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61.
针对基于宏观基本图(MFD)的路网多子区协同控制未考虑各子区拥堵状态差异性及均衡性的问题,本文提出以多子区状态可达一致为目标的子区边界状态反馈控制设计方法. 首先,基于路网 MFD模型建立路网多子区协同模型;进一步,基于部分变量稳定性理论,设计多子区状态可达一致的边界状态反馈控制律.在此基础上,考虑子区拥堵状态的差异性,设计了子区间的协同控制策略,快速缓解子区拥堵状态;同时,提出子区边界输入流的分配优化策略.最后,以潍坊市实际路网为背景建立仿真模型.实验结果表明,本文方法可实现子区交通流分布的均衡性,快速缓解子区拥堵状态,较大幅度地提升路网运行效率. 相似文献
62.
《Vehicle System Dynamics: International Journal of Vehicle Mechanics and Mobility》2012,50(11):1061-1082
The dynamic model was developed to evaluate vibration accelerations and ride comforts during the running of the Korean-standardised rubber-tired light rail vehicle. Ride comfort indexes were analysed and tested in accordance with UIC 513R by using the dynamic model and the actual vehicle in the test track. Based on the comparisons between analysis results and test results, the validity of the developed dynamic model was evaluated. It was verified whether or not the developed Korean-standardised rubber-tired light rail vehicle met the specified target specification on ride comfort. In addition, the influence of the wearing of guide wheels on ride comfort was estimated. 相似文献
63.
奇摄动三阶非线性边值问题 总被引:1,自引:1,他引:0
利用微分不等式技巧和Volterra型积分算子,研究了三阶非线性奇摄动边值问题εx^(3)=f(t,x,x′,w(ε)x^(3),ε),g(x′(0),x″(0)=0,x(1)=A,x′(1)=B的存在性及渐近估计。 相似文献
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65.
文章选取了7辆车进行噪声舒适性主客观评价试验,客观评价指标为驾驶员耳边噪声值,主观评价指标为滚动噪声、边棱敏感性等5个,评车师根据试验情况对试验车各指标进行打分并给出总分值。比较了不同试验车速车辆前后排的噪声值,并对主、客观数值进行多元回归分析。 相似文献
66.
斜拉索由于具有自身质量轻、结构刚度差、结构阻尼小和自身长细比大的特点,极容易发生风(雨)致振动,对桥梁结构的安全性能产生很大的影响,而斜拉索作为斜拉桥的重要受力构件,准确掌握其风荷载对于桥梁抗风设计具有重要意义,特别是斜拉索在生产、运输和安装过程中表面可能受到损伤,该斜拉索在临界雷诺数区的气动力特性和流场特性更是值得研究的问题。针对此种状况,通过同步测力风洞试验,对表面无损伤斜拉索模型和表面损伤斜拉索模型在不同风攻角下的升力系数进行时程分析,得到边界层转捩的3个区域;将升力系数时程进行快速傅里叶变换计算得到升力时程频谱图,并通过频谱图分析随机信号的频域特征;对比从雷诺数亚临界、临界到超临界区表面无损伤和表面损伤斜拉索的流场变化,并从周围流场变化的角度分析雷诺数临界区斜拉索气动稳定性及可能的机理。研究结果表明:表面无损伤和表面损伤模型的升力系数随雷诺数的变化规律基本一致,二者的升力时程在TrBL0向TrBL1阶段和TrBL1向TrBL2阶段过渡过程中会出现双稳态现象,损伤会影响斜拉索尾流区旋涡脱落的情况,进而对不同雷诺数下的Strouhal数值变化产生一定的影响。 相似文献
67.
68.
列车纵向冲击的检测与分析 总被引:2,自引:1,他引:1
针对列车纵向冲击问题,提出了信号采集与处理方案,设计了一套随车采集和分析系统。文中介绍了系统组成、工作原理及运行过程,初步建立了纵向冲击与旅客乘坐舒适度之间的数学模型,并运用该模型进行了实际演算,取得了预期的效果。 相似文献
69.
Laurence C. Breaker David B. Gilhousen Hendrik L. Tolman Lawrence D. Burroughs 《Journal of Marine Systems》1998,16(3-4)
Measurements of boundary layer moisture have been acquired from Rotronic MP-100 sensors deployed on two NDBC buoys in the northern Gulf of Mexico from June through November 1993. For one sensor, which was retrieved approximately 8 months after deployment, the post- and precalibrations agreed closely and fell well within WMO specifications for accuracy. The second sensor operated continuously from June 1993 to February 1997 (3.5 years). Buoy observations of relative humidity and supporting data were used to calculate specific humidity and the surface fluxes of latent and sensible heat. Specific humidities from the buoys were compared with observations of moisture obtained from nearby ship reports, and the correlations were generally high (0.7–0.9). Surface gravity wave spectra were also acquired. The time series of specific humidity and the other buoy parameters revealed three primary scales of variability, small (h), synoptic (days), and seasonal (months). The synoptic variability was clearly dominant and occurred primarily during September, October, and November. Most of the synoptic variability was due to frontal systems that dropped down into the Gulf of Mexico from the continental US followed by air masses which were cold and dry. Cross-correlation analyses of the buoy data indicated that: (1) the moisture field was highly coherent over distances of 800 km or more in the northern Gulf of Mexico; and (2) both specific humidity and air temperature served as tracers of the motion associated with propagating atmospheric disturbances. These correlation analyses also revealed that the prevailing weather systems generally entered the buoy domain from the South prior to September, but primarily from the North thereafter. Spectra of the various buoy parameters indicated strong diurnal and semidiurnal variability for barometric pressure and sea surface temperature (SST) and lesser variability for air temperature, wind speed and significant wave height. The surface fluxes of latent and sensible heat were dominated by the synoptic events which took place from September through November with the transfer of latent heat being primarily from the ocean to the atmosphere. Finally, an analysis of the surface wave observations from each buoy, which included calculations of wave age and estimates of surface roughness, indicate that major heat and moisture flux events coincide with periods of active wave growth, although the data were insufficient to identify any causal relationships. 相似文献
70.