上海世博会公共客运系统设计

世博参观游客交通的合理组织是办好世博会的关键问题之一。在总结上海世博会交通条件的基础上,提出以公共交通为核心的世博会客流集散策略,并采用由整体到局部系统化分析的方法,进行了世博公共交通系统的总体设计。基于世博游客集散的三条对策,以提高公共交通系统吸引力为目标,建立了世博公共交通系统的总体框架;接着就世博公共交通系统两个主要子系统“交通转换系统”和“EXPOBUS系统”,进行了系统的功能分析、服务流程分解和服务对象分类;最后梳理了系统设施需求,提出了各子系统的系统设计与规划方案。通过研究,期望能建立高效的、具有吸引力的公共交通系统,保障上海世博会的成功举办。     

水翼参数对水翼复合小水线面双体船纵向运动性能的影响

以静排水量为400 t的水翼复合小水线面双体船HYSWATH为研究对象,对其纵向运动性能进行数值模拟,将理论计算结果与模型试验结果进行对比分析,验证CFD理论计算方法的可靠性。并且以此为基础,研究水翼参数变化对HYSWATH纵向运动性能的影响,为后续该类船舶的设计提供理论参考。     

深海拖曳系统自稳定二级拖体姿态控制研究

二级深拖系统具有可控性强、母船扰动弱等优点,是重要的海洋探测平台。在实际工作中,二级拖体姿态稳定是保证探测数据准确的基本前提。本文以具有自主调节功能的二级拖体为例,对其姿态控制进行研究。首先建立了二级拖缆的“弹簧——阻尼”模型,并在此基础上建立了二级深拖系统的数学模型。其次根据该系统具有非线性、时变性等特点,设计了具有参数自修正功能的模糊自适应PID控制器,以实现在不同工况下对二级拖体的姿态进行控制。仿真结果表明,未加载控制器时,海况变化对拖体姿态有显著影响,其俯仰角和横滚角均会发生大范围波动。加载模糊自适应PID控制器后,拖体通过自主调节,能够使姿态波动控制在较小范围,从而满足工作要求,验证了拖缆数学模型的正确性和所采用的控制方法的可行性。     

拖曳式试验系统拖缆平台振动测试与分析

工程应用中,拖曳式试验系统拖缆平台存在明显的振动现象,振动产生的辐射噪声会对环境声场产生影响.基于拖缆平台的结构及运行原理,分析其内部的主要激励源,并进行现场振动测试.测试试验对平台支柱、绞车系统和隔振装置的振动信号进行了测量和分析,结果表明,平台支柱存在一定程度的振动,绞车机架振动主要由传动装置激励产生,隔振螺栓隔振效果不佳.测试数据及结果可为系统在工程应用中的优化设计和振动控制提供参考.     

船舶机舱空气质量监测评价仪的设计及实现

机舱多模式空气质量监测评价仪是对机舱气体进行实时监测并做出评价的智能化产品.本仪器通过多种传感器对机舱气体中部分物质的含量进行采集,利用单片机进行数据整理和分析,实时给出评价.该仪器对于监测机舱环境的空气品质,为轮机人员提供自我防护决策提供了依据和保障,有较大的意义和实用价值.     

基于CFD的船舶货舱通风数值模拟

以某集装箱船的货舱通风系统为研究对象,根据船舶舱室的通风系统的特点,采用合理的数值模拟方法,并利用拉格朗日粒子示踪的方法描述舱室中的气体流动状况.在此基础上,分析比较3种不同的通风设计方案,通过对比分析研究送风管上开孔朝向和数目对通风效果的影响,确定对通风最有利的方案.模拟结果表明,应用CFD技术进行通风系统分析,可以很好地从流场的分布特性以及空气粒子的运动追踪等方面来评估设计方案的优劣,为通风系统的设计、优化提供有力的工具.     

