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121.
M. Ziyaeifar 《Vehicle System Dynamics: International Journal of Vehicle Mechanics and Mobility》2005,43(11):771-794
The investigation of problems related to the interaction of train, bridge and track systems has been accelerated by the emergence of high-speed trains. Such studies are required, not only for the endurance issues regarding bridge and tracks, but to assure trains' functionality and performance. The suspension mechanism of train systems is of prime importance in defining the functionality of high-speed trains, and accurate mathematical models of the mechanism are imperative. This paper introduces a numerical technique for an interaction study of train-bridge-track systems based on Maxwell (three-element type) modeling of the suspension mechanisms of vehicles. Track irregularity in sinusoidal form is also integrated into the mathematical model. Although the proposed technique is simple in formulation, it offers phenomenal accuracy in representing the interaction of train, track and bridge systems. In a numerical example, the dynamic behavior of a train-bridge system has been studied. Results of this analysis provide a valuable insight into the contributing roles of different parameters in this subject. 相似文献
122.
减轻列车轮轨横向动力作用的技术措施 总被引:1,自引:0,他引:1
基于铁道车辆-轨道耦合动力学理论及仿真分析系统,分析了机车车辆悬挂参数、结构参数及轨道结构参数对轮轨横向相互作用的影响,在此基础上提出了降低轮轨横向动力作用的技术措施:(1)一系水平定位刚度(纵向和横向刚度)对轮轨横向动力作用影响较大,刚度值选取的基本设计原则是,在充分满足运动稳定性的前提下,尽可能降低刚度值;(2)二系水平(包括纵向和横向)刚度对轮轨横向动力作用影响不明显,设计时,应更多地考虑机车车辆的平稳性;(3)簧下质量对轮轨横向动力作用影响较大,较小簧下质量,将使轮轨横向动力作用得到显著的降低;(4)较低的扣件横向刚度、扣件垂向刚度及道床横向刚度等参数值将有利于降低轮轨横向动力作用。 相似文献
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Timed RAISE方法在列控系统等级转换场景中的应用研究 总被引:1,自引:1,他引:0
《铁道标准设计通讯》2015,(8):164-169
高速铁路列车运行控制系统是一个复杂的实时性系统,结合其实际特点,将域方法作为系统描述的切入。通过对模型检验和定理证明两种验证方法的分析比较,提出使用基于定理证明的时间化工业软件工程的严格方法Timed RAISE形式化方法对等级转换(CTCS-2级至CTCS-3级)场景进行描述,并对其场景交互一致性和实时性进行验证,结果表明该场景不会出现场景交互一致性错误,也不会违反时间的约束。 相似文献
125.
Igor P. Semiletov Irina I. Pipko Irina Repina Natalia E. Shakhova 《Journal of Marine Systems》2007,66(1-4):204
Climatic changes in the Northern Hemisphere have led to remarkable environmental changes in the Arctic Ocean, which is surrounded by permafrost. These changes include significant shrinking of sea-ice cover in summer, increased time between sea-ice break-up and freeze-up, and Arctic surface water freshening and warming associated with melting sea-ice, thawing permafrost, and increased runoff. These changes are commonly attributed to the greenhouse effect resulting from increased atmospheric carbon dioxide (CO2) concentration and other non-CO2 radiatively active gases (methane, nitrous oxide). The greenhouse effect should be most pronounced in the Arctic where the largest air CO2 concentrations and winter–summer variations in the world for a clean background environment were detected. However, the air–land–shelf interaction in the Arctic has a substantial impact on the composition of the overlying atmosphere; as the permafrost thaws, a significant amount of old terrestrial carbon becomes available for biogeochemical cycling and oxidation to CO2. The Arctic Ocean's role in determining regional CO2 balance has been ignored, because of its small size (only 4% of the world ocean area) and because its continuous sea-ice cover is considered to impede gaseous exchange with the atmosphere so efficiently that no global climate models include CO2 exchange over sea-ice. In this paper we show that: (1) the Arctic shelf seas (the Laptev and East-Siberian seas) may become a strong source of atmospheric CO2 because of oxidation of bio-available eroded terrestrial carbon and river transport; (2) the Chukchi Sea shelf exhibits the strong uptake of atmospheric CO2; (3) the sea-ice melt ponds and open brine channels form an important spring/summer air CO2 sink that also must be included in any Arctic regional CO2 budget. Both the direction and amount of CO2 transfer between air and sea during open water season may be different from transfer during freezing and thawing, or during winter when CO2 accumulates beneath Arctic sea-ice; (4) direct measurements beneath the sea ice gave two initial results. First, a drastic pCO2 decrease from 410 μatm to 288 μatm, which was recorded in February–March beneath the fast ice near Barrow using the SAMI-CO2 sensor, may reflect increased photosynthetic activity beneath sea-ice just after polar sunrise. Second, new measurements made in summer 2005 beneath the sea ice in the Central Basin show relatively high values of pCO2 ranging between 425 μatm and 475 μatm, values, which are larger than the mean atmospheric value in the Arctic in summertime. The sources of those high values are supposed to be: high rates of bacterial respiration, import of the Upper Halocline Water (UHW) from the Chukchi Sea (CS) where values of pCO2 range between 400 and 600 μatm, a contribution from the Lena river plume, or any combination of these sources. 相似文献
126.
《Vehicle System Dynamics: International Journal of Vehicle Mechanics and Mobility》2012,50(11):1667-1685
A two-dimensional computational model for assessment of rolling contact fatigue induced by discrete rail surface irregularities, especially in the context of so-called squats, is presented. Dynamic excitation in a wide frequency range is considered in computationally efficient time-domain simulations of high-frequency dynamic vehicle–track interaction accounting for transient non-Hertzian wheel–rail contact. Results from dynamic simulations are mapped onto a finite element model to resolve the cyclic, elastoplastic stress response in the rail. Ratcheting under multiple wheel passages is quantified. In addition, low cycle fatigue impact is quantified using the Jiang–Sehitoglu fatigue parameter. The functionality of the model is demonstrated by numerical examples. 相似文献
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采用势流理论计算限制水域船舶水动力相互作用力(英文) 总被引:1,自引:0,他引:1
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