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The influence of meteorology, urban topography and traffic on the variability in concentrations of a traffic-related pollutant in urban street canyons

机译:气象,城市地形和交通对城市街道峡谷交通污染物浓度变化的影响

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摘要

A comprehensive study into the spatial and temporal variations in concentrations of a traffic-related pollutant was undertaken in two urban street canyons located in York, U. K. During the field experiment, investigations were carried out in order to determine the influence of meteorology, urban topography and traffic on the measured concentrations of a traffic-related pollutant. The pollutant measured in this study was carbon monoxide (CO). Results are presented from simultaneous and continuous measurements of the background (or reference) wind speed and direction, the in-canyon wind and turbulence fields, traffic characteristics and CO concentrations collected over a period of one month. The background wind was found to influence the development of in-canyon wind flow features, which became mechanisms for pollutant dispersion. Under certain background winds, evidence of across-canyon recirculating flows with horizontally- and vertically-aligned axes is presented. During these conditions, turbulence and traffic-related pollutants are likely to have been transported in the across-canyon re-circulating flows. During background wind orientated perpendicular to the street axis, the 15-minute mean concentrations of CO were a factor of 2 or 3 higher on the leeward (or upwind) side of the street canyons compared to the windward side. This was caused by the development of an across-canyon recirculating flow with a horizontally-aligned axis. Down draughts were measured on the windward side of the canyon during these conditions, while updraughts were measured on the leeward side. The wind direction at street level opposed the direction of the above-roof flow, causing the transport of CO towards the leeward side of the street canyon where concentrations increased. Evidence Results are presented from simultaneous and continuous measurements of the background (or reference) wind speed and direction, the in-canyon wind and turbulence fields, traffic characteristics and CO concentrations collected over a period of one month. The background wind was found to influence the development of incanyon wind flow features, which became mechanisms for pollutant dispersion. Under certain background winds, evidence of across-canyon re circulating flows with horizontally- and vertically-aligned axes is presented. During these conditions, turbulence and traffic-related pollutants are likely to have been transported in the across-canyon re circulating flows. During background wind orientated perpendicular to the street axis, the 15-minute mean concentrations of CO were a factor of 2 or 3 higher on the leeward (or upwind) side of the street canyons compared to the windward side. This was caused by the development of an across-canyon recirculatingf low with a horizontally-aligned axis. Downdraughts were measured on the windward side of the canyon during these conditions, while updraughts were measured on the leeward side. The wind direction at street level opposed the direction of the above-roof flow, causing the transport of CO towards the leeward side of the street canyon where concentrations in creased. Evidence of counter-rotating comer vortices with vertically-aligned axes are also presented and are thought to have been caused by along-canyon converging flows during certain background winds. However, across-canyon flow during these conditions also accounted for the higher concentrations of CO measured on the leeward side of the canyon, compared to the windward side. Background winds orientated oblique to the street axis were found to produce across-canyon rearticulating flows. On the other hand, parallel background winds produced channel flows, which had a 'flushing' effect, causing some of the lowest concentrations of CO to be measured during these conditions. Traffic-produced turbulence was investigated in the street canyon during the field experiment. Comparisons were made between calculated and measured turbulence parameters. The results indicate that the parameterisation performs reasonably well, particularly during weak perpendicular background winds when traffic-produced turbulence effects are likely to have been most dominant. The traffic was also investigated due to the implications of traffic characteristics on the variability in concentrations of CO. The influence of free-, unstable- and congested-traffic flows on measured CO concentrations was determined. The highest mean concentrations were measured during congested traffic conditions, when the emission levels are likely to have been elevated due to stop-start driving events. The combined influence of the background wind and traffic characteristics was investigated. Results are presented which show that the highest mean CO concentrations were measured during perpendicular background winds and during congested traffic conditions. The implications of using variable emission rates in a computational fluid dynamics (CFD) dispersion model were investigated in a sensitivity study. Results are also presented from the flow model study, which was conducted to help in the interpretation of the field experiment data.
机译:在英国约克的两个城市街道峡谷中,对交通相关污染物浓度的时空变化进行了全面研究。在野外实验中,进行了调查以确定气象,城市地形和地形的影响。流量取决于所测量的与交通相关的污染物的浓度。在这项研究中测量的污染物是一氧化碳(CO)。结果来自同时(连续)测量背景(或参考)风速和风向,峡谷内风和湍流场,交通特征以及在一个月内收集的一氧化碳浓度。发现背景风影响峡谷内风流特征的发展,这成为污染物扩散的机制。在某些背景风的作用下,提供了横轴和纵轴对齐的跨峡谷再循环流的证据。在这些情况下,湍流和与交通有关的污染物可能已经在跨峡谷的再循环流中被运输了。在垂直于街道轴定向的背景风中,与上风侧相比,街道峡谷的背风(或上风)侧的15分钟平均CO浓度高2到3倍。这是由于水平轴线对齐的跨峡谷循环流的发展引起的。在这些情况下,在峡谷的上风侧测量了下吃水,而在下风侧测量了吃水。街道水平的风向与屋顶流动方向相反,导致CO向着浓度增加的街道峡谷的下风侧输送。证据结果是通过同时(连续)测量背景(或参考)风速和风向,峡谷内风场和湍流场,交通特征以及在一个月内收集的一氧化碳浓度得出的。发现背景风会影响incanyon风流特征的发展,这成为了污染物扩散的机制。在某些背景风的作用下,提供了横轴和纵轴对齐的跨峡谷再循环流的证据。在这些情况下,湍流和与交通有关的污染物很可能已经在整个峡谷的再循环流中被运输了。在垂直于街道轴定向的背景风中,与上风侧相比,街道峡谷的背风(或上风)侧的15分钟平均CO浓度高2到3倍。这是由于开发出了一个水平对齐的轴跨峡谷循环流。在这些情况下,在峡谷的上风侧测量了下风量,而在下风侧测量了下风量。街道水平的风向与屋顶上方的流动方向相反,导致CO向着浓度增加的街道峡谷的下风侧输送。还提供了具有垂直对齐轴的逆转角涡旋的证据,并认为这是由某些背景风期间沿峡谷汇聚的流动引起的。但是,与顺风侧相比,在这些条件下跨峡谷流动也导致了在峡谷的背风侧测得的较高的CO浓度。发现倾斜于街道轴线的背景风会产生跨峡谷的网格状流动。另一方面,平行的背景风产生通道流,这具有“冲洗”效应,导致在这些条件下测得的一些最低浓度的CO。在野外实验期间,在街道峡谷中调查了交通产生的湍流。在计算和测量的湍流参数之间进行了比较。结果表明,该参数设置的效果相当好,尤其是在垂直垂直背景风较小的情况下,此时由交通产生的湍流效应可能是最主要的。由于交通特性对CO浓度变化的影响,还对交通进行了调查。确定了自由,不稳定和拥挤交通流量对测得的CO浓度的影响。在交通拥挤的情况下测得的最高平均浓度,这是因为停车/停车驾驶事件可能导致排放水平升高。研究了背景风和交通特性的综合影响。结果表明,在垂直背景风和拥挤的交通状况下,测得的最高平均CO浓度。在敏感性研究中研究了在计算流体动力学(CFD)扩散模型中使用可变排放速率的含义。流动模型研究还提供了结果,该研究旨在帮助解释现场实验数据。

著录项

  • 作者

    Boddy John William Douglas;

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  • 年度 2005
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  • 原文格式 PDF
  • 正文语种 English
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