基于负荷敏感技术的调距桨控制系统设计

探讨调距桨控制问题,提出了基于负荷敏感技术的调距桨控制系统设计方法,设计了积分分离式PID控制算法．应用结果表明,积分分离式PID控制算法用于负载敏感技术的调距桨回路控制是有效的．     

基于功能损伤的复杂电磁环境下炮兵目标毁伤评估

为适应复杂电磁环境,提高炮兵指挥员“科学决策,量敌用兵”的水平,依据目标在复杂电磁环境下的特点,综合利用了指数法和D-S理论等方法,分别对典型目标、电磁敏感目标和系统目标进行了功能损伤性毁伤评估。     

高速航行体的自然超空泡流阻力特性研究

利用Fluent6.2对水下带圆盘空化器高速航行体的自然超空泡流动进行了数值模拟,计算分析了超空泡高速航行体的阻力特性,研究了空化器直径、航行体长细比对航行体超空泡减阻效果的影响,分析了高速航行体的超空泡减阻率。结果表明,超空泡形态下随着航行体速度衰减,航行体压差阻力系数缓慢减小,粘性阻力系数迅速增大,航行体的总阻力系数增加;航行体阻力系数与头部空化器直径的平方成反比;增加航行体的长细比,可以获得更小的阻力系数;高速航行体的超空泡减阻率可达95%以上。最后将仿真计算结果与水靶道试验进行了对比,二者基本相符。     

Seasonal and interannual variation of physical and biological processes during 1994–2001 in the Sea of Japan/East Sea: A three-dimensional physical–biogeochemical modeling study

A Pacific basin-wide physical–biogeochemical model has been used to investigate the seasonal and interannual variation of physical and biological fields with analyses focusing on the Sea of Japan/East Sea (JES). The physical model is based on the Regional Ocean Model System (ROMS), and the biogeochemical model is based on the Carbon, Si(OH)₄, Nitrogen Ecosystem (CoSiNE) model. The coupled ROMS–CoSiNE model is forced with the daily air–sea fluxes derived from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) reanalysis for the period of 1994 to 2001, and the model results are used to evaluate climate impact on nutrient transport in Mixed Layer Depth (MLD) and phytoplankton spring bloom dynamics in the JES.The model reproduces several key features of sea surface temperature (SST) and surface currents, which are consistent with the previous modeling and observational results in the JES. The calculated volume transports through the three major straits show that the Korea Strait (KS) dominates the inflow to the JES with 2.46 Sv annually, and the Tsugaru Strait (TS) and the Soya Strait (SS) are major outflows with 1.85 Sv and 0.64 Sv, respectively. Domain-averaged phytoplankton biomass in the JES reaches its spring peak 1.8 mmol N m^− 3 in May and shows a relatively weak autumn increase in November. Strong summer stratification and intense consumption of nitrate by phytoplankton during the spring result in very low nitrate concentration at the upper layer, which limits phytoplankton growth in the JES during the summer. On the other hand, the higher grazer abundance likely contributes to the strong suppression of phytoplankton biomass after the spring bloom in the JES. The model results show strong interannual variability of SST, nutrients, and phytoplankton biomass with sudden changes in 1998, which correspond to large-scale changes of the Pacific Decadal Oscillation (PDO). Regional comparisons of interannual variations in springtime were made for the southern and northern JES. Variations of nutrients and phytoplankton biomass related to the PDO warm/cold phase changes were detected in both the southern and northern JES, and there were regional differences with respect to the mechanisms and timing. During the warm PDO, the nutrients integrated in the MLD increased in the south and decreased in the north in winter. Conversely, during the cold PDO, the nutrients integrated in the MLD decreased in the south and increased in the north. Wind divergence/convergence likely drives the differences in the southern and northern regions when northerly and northwesterly monsoon dominates in winter in the JES. Subjected to the nutrient change, the growth of phytoplankton biomass appears to be limited neither by nutrient nor by light consistently both in the southern and northern regions. Namely, the JES is at the transition zone of the lower trophic-level ecosystem between light-limited and nutrient-limited zones.