首页> 外文会议>International conference on urban air quality-measurement, modeling and management >RESULTS FROM THREE FIELD TRACER EXPERIMENTS ON THE NEIGHBOURHOOD SCALE IN THE CITY OF BIRMINGHAM UK
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RESULTS FROM THREE FIELD TRACER EXPERIMENTS ON THE NEIGHBOURHOOD SCALE IN THE CITY OF BIRMINGHAM UK

机译:三个现场示踪实验对伯明翰市英国市邻里规模的实验

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The physical processes governing flow and pollutant dispersion at the neighbourhood scale, a spatial scale intermediate between the street scale and the city scale, is not well understood. Furthermore, it is not clear whether a traditional approach using averaged characteristics such as the aerodynamic roughness length is sufficient to predict the concentration field at this scale. To investigate pollutant dispersion in a real urban area, three field experiments were designed within the UK-URGENT programme sponsored by NERC. The experiments were performed in the City of Birmingham using a finite duration release of inert, non-toxic and non-depositing tracers, vis. per-fluoromethylcyclohexane (PMCH) and perfluoromethylcyclopentane (PMCP). Measurements were taken using air bag samplers placed in an arc at 3.5 km (first experiment) and 1 km (second and third experiments) from the source; some trap samplers were placed outside the main arc in the outskirts of the city. Measurements were analysed in the laboratory using a novel gas-chromatography technique. Data so obtained were compared with predictions from a simple steady-state model and a time-dependent model. The concentration-time series were very asymmetrical with a sharp rise, a plateau followed by a relatively slow decrease and finally a long-lived plateau above (or possibly very slow decrease to) the background level.
机译:管理流动和污染物分散在邻域鳞的物理过程,街道规模与城市规模之间的空间秤中间,并不了解。此外,目前尚不清楚使用诸如空气动力学粗糙度长度的平均特性的传统方法是否足以以这种规模预测浓度场。为了调查真实城区的污染物分散,三个现场实验是在NERC赞助的英国紧急计划中设计的。使用惰性,无毒和不沉积的示踪剂的有限持续时间释放,在伯明翰市进行实验。每氟甲基环己烷(PMCH)和全氟甲基环戊烷(PMCP)。使用从源3.5 km(第一实验)和1 km(第二和第三实验)的弧形放置在弧形中的空气袋采样器进行测量;一些陷阱取样器被放置在城市郊区的主弧外。使用新型气相色谱技术在实验室分析测量。将如此获得的数据与来自简单稳态模型的预测和时间依赖模型进行了比较。浓度 - 时间序列非常不对称,剧烈升高,高原随后是相对缓慢的减少,最后一个高于(或可能非常缓慢地减少)背景水平。

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