装车地直达列车开行方案优化模型

铁路货物运输在国民经济增长和发展过程中起着越来越重要的作用，而装车地直达运输是一种现代和高效的车流组织形式。它不但能够加快货物送达、加速车辆周转，而且可以减轻编组站作业负担、降低运输成本。本文对装车地直达列车开行方案问题进行了研究。在分析组织装车地直达列车的可能性、合理性及费用参数选择的基础上，构建了装车地直达列车开行方案非线性0-1规划模型。模型中充分考虑了车流在装车地的各种组合方案，并将运输与库存成本纳入同一目标函数，以物流系统成本最优来确定货物列车开行方案。构建的模型能够更全面地描述装车地车流的各种组合，最后给出的构模实例对模型的有效性、合理性进行了验证。     

轴箱轴承轴向自由间隙对机车动力学影响分析

对于速度200 km/h的C0-C0轴式高速机车,轴箱轴承轴向自由间隙对机车高速运行时横向动力学性能的影响较大。本文采用SIMPACK动力学软件,建立了牵引电机架悬的C0-C0轴式高速机车计算模型,就轴箱轴承轴向自由间隙对机车运行稳定性、横向动力学性能和曲线通过性能的影响进行了较为深入的研究。研究表明,合理设置轴箱的端轴和中间轴轴承的轴向自由间隙,可以提高机车稳定性、改善机车直线以及曲线运行品质。较大的中间轴轴向自由间隙和较小的端轴轴向自由间隙对提高机车运行稳定性有利。对于速度200 km/h的C0-C0轴式高速机车,端轴和中间轴的轴向间隙分别取0.5~1 mm和5~8 mm较为合适。     

B_0-B_0-B_0抱轴式机车黏着利用率分析

就B0-B0-B0轴悬式机车二系簧分布,车轮踏面磨耗,车钩高度,一、二系垂向刚度,端、中转向架牵引点高度,电机吊挂点到车轴中心的距离,转向架中心距,轴距等对机车黏着利用率的影响进行分析。研究结果和建议可供设计部门制订技术方案时参考。     

Analysis of the contribution of ice algae to the ice-covered ecosystem in Lake Saroma by means of a coupled ice–ocean ecosystem model

A new coupled ice–ocean ecosystem model that links the pelagic and ice ecosystems was used to clarify the role of ice algae in ice-covered ocean ecosystems. The model was applied to Lake Saroma (Hokkaido, Japan) in 1992. Comparison of the model's results with observational data confirmed that the model reproduced the behavior of the ecosystem with acceptable accuracy during the period from winter to spring. The primary production of the ice algae is effectively transported into the pelagic system by means of physical releasing effects: brine convection, ice melting and freezing, and diffusion generated at the bottom of the ice. Ice algae released from the ice are rapidly exported because of their high sinking speed and the shallow depth of Lake Saroma. For this reason, the zooplankton in Lake Saroma cannot graze these released algae. However, zooplankton actively graze the ice algae living along the bottom of the ice. These results show that, before their release, ice algae play an important role as a food source for overwintering zooplankton. A sensitivity analysis revealed a positive correlation between the sinking speed of the released ice algae and the magnitude of the spring bloom by pelagic phytoplankton, and that the time when secondary production becomes active is an important factor in the linkage between these two algal populations.     

超大吨位悬浇梁0#块施工技术

通过南宁葫芦鼎大桥工程实例,详细介绍了3400t 0#块钢管桩支撑方法、大块钢模板施工及长联钢构的C60混凝土施工技术,总结了0#块施工的新工艺。     

WnSi^0,±（n=1～5）团簇结构和稳定性的密度泛函理论研究

用密度泛函理论（Density Functional Theory,DFT）中的B3LYP／lanl2dz方法,优化并得到了WnSi^0,±（n=1～5）团簇的各种稳定构型,并对基态构型的能量进行了系统的理论分析．结果表明：WnSi^0,±团簇基态结构与Wn＋1团簇的生长模式相似,除W3Si＋团簇与W5Si^-团簇外,阳离子与阴离子团簇的稳定结构基本上保持了对应中性团簇的稳定结构;WSi团簇相对于其他团簇更易得到电子变成负离子,W5Si团簇较易失去电子变成阳离子;W3Si团簇具有较弱的化学活性,W5Si-团簇具有较强的化学活性．     

0号块波形钢腹板安装工艺流程控制

波形钢腹板组合桥梁相比于传统桥梁具有自重轻、防止腹板开裂、力学性能好等许多优点,得到越来越多青睐,然而,国内波形钢腹板的安装工法还不够完善。现提出一种新型波形钢腹板安装工艺,对国内波形钢腹板组合箱梁悬浇施工0号块波形板安装控制方法进行论述。其中,对安装过程中的关键控制点及其方法做了详细细说明和分析,能极大地改善工法和提高施工效率。     

多波束宽带恒定束宽波束形成器的DSP实现

波束形成是声纳、雷达信号处理中的重要环节。由于高性能的宽带波束形成算法运算量大交难以实时实现,因此开发研制高速度、高精度、高性能的波束形成器、就很必要。文章提出采用ＴＭＳ３２０Ｆ２０６及ＩＭＳＡ１００为主要芯片,构成多波束宽恒定束宽波束形成器,可实现实时、高速、高性能的多波束宽带恒定束宽波束形成,并给出了具体设计方案。水池实验结果,表明本文的系统设计方案正确、可靠。     

一种新的模糊逻辑代数系统

基于对模糊逻辑和模糊推理的系统研究,一种新的模糊逻辑代数－Ｒ０代数已于近期被建立,这为模糊逻辑提供了一种新的代数框架。文中对Ｒ０代数作进一步研究,给出Ｒ０代数的一系列代数性质,并澄清Ｒ０代数与其它模糊逻辑代数系统之间的关系。     

Formation of Denmark Strait overflow water and its hydro-chemical composition

The dense overflow across the Denmark Strait is investigated with hydrographic and hydro-chemical data and the water mass composition of the Denmark Strait Overflow Water (DSOW) is determined by multivariate analysis. Hydrographical properties, the transient tracers CFC-11 and CFC-12, oxygen and nutrients are utilized for the water mass definitions. Distribution and characteristics of water masses north of Denmark Strait are described, the important water masses at the sill and the variability on weekly time-scales are discussed, and the entrainment and mixing of water into the overflow plume in the northern Irminger Basin is calculated. The analysis indicates that water masses both from the Nordic Seas and the Arctic Ocean are important for the formation of DSOW. It is found that water masses transported with the East Greenland Current make up about 75% of the overflow at the sill. The overflow at, and shortly south of, the sill is inhomogeneous with a low-salinity component dominated by Polar Intermediate Water. The high-salinity component of the overflow is mainly of Arctic origin. The water mass composition, and the short-term variability for 7 repeats of sections close to the sill are described, and these illustrate that the overflow is in fact a composite of a number of water masses with different formation and transport histories. This indicate that the overflow is a robust feature, but that it responds to variations in the circulation or atmospheric forcing that influences the formation of intermediate and deep water masses within the Arctic Mediterranean and the North Atlantic. At a section about 400 km south of the sill the overflow is well mixed and modified by entrainment of, mainly, Iceland–Scotland Overflow Water and Labrador Sea Water, together constituting 30% of the overflow plume. The entrainment of Middle Irminger Water dominates shortly downstream of the sill, before the overflow plume reaches too deep but the entrainment seems to be intermittent in time.