphere have a high proportion of their composition comprised of semi-volatile compounds (SVOCs). The evaporation/condensation processes of these SVOCs can alter UFP number size distributions and play an important role in determining the fate of UFPs in urban areas. The neighbourhood-scale dispersion (over distances < 1 km) and evolution of traffic-generated UFPs for a real-world street network in central London was simulated by using the WRF-LES model (the large eddy simulation mode of the Weather Research and Forecasting modelling system) coupled with multicomponent microphysics. The neighbourhood scale dispersion of UFPs was significantly influenced by the spatial pattern of the real-world street emissions. Model output indicated the shrinkage of the peak diameter from the emitted profile to the downwind profile, due to an evaporation process during neighbourhood-scale dispersion. The dilution process and the aerosol microphysics interact with each other during the neighbourhood dispersion of UFPs, yielding model output that compares well with measurements made at a location downwind of an intense roadside source. The model captured the total SVOC concentrations well, with overestimations for gas concentrations and underestimations for particle concentrations, particularly of the lighter SVOCs. The contribution of the intense source, Marylebone Road (MR) in London, to concentrations at the downwind location (as estimated by a model scenario with emissions from MR only) is comparable with that of the rest of the street network (a scenario without emissions from MR), implying that both are important. An appreciable level of non-linearity is demonstrated for nucleation mode UFPs and medium range carbon SVOCs at the downwind receptor site.
交通产生的超细颗粒(UFPs)在城市大气中有很高的比例,其组成部分由半挥发性化合物(SVOCs)组成。这些 SVOCs 的蒸发/冷凝过程可以改变 UFP 的数浓度粒径分布,并在决定 UFPs 在城市地区的命运方面发挥重要作用。利用 WRF-LES 模型(天气研究和预测建模系统的大涡模拟模式)结合多组分微物理,模拟了伦敦市中心真实街道网络中交通产生的 UFPs 的局域尺度扩散(距离<1km)和演化。UFPs 的局域尺度扩散受到真实街道排放的空间模式的显著影响。模型输出表明,由于局域尺度扩散过程中的蒸发过程,从发射轮廓到顺风轮廓的峰值直径缩小。稀释过程和气溶胶微物理在 UFPs 的局域扩散过程中相互作用,产生的模型输出与在强路边源下风处测量的结果相吻合。该模型很好地捕捉了总 SVOC 浓度,对气体浓度的高估和对颗粒浓度的低估,特别是对较轻的 SVOCs。伦敦马里波恩路(MR)强烈源对下风处浓度的贡献(通过仅来自 MR 的排放的模型情景估计)与街道网络其余部分的贡献相当(没有来自 MR 的排放的情景),这表明两者都很重要。在下游受体位置,对成核模态 UFPs 和中程碳 SVOCs 表现出相当大的非线性水平。