空间复合材料加筋板流固耦合振动分析

本文用结构有限元与流体边界元方法研究了空间复合材料加筋板结构的流固耦合自由振动，推导了用于结构分析的分项插值型复合材料八节点板单元和三节点梁单元，以及用于流场分析的线性边界单元。用修正的RIRZ向量法与波前法相结合的方法求解特征值问题，避免了因附连水质量引起的结构质量矩阵为满阵的内存困难和非对称矩阵方程约化困难。算例表明，附连水质量对复合材料结构的动力特性影响要比各向同性材料严重得多。     

跨座式单轨平移式道岔结构数值仿真分析

根据相关规范给出平移式道岔结构在列车作用下的动力荷载类型及相应计算方法。为减少计算单元的划分数量、提高计算分析效率,提出单元重分法模拟列车移动加载。运用有限元数值仿真方法,对平移式道岔在列车运行过程中的力学行为和结构安全性进行分析。结果表明:列车运行过程中平移式道岔结构在长台车处产生最大应力,其应力比为0.86,梁体挠度小于规范规定的相应限值,说明在列车运行过程中平移式道岔的强度和刚度均能够满足结构安全性要求;长台车上部连接板的边缘处存在较大的集中应力,因此在道岔结构制造和施工过程中,需确保其焊缝连接强度不小于母材强度。     

列控车载设备随机振动仿真分析

利用有限元分析软件ABAQUS对某一列控车载设备的结构进行了动力学仿真分析,首先提取了列控车载设备的模态,并在此基础上进行了基于ASD(Acceleration Spectral Density)的随机振动分析,最后给出结构上的改进方案。通过研究发现,将CAE与产品结构设计相结合,可以提前预测产品的环境适应性、发现设计风险并提出改进方案,因此仿真分析可以缩短产品的开发周期、降低开发成本。     

轿车前梁有限元分析

利用轿车前梁的CATIA模型建立其有限元模型。通过前悬架的ADAMS模型确定前梁的受力。应用这些方法将CAD、CAE有机的结合在一起，提高了有限元分析的效率和准确性。为了检验模型的精确程度，对前梁进行了静态加载试验。结果表明计算和试验结果有很好的一致性。     

半刚性基层与沥青层之间界面条件对结构性能的影响

利用弹性层状体系理论计算了在不同层间条件下的半刚性沥青路面沥青层中的剪应力、拉应力分布情况及路表弯沉值,分析了基层与沥青层之间由于层间界面条件变化引起的路面结构受力状态的变化。计算表明基层与面层保持连续的界面条件是十分重要的;过分致密不透水的半刚性基层有可能造成路面的早期损坏。     

下沉短桩越顶问题的有限元分析

下埋短桩是一种介于抗滑键与全长桩的一种特殊的抗滑桩,在合适的位置上采用将桩顶下沉设置较短的桩就可使边坡达到设计要求的安全系数,而桩身内力较全长桩有所降低,因此从经济角度与受力方面来看,具有良好的应用前景,但是滑体有可能沿桩顶失稳剪出,导致边坡工程失败,在应用上受到了很大的制约.现以云阳县太公沱至余家包库岸大咀段库岸滑坡工程为例,对用下埋短桩治理后是否越过抗滑短桩桩顶问题,采用了有限元强度折减法验证.     

锚固体的布设位置与形态对固坡效果的影响

为揭示灌浆锚固体对固坡效果的影响规律,利用有限元强度折减法,计算了单根锚固体分别在垂直或水平布设于坡体不同位置条件下以及布设角度不同等条件下锚固体的变形和边坡的稳定系数。分析表明:在坡体中置入锚固体对边坡的稳定性均有不同程度的提高,其中垂直布设较水平布设的固坡效果更为显著;布设位置在坡高约1/3处最为理想;锚固体与坡面夹角也对固坡效果有较大的影响。     

