渤海波浪地理信息系统的建立

随着地理信息系统(GIS)的广泛应用,建立一个具有波浪预报或后报功能的信息系统为工程建设服务,不仅十分必要,而且随着波浪模拟技术的发展变得可能。文中论述了采用第三代波浪模型中的SWAN(SimulatingWAves Nearshore)来模拟渤海波浪场,在获得较长时间波浪模拟结果的基础上,对渤海波浪地理信息系统的建立进行了一些尝试和探索。这些波浪资料对于港口及海洋工程是十分必要的。     

船舶压载舱的牺牲阳极保护

论述了船舶压载舱产生腐蚀的原因、防腐蚀保护的方法。介绍了中国船级社有关牺牲阳极阴极保护的原则规定、设计要求、安装要求、定期检查项目。最后,将腐蚀的舱壁采用涂装或牺牲阳极阴极保护两种方法进行了经济效益对比分析,得出安装牺牲阳极阴极保护的经济效益显著的结论。     

提速干线编组站出发子系统内部匹配与协调关系

分析提速干线编组站货物列车到发时刻不均衡运营特征,根据编组站作业特点和要求,运用排队论和随机过程理论,对出发子系统转场和接车可靠性、临界密集出发时间进行计算分析。认为出发子系统允许的接车延误概率应控制在0.12以内;当区间通过能力利用率在繁忙时间达0.85以上时,出发场的到发线应在10股以上。提高出发子系统转场和接车可靠性的措施包括:提高无调比、适当增加出发场到发线数量、降低编组调车机车的作业负荷、减小出发时间间隔不均衡系数。给出一定出发强度下的临界密集发车时间计算式,便于指导运输组织工作。改善出发子系统匹配与协调关系的有效途径包括:合理配置列检组数、转线接车延误率控制在10%以内、密集到发期间区段通过能力利用率不能超过90%、降低衔接区间发车时间间隔变异系数、连续高密集发车时间不能超过临界发车时间、适当增加分类线及到发线数量、优化列车运行计划、平衡双向系统作业负荷、加强管理、优化运输组织。     

不等高接触悬挂在同一组软横跨上的处理方案

针对株洲客车站北咽喉第5次提速改造和兼顾浙赣线引入线接触线高度6450mm改造的特殊要求,通过分析比较不等高接触悬挂在软横跨上的处理模式,提出经济合理、高效便捷的处理方案,为今后此类施工提供借鉴。     

A high order linear model for the prediction of internal lee waves at the main sill of the Strait of Gibraltar

A linear theory for the physical fields in the water column under the action of large amplitude internal lee waves at the main sill of the Strait of Gibraltar is developed. The procedure is a combination of the perturbation and normal modes methods in order to study steady resonant conditions. The lowest order linear approach of the methodology resumes the Taylor–Goldstein equation, which can reconstruct the main features of the observed fields but the high order approach gives the finest structure and sometimes the largest contributions. The role of the non-linear terms is investigated up to the second order taking into account the non-linear interactions between modes, leading to an effective reconstruction of the whole water column for the velocity field.     

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。     

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。     

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。     

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.