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Mass Transfer Velocity and Momentum Vertical Exchange in Simulated Deep Street Canyons

机译:模拟深街峡谷的传质速度和动量垂直交换

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A box model to simulate mass transfer inside deep street canyons and with atmospheric flow above is introduced and discussed. Two ideal deep street canyons with aspect ratios of 3 and 5 (the aspect ratio being the ratio between building height and street width H/W) are considered. This range of aspect ratios, found in many densely populated historical centres in Mediterranean cities as well as in other cities around the world, potentially creates high air pollutant concentration levels. Our model isbased on a combination of analytical solutions and computation fluid dynamics (CFD) simulations using carbon monoxide (CO) as a tracer pollutant. The analytical part of the model is based on mass transfer velocity concepts while CFD simulations are usedboth for a preliminary validation of the physical hypothesis underlying the model (steady-state simulations) and to evaluate the concentration pattern with time (transient or wash-out simulations). Wash-out simulation curves were fitted by model curves,and mass transfer velocities were evaluated through a best-fitting procedure. Upon introducing into the model the contribution of traffic-produced turbulence, the modelled CO concentration levels became comparable with those obtained in real-world monitoring campaigns. The mass transfer rate between the canyon and the above atmosphere was then expressed in terms of an overall mass transfer velocity, which directly allows the evaluation of the mass transfer rate between the bottom volume of the canyon (pedestrian level) with the above atmosphere. Overall mass transfer velocities are reported as a function of the operating conditions studied (H/W = 3-5 and wind speeds = 2-8 ms~(-1)). Finally, a simple expression is reported for determining pollutant concentrations at the pedestrian level based on the overall mass transfer velocity defined.
机译:介绍并讨论了一个模拟深街道峡谷内部以及上面有大气流动的传质的盒子模型。考虑两个纵横比分别为3和5(纵横比为建筑物高度与街道宽度H / W之比)的理想深街道峡谷。在地中海城市以及世界其他城市的许多人口稠密的历史中心中发现的宽高比范围,可能会导致空气污染物浓度较高。我们的模型基于分析解决方案和使用一氧化碳(CO)作为示踪污染物的计算流体动力学(CFD)模拟的组合。该模型的分析部分基于传质速度概念,而CFD模拟都用于对模型基础的物理假设(稳态模拟)进行初步验证,并评估随时间变化的浓度模式(瞬态或冲洗模拟) )。通过模型曲线拟合洗脱模拟曲线,并通过最佳拟合程序评估传质速度。在将模型中交通产生的湍流的贡献引入模型后,模拟的一氧化碳浓度水平变得与在现实世界的监测活动中获得的浓度相当。然后,以整体传质速度表示峡谷与上述大气之间的传质速率,这直接允许评估上述大气与峡谷底部体积(行人水平)之间的传质速率。报告的整体传质速度是所研究的操作条件的函数(H / W = 3-5,风速= 2-8 ms〜(-1))。最后,报告了一个简单的表达式,用于根据定义的整体传质速度确定行人水平的污染物浓度。

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