浮筏隔振装置的超单元建模方法

浮筏是一种集弹簧、阻尼器、刚体和弹性体为一体的混合动力学系统，对其建立合适的动力学模型存在困难，为此本文提出一种超单元建模方法。该方法首先在物理空间中对装置中弹性体的有限元模型进行降阶，并建立相应的超单元，然后与普通单元一样把它们直接组装到总体模型中。用该方法建立起来的动力学降价模型不仅在规模上远小于未降阶的有限元模型，而且能很好地保留原模型在中、低频段内的动态特性。数值示例表明，本文提出的超单元建模方法是一种有效的浮筏隔振装置建模方法。     

长冲隧道进口段开挖方法的优化分析

根据隧址区工程地质特征,建立了长冲隧道进口段的有限元模型;模拟了台阶分部法和CD工法开挖隧道的过程,通过对围岩的位移和应力特征、屈服接近度和支护结构受力特征的分析,从施工工序和施工力学角度对两种开挖方法进行了比较,结果表明设计推荐采用的CD工法较台阶分部法没有明显的优势。     

基于遗传算法优化的小波神经网络对船舶受扰力及力矩建模预报

首先构造小波神经网络,建立船舶横向和纵向运动模型及其运动受扰力模型,采用小波神经网络对船舶受扰力建模预报,并用遗传算法对其进行优化,对预报结果进行分析比较,给出超前5秒、15秒的船舶运动受扰力与力矩预报结果.     

基于山区复杂路段下的车辆主动限速控制系统研究

山区复杂路段交通事故频发,行车安全问题亟待解决,因此研究该路段下的主动限速控制技术具有重要意义。本文阐述了主动限速控制系统的原理与构成,并且对车辆的运行安全车速进行了分析与建模,提出了主动限速的控制策略。最后通过对该系统软硬件进行了调试,初步验证了其可行性比较合理,能够指导驾驶人的行车安全。     

TBM刀盘的有限元参数化建模系统开发

针对设计和研究人员快速构建TBM刀盘有限元模型的需求,采用APDL与VC++可视化编程技术相结合的方法,在编制刀盘建模APDL程序的基础上,开发友好的人机交互界面,实现了VC++与ANSYS之间的参数传递,建立了一套可视性良好的TBM刀盘有限元参数化建模系统。以某型号直径4 m TBM刀盘为例构建有限元模型,验证了该系统良好的实用性和可靠性。通过对此建模系统的开发,可实现TBM刀盘数字化建模、分析等全套设计。     

基于特征的高速列车铝合金车体断面参数化建模

针对高速列车铝合金车体断面结构复杂、设计周期长和建模效率低等特点,提出了一种基于特征的高速列车铝合金车体断面参数的建模方法.引入特征概念,定义车体断面型材的特征及其拓扑关系,采用CATIA系统中CAA二次开发技术,对车体断面的轮廓和车体断面型材的特征进行参数化建模,建立车体断面型材的特征库,通过车体断面的骨架进行自动装配设计;最后以某型车铝合金车体断面参数化建模为例验证该方法的正确性和有效性.     

可编程压电式电气比例阀的建模与实验研究

提出了一种可编程压电式电气比例阀方案,构建了系统的动态非线性数学模型,从而对其时域和频域特性进行了仿真分析。通过系统一系列实验得出实验曲线与仿真曲线基本吻合,从而证明了仿真模型的正确性,该结论为压电式电气比例阀的进一步研究奠定了实验基础。     

用一个模型分析焊轨列车应用的条件

通过对秦皇岛 -沈阳客运专线 B2 7标段情况的分析得出铺轨基地存轨场地的面积是制约焊轨列车应用的一个重要因素。以预存长钢轨的数量为主要参数 ,利用焊轨列车在两个基地间工作的时间约束关系 ,建立起相应的模型 ,通过对其中其它参数的分析 ,得出应用焊轨列车所适宜的条件。在此基础上结合一次铺设跨区间无缝线路的工艺分析了焊轨工序与铺轨、大型机械养路工序的关系 ,提出了设备配套的建议和施工中应注意的一些问题。本文对设备选型、施工组织的编制及新工艺的采用有一定借鉴意义。     

Using a random displacement model to simulate turbulent particle motion in a baroclinic frontal zone: A new implementation scheme and model performance tests

Numerical artifacts can limit accurate simulation of turbulent particle motion when Lagrangian particle-tracking models are implemented in hydrodynamic models with stratified conditions like fronts. Yet, modeling of individual particle motion in frontal regions is critical for understanding sediment dynamics as well as the transport and retention of planktonic organisms. The objective of this research was to develop a numerical technique to accurately simulate turbulent particle motions in a particle-tracking model embedded within a hydrodynamic model of a frontal zone. A new interpolation scheme, the ‘water column profile’ scheme, was developed and used to implement a random displacement model for turbulent particle motions. A new interpolation scheme was necessary because linear interpolation schemes caused artificial aggregation of particles where abrupt changes in vertical diffusivity occurred. The new ‘water column profile’ scheme was used to fit a continuous function (a tension spline) to a smoothed profile of vertical diffusivities at the x–y particle location. The new implementation scheme was checked for artifacts and compared with a standard random walk model using (1) Well Mixed Condition tests, and (2) dye-release experiments. The Well Mixed Condition tests confirmed that the use of the ‘water column profile’ interpolation scheme for implementing the random displacement model significantly reduced numerical artifacts. In dye-release experiments, high concentrations of Eulerian tracer and Lagrangian particles were released at the same location up-estuary of the salt front and tracked for 4 days. After small differences in initial dispersal rates, tracer and particle distributions remained highly correlated (r = 0.84 to 0.99) when a random displacement model was implemented in the particle-tracking model. In contrast, correlation coefficients were substantially lower (r = 0.07 to 0.58) when a random walk model was implemented. In general, model performance tests indicated that the ‘water column interpolation’ scheme was an effective technique for implementing a random displacement model within a hydrodynamic model, and both could be used to accurately simulate diffusion in a highly baroclinic frontal region. The new implementation scheme has the potential to be a useful tool for investigating the influence of hydrodynamic variability on the transport of sediment particles and planktonic organisms in frontal zones.