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排序方式: 共有206条查询结果,搜索用时 234 毫秒
1.
基于前轮转角约束自适应模型预测控制的路径跟踪研究 总被引:1,自引:0,他引:1
针对在车辆行驶中较小的前轮转角无法充分利用路面附着能力,较大的前轮转角使得车辆的行驶稳定性差的问题,文章提出了一种前轮转角约束自适应模型预测方法。首先建立车辆的动力学模型,然后通过计算得到轮胎纵向力,最终得到车辆的前轮转角。将车辆的状态量与前轮转角自适应约束条件输入给模型预测控制器,输出车辆的前轮转角,实现对参考路径的跟踪。在Carsim和MATLAB平台上联合仿真,仿真结果表明前轮转角约束自适应模型预测控制的车辆相比固定转角约束的车辆具有较好的跟踪能力和稳定性。 相似文献
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由于隧道受洞口立交及其上跨线的影响,使隧道洞口仰坡较高,因此,隧道仰坡的稳定,直接影响隧道进洞和隧道营运安全。介绍塘朗山隧道出口高仰坡在施工过程中变形的原因、仰坡的稳定性分析和采取的加固设计方案。 相似文献
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隧道建设进入山区,仰坡开挖越来越高,而且洞口经常出现偏压现象,仰坡经常开裂失稳。应用锚索框架梁结合挡墙方案成功地解决了此类问题。 相似文献
5.
Juan Carlos Molinero Frdric Ibanez Sami Souissi Emmanuel Bosc Paul Nival 《Journal of Marine Systems》2008,69(3-4):271
High frequency sampling was performed in daylight hours along a 35 km transect in the Ligurian Sea to investigate the upper layer zooplankton distribution during the spring phytoplankton bloom. The results show detailed spatial structure and biomass of key zooplankton functional groups, copepods, salps and krill larvae, within the different water masses characterizing this region. Although observed values of total copepod biomass distribution were rather constant along the transect, species-specific patterns were observed in the copepod spatial distribution. The larger species Calanus helgolandicus, as well as Centropages typicus, Oithona spp., and Oncaea spp., were associated with the frontal zone. However, Acartia spp. had a scattered distribution, and Clausocalanus/Paracalanus did not have a clear pattern. In addition, krill larvae were concentrated in the frontal area and salps had a scattered pattern. The cross-shore zooplankton distribution appeared strongly influenced by both the Northern Ligurian current governing inshore waters, which acts as a major flushing forcing, and the Ligurian front, which governs offshore waters and may act as retention area for zooplankton. 相似文献
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转向前桥在汽车上一个非常重要的功能就是实现汽车转向,而转向角是决定转向前桥性能的一个非常重要的参数,本文解决了在桥总成装配线快速调整某转向前桥转向角问题。 相似文献
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汽车前桥工字梁是汽车中的重要部件,应具有足够的强度和刚度。首先按照厂家所提供的AUTOCAD图纸在UG中建立桥壳几何模型,然后在Hyperworks软件中进行网络划分,并进行加载和约束,完成有限元计算分析。 相似文献
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随着中国新基建战略的提出及自动驾驶和网联通信技术的不断发展,网联自动驾驶车辆(CAV)、自动驾驶车辆(AV)和常规人驾车辆混行的交通流将在未来长时间存在。建立适用于网联自动驾驶车辆、自动驾驶车辆和常规人驾车辆3种类型车辆的混流跟驰模型,考虑多前后车车头间距、多前车速度差、加速度差、与主体车辆的相对距离等因素,并进行典型场景的数值仿真。刹车和起步过程的3种混流数值仿真结果显示,模型在几种典型混行场景下均具有可行性,车辆的加速度和速度变化更为平缓。不同CAV比例下的数值仿真结果显示,车队中CAV比例越高,车队整体恢复至平稳状态的时间越短,波动幅度越小。CAV均质流数值仿真结果表明,与MHVAD模型相比,该模型不稳定区域减小33.8%,所控制的车队速度波动幅度减小14%。CAV与AV混流的数值仿真结果显示,与PATH实验室模型相比,由该模型控制的车队加速度进入相对稳定状态提前5.5 s。该模型可用于不同车辆均质流及3种车辆混行的队列控制,在目前开展混行实车试验困难的情况下,也可应用该模型进行混行跟驰仿真,从而为混行交通流的道路交通管理及基础设施布设提供理论依据和模型支持。 相似文献
9.
本文介绍了车辆前桥工字梁承孔在行驶当中踩刹车时突然断裂的机械事故的原因,阐述了公交车辆前桥工字梁承孔的重要性,论证了对公交车辆前桥工字梁承孔维修的必要性和重要性,得出了相关的方法和建议。 相似文献
10.
John H. Simpson J.A. Mattias Green Tom P. Rippeth Thomas R. Osborn W. Alex M. Nimmo-Smith 《Journal of Marine Systems》2009,77(4):428
We report on an intensive campaign in the summer of 2006 to observe turbulent energy dissipation in the vicinity of a tidal mixing front which separates well mixed and seasonally stratified regimes in the western Irish Sea. The rate of turbulent dissipation ε was observed on a section across the front by a combination of vertical profiles with the FLY dissipation profiler and horizontal profiles by shear sensors mounted on an AUV (Autosub). Mean flow conditions and stratification were obtained from a bed mounted ADCP and a vertical chain of thermistors on a mooring. During an Autosub mission of 60 h, the vehicle, moving at a speed of ~ 1.2 m s− 1, completed 10 useable frontal crossings between end points which were allowed to move with the mean flow. The results were combined with parallel measurements of the vertical profile of ε which were made using FLY for periods of up to 13 h at positions along the Autosub track. The two data sets, which show a satisfactory degree of consistency, were combined to elucidate the space–time variation of dissipation in the frontal zone. Using harmonic analysis, the spatial structure of dissipation was separated from the strong time dependent signal at the M4 tidal frequency to yield a picture of the cross-frontal distribution of energy dissipation. A complementary picture of the frontal velocity field was obtained from a moored ADCP and estimates of the mean velocity derived from the thermal wind using the observed density distribution. which indicated the presence of a strong (0.2 m s− 1) jet-like flow in the high gradient region of the front. Under neap tidal conditions, mean dissipation varied across the section by 3 orders of magnitude exceeding 10− 2 W m− 3 near the seabed in the mixed regime and decreasing to 10− 5 W m− 3. in the strongly stratified interior regime. The spatial pattern of dissipation is consistent in general form with the predictions of models of tidal mixing and does not reflect any strong influence by the frontal jet. 相似文献