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Traffic Kinematic Waves at Road Hump Zone:Perceptions and Analysis

机译:驼峰区交通运动波的感知与分析

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Aims: Traffic kinematic and shockwaves have often been used interchangeably in any literatures.The paper investigated traffic kinematic waves at road hump zone and their shockwave implications.Study Design: Road hump impact study.Place and Duration of Study: The study was carried out at locations along Jalan Universiti, Skudai, Johor Malaysia, between April 2012 and October 2012.Methodology: Based on the hypothesis that road hump cannot be held solely accountable for traffic shockwave occurrences, with and without road hump impact study was carried out at four sites in Malaysia. Road section was divided into two sections A (without road hump) and B (with road hump). Traffic volume, speed, headway, gaps and vehicle types were collected with automatic traffic counters continuously for eight weeks. Empirical data were supplemented with design data supplied by ministry of works. Data were collated and compared.Results: Results show that road humps are effective speed reduction mechanism. Although speed reductions were recorded, traffic shockwaves were not recorded and also there was no evidence to suggest that significant kinematic waves were caused at road humps. Differences between traffic shockwave and kinematic wave results affirmed that traffic shockwave will only occur at the capacity constrained section of flow/density curve.Conclusion: The paper asserted that traffic kinematic wave and shockwave propagations are related but not the same and concluded that road humps cannot be held solely accountable for traffic shockwaves. Further, that traffic shockwave is more likely to be caused by the led driver’s erratic behaviour on approach to the barrier.
机译:目的:交通运动波和冲击波在任何文献中都经常互换使用,本文研究了道路驼峰区的交通运动波及其冲击波的研究设计:道路驼峰的影响研究研究的地点和持续时间:该研究在2012年4月至2012年10月,在马来西亚柔佛州士古来的惹兰大学(Jalan Universiti)进行研究。方法:基于以下假设:在有或没有道路驼峰影响研究的情况下,道路驼峰不能仅对交通冲击波的发生负责。马来西亚。道路部分分为A(无驼峰)和B(有驼峰)两部分。使用自动交通计数器连续八周收集交通量,速度,行进距离,差距和车辆类型。经验数据由工程部提供的设计数据进行了补充。结果:结果表明,驼峰是有效的减速机制。尽管已记录了减速,但未记录到交通冲击波,也没有证据表明在道路驼峰处产生了很大的运动波。交通冲击波与运动波结果之间的差异证实了交通冲击波只会在流量/密度曲线的能力约束部分发生。结论:本文断言交通运动波与冲击波的传播是相关的,但并不相同,并得出结论:道路驼峰不能仅对交通冲击波负责。此外,交通冲击波很可能是由驾驶员在驶入障碍物时的不正常行为引起的。

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