基于规范方法的小水线面双体船疲劳强度研究

论文介绍了船舶结构疲劳强度评估基本原理,并对一条2200t级小水线面双体船进行规范法疲劳强度评估。针对小水线面双体船结构特点,采用规范进行疲劳载荷计算;结合全船有限元计算结果进行疲劳部位筛选;采用有限元法提取疲劳部位的热点应力,并计算疲劳部位的累积损伤度。分析计算结果,提出疲劳部位优化方案。     

Impact of macrozoobenthic structures on near-bed sediment fluxes

Sandy sediments in shallow coastal waters of the Baltic Sea are often characterised by large numbers of biogenic structures which are produced by macrozoobenthos species. A series of experiments was devised to quantify how the interaction of such structures with the near-bed flow regime affects the sediment flux. Most experiments were done with simplified replicates of structures generated by typical species commonly found in the Mecklenburg Bight, starting with solitary structures and regularly-spaced arrays in a range of characteristic population densities, followed by a complex benthic macrofauna community, both artificial and alive. A laboratory flume channel, equipped with an acoustic Doppler flow sensor and a topography scanning laser, was used for high-resolution measurements (2 mm horizontal step size and 0.3 mm vertical resolution) of sand erosion (220 µm median grain size, at 20 cm s^− 1) and fine particle deposition (8 µm grain size, at 5 cm s^− 1). Sediment transport threshold values were measured for each layout. As a rule-of-thumb, both the erosion fluxes and the deposition of suspended matter increased considerably at low population densities (below 2%, expressed as percent of the sediment surface covered, i.e. roughness density RD). Above densities of 4%, erosion almost stopped inside the test arrays, and deposition remained well below the level of unpopulated areas. An attempt to extrapolate these findings to field conditions (using field current velocity data from 2001) showed that the net flux switched from erosion to deposition for densities above 5%. These parameters can now be integrated into a numerical sediment transport model coupling waves, currents, sediment dynamics and biological processes, which is currently under construction at the Baltic Sea Research Institute (IOW), Rostock, Germany.     

Characteristic flow patterns generated by macrozoobenthic structures

A laboratory flume channel, equipped with an acoustic Doppler flow sensor and a bottom scanning laser, was used for detailed, non-intrusive flow measurements (at 2 cm s^− 1 and 10 cm s^− 1) around solitary biogenic structures, combined with high-resolution mapping of the structure shape and position. The structures were replicates of typical macrozoobenthic species commonly found in the Mecklenburg Bight and with a presumed influence on both, the near-bed current regime and sediment transport dynamics: a worm tube, a snail shell, a mussel, a sand mound, a pit, and a cross-stream track furrow. The flow was considerably altered locally by the different protruding structures (worm tube, snail, mussel and mound). They reduced the horizontal approach velocity by 72% to 79% in the wake zone at about 1–2 cm height, and the flow was deflected around the structures with vertical and lateral velocities of up to 10% and 20% of the free-stream velocity respectively in a region adjacent to the structures. The resulting flow separation (at flow Reynolds number of about 4000 and 20,000 respectively) divided an outer deflection region from an inner region with characteristic vortices and the wake region. All protruding structures showed this general pattern, but also produced individual characteristics. Conversely, the depressions (track and pit) only had a weak influence on the local boundary layer flow, combined with a considerable flow reduction within their cavities (between 29% and 53% of the free-stream velocity). A longitudinal vortex formed, below which a stagnant space was found. The average height affected by the structure-related mass flow rate deficit for the two velocities was 1.6 cm and 1.3 cm respectively (80% of height and 64%) for the protruding structures and 0.6 cm and 0.9 cm (90% and 127% of depth) for the depressions. Marine benthic soft-bottom macrozoobenthos species are expected to benefit from the flow modifications they induce, particularly in terms of food particle capture due to altered particle pathways and residence times, but also for the exchange of gases, solutes and spawn. The present results confirm previous studies on flow interaction effects of various biogenic structures, and they add a deeper level of detail for a better understanding of the fine-scale effects.