波浪作用下粉沙质底沙运动特性的试验研究

本文利用山东潍坊现场沙(d_(50)≈0.0813mm),通过水槽试验研究了波浪作用下粉沙质底沙的运动特性、床面形态、起动特点及输沙规律等,为分析研究粉沙质海岸的泥沙问题提供了基本数据和研究方法.     

国内外合成闸瓦力学性能和摩擦性能的研究

利用材料试验机、冲击试验仪、制动动力试验台等检测仪器设备,对国内外合成闸瓦的力学性能和摩擦磨损性能等进行了综合测试和分析。结果表明,国外合成闸瓦的冲击强度高,压缩强度和压缩模量低,摩擦因数低于我国闸瓦,磨耗量较小。因此,国外合成闸瓦具有良好的使用性能和较长的使用寿命。     

关于ND算法的几点讨论

本文对《基于二阶导数的优化算法》一文中提出的ND算法的收敛性等问题进行了讨论。从理论上证明了：当步长充分小时，ND算法较梯度法收敛速度快。计算机计算结果也证实了ND算法有较快的收敛速度。     

一个改进的二次规划型算法

建立非线性等式和不等式约束规划问题的一个序列二次规划(SQP)型算法.算法的每次迭代只需解一个确实可解的二次规划,然后对其解进行简单的显式校正,便可产生关于罚函数是下降的搜索方向,克服Maratos效应.在适当的假设条件下,还论证了算法的全局收敛性和超线性收敛性.     

铁路货物运输市场价格优化模型研究

常用的定价方法主要是成本定价法、投资回报率法以及目标利润率方法等,但这些方法在使用时不易掌握,不能分析各类市场因素对价格水平的影响以及影响程度。为了能够在定价中综合考虑市场因素,根据优化理论建立了铁路货物运输市场价格模型,模型中以收入与支出的差额最大化为优化目标,以运输价格水平与货物的市场价格水平之间保持一定的比例为约束,其结果描述了各种因素与价格之间的关系,由此可以分析影响运价的价格弹性、各种运输方式的市场份额等主要因素的作用和影响,并通过具体示例进行了价格测算。     

U71 Mn 50 kg·m-1普通碳素钢钢轨疲劳裂纹扩展速率试验研究

根据室内对U71Mn50kg·m-1普通碳素钢钢轨按三点弯曲标准进行的试验,测定该钢轨的疲劳裂纹扩展速率,即裂纹扩展深度a及其对应的循环次数N值。利用中值法求得裂纹扩展深度对循环次数的微分值。根据断裂理论求得相应的裂纹前沿应力强度因子幅度ΔK。根据Paris公式,对以上两值取自然对数进行线性回归分析,确定该公式中U71Mn50kg·m-1普通碳素钢钢轨疲劳裂纹扩展速率的两个材料常数C为3 8771×10-12,m为3 6343。     

基于空隙模型的大空隙沥青混合料设计

空隙率的大小对大空隙沥青混合料的渗透性及力学性能具有很大影响,透水铺面应根据用途选择合适的空隙率,在一定的水头（降雨强度）下利用空隙模型确定的目标空隙率进行混合料配合比设计．结果表明,空隙模型确定的目标空隙率可为混合料的配合比设计提供理论指导,提高了传统设计方法的工作效率和准确性．     

回填土区深层搅拌桩和高压旋喷桩复合地基的静承载性能

结合实际工程现场静载试验,采用有限元计算方法研究了桩长和桩土模量比对深层搅拌桩和高压旋喷桩复合地基在回填土中的桩体承载特性、荷载传递及复合地基变形特性的影响。结果表明,在回填土区,深层搅拌桩以桩体上部破坏为主,增加桩长不能有效地提高复合地基承载力,增加桩体强度尤其是上部桩体的强度则能够较大地提高复合地基承载力,高压旋喷桩可有效增强回填土地基的承载力。提出的桩体弹性模量取值范围可供设计参考。     

关于码头超能力靠泊问题的分析

文中通过对我国沿海港口建设和生产发展状况进行分析，指出了产生码头超能力靠泊的原因，并深入讨论了码头超能力靠泊的危害，最后，从提高码头生产效率、遵守限定条件靠泊核准的新船型等方面提出了解决码头超能力靠泊的方法。     

Biologically induced differences in erodibility and aggregation of subtidal and intertidal sediments: a possible cause for seasonal changes in sediment deposition

This study was carried out to describe the difference in erodibility and aggregation in a tidal basin including both subtidal and intertidal study sites and to use these results to explain the shifting erosion/deposition cycles at the sites. Erosion thresholds, erosion rates and settling velocities of the eroded material were measured at a mudflat transect and at sediment cores taken from a nearby tidal channel during surveys made in May 2000 and March 2002. Surface samples were analysed for grain-size, chl. a content, faecal pellet content, dry bulk density and organic content. Additionally, surface samples were taken at eight occasions in the period January 2002 to May 2003 from shallow tidal channels in the area. These samples were analysed for mud content and showed that major shifts in sediment distribution occurred in the period. The erodibility of the mudflat was generally high due to pelletization by the mudsnail Hydrobia ulvae but close to the salt marsh much lower erodibility was found, probably due to stabilisation by microphytobenthos. In contrast, the erodibility of the channel bed seemed to be very little influenced by biological activity and the relatively low erodibility found here was caused by physical characteristics of the sediment. The sediment eroded from the mudflat was generally strongly pelletized and showed high settling velocities whereas less aggregation and lower settling velocities were found for the channel bed sediments. Temporal variations of the mudflat stability and hydrodynamics resulted in temporal variations of deposition and erosion and the changing stability at the mudflat is likely to be one of the main reasons for a general transport of fine-grained sediment from the mudflat to the channel in the cold seasons and vice versa during the rest of the year.