单磁铁系统的稳定性与仿真分析

采用带状态观测器的气隙-速度-加速度反馈控制系统,在多体系统仿真软件SIMPACK平台上,考虑悬浮系统、电磁系统及控制系统的耦合作用,建立单磁铁-轨道梁-控制器的综合模型,模拟磁浮列车在弹性轨道梁上静止悬浮的过程,分析轨道梁的特征对车轨耦合振动的影响,研究共振的产生及解决方法,为磁悬浮列车的整车静止悬浮稳定性分析提供依据。     

高速公路路堤填土工程适宜性评价方法的探讨

路堤填筑是高速公路路基工程的一个重要环节，路堤填土工程适宜性研究尤为重要，基于高速公路路堤填土工程性质的分析，提出了填土工程适宜性评价的一种方法，分析了其可行性和难点，以广东西部沿海高速公路某试验段为例，进行了工程适宜性评价。这将对高速公路路基施工提供新的理论依据。     

上海外环线浦东段(二期)沥青面层技术要点

该文对上海城市外环线浦东段 (二期 )工程沥青面层技术做了简要的介绍 ,提出了施工过程中重点考虑的因素。     

揭阳市东山区沟口村民房墙体开裂问题研究

相邻建筑物在地基中产生的沉降总是相互影响,需要从新旧建筑物的强度、刚度、结构类型、地质情况、荷载大小等方面进行分析,从而提出对不同类型结构的处理方法。     

论海运提单的运输合同属性

通过提单的历史演变及有关立法及业务实际程序考察,论述提单的运输合同属性,更正有关立法的误会。     

计算机模拟在港口营运中的应用

介绍港口营运的计算机模拟。根据作者对计算机模拟在港口营运应用的经验,介绍港口模拟的步骤、港口模拟的应用范围,并给出一算例。     

无刷直流推进电动机动态性能的仿真

建立无刷直流推进电动机的动态仿真数学模型,利用系统矩阵的特征值和特征向量,以及对称性边界条件确定初始状态,对起动等动态过程进行了仿真和分析。仿真结果对于船舶永磁同步推进系统的设计具有重要的指导意义。     

新型码头钢-混凝土组合面板

基于特殊需要,提出了带型钢加劲肋的钢板-混凝土组合板这一新型组合码头面板。以加劲肋形式、组合板厚度和栓钉布置为参数,进行了9块组合板的力学性能试验。试验结果表明,通过适当地选择型钢加劲肋形式、合理地布置栓钉和确定混凝土厚度,可以保证组合作用的发挥。组合板的正截面承载力可按基于修正平截面假定的极限状态计算;组合板的变形,可在按现行钢结构设计规范计算的基础上,加上考虑界面滑移影响的附加变形值予以修正。计算值与试验值吻合较好。     

因地制宜,综合施治,务实解决街坊小区积水顽症

上海市杨浦区某些街坊小区一遇暴雨即产生严重的积水问题。通过调查研究，找出病症，提出改造方案．有效地解决了小区的积水顽症。本文结合实际，总结了若干综合技术措施和行政管理、协调手段。     

Distribution of suspended sediment in the coastal sea off the Ganges–Brahmaputra River mouth: observation from TM data

Remote sensing technique was applied to estimate suspended sediment concentration (SSC) and to understand transportation, distribution and deposition of suspended sediment in the estuary and throughout the coastal sea, off the Ganges–Brahmaputra River mouth. During low river discharge period, zone of turbidity maximum is inferred in the estuary near the shore. SSC map shows that maximum SSC reaches 1050 mg/l in this period. Magnitude of SSC is mainly owing to resuspension of the bottom surface sediments induced by tidal currents flowing over shallow water depths. The influence of depth on resuspension is farther revealed from the distribution and magnitude of SSC along the head of Swatch of No Ground (SNG) submarine canyon. During high river discharge period, huge river outflow pushed the salt wedge and flashes away the suspended sediments in the coastal sea off the river mouth. Zone of turbidity maximum is inferred in the coastal water approximately within 5–10 m depth of water, where the maximum SSC reaches 1700 mg/l. In this period, huge fluvial input of the suspended sediments including the resuspended bottom sediments and the particles remaining in suspension for longer period of time since their initial entry control mainly the magnitude of SSC. In the estuary near the shore, seasonal variation in the magnitude of SSC is not evident. In the coastal sea (>5 m water depth), seasonal influence in the magnitude of SSC could be concluded from the discrepancy between SSC values of two different seasons. Transportation and deposition of suspended sediments also experiences seasonal variations. At present, suspended sediments are being accumulated on the shallow shelf (between 5 and 10 m water depth) in low discharge period and on the mid-shelf (between 10 and 75 m water depth) during high discharge period. An empirical (exponential) relationship was found between gradual settle down of suspended sediments in the coastal sea and its lateral distance from the turbidity maximum.