应用广义拟余能原理研究流固耦合问题(英文)

水动力学与固体力学交叉的流固耦合理论是船舶与海洋工程结构响应分析与直接设计的重要工具.本文应用卷变积方法,按照广义力和广义位移之间的对应关系,将弹性动力学的基本方程卷乘上相应的虚量,然后积分,代数相加,并考虑到体积力和面积力均为伴生力,建立了非保守系统初值问题的两类变量的广义拟余能原理.应用广义拟余能原理研究流固耦合问题,分析了结构的动力响应,给出同时求解力类量和位移类量两类变量的计算方法.     

天津海事局：应对金融危机 十项措施服务港航企业

2008年12月11日,天津海事局宣布即日起将通过“提高港口船舶通航效率、公布天津主航道新的通航标准”、“推荐天津港砂石运输船舶专用航路”等十项措施,支持港航企业抵御金融危机。 天津海事局副局长黄何介绍,为支持港航企业抵御金融危机,尽可能地减轻金融危机带来的不利影响,天津海事局提出了十项措施,尽最大的努力协助天津地区港航企业渡过难关。     

加快海事强局建设步伐助推河北沿海经济腾飞

当前,交通运输行业正掀起深入学习实践科学发展观的热潮。深入贯彻科学发展观,重在发展,贵在实践。河北海事局努力提升提高“三个服务”的能力和水平,力求在解决突出问题上取得新成效,在创新体制机制上推出新举措,在提高促进科学发展能力上取得新进步,以加快强局建设步伐,助推河北沿海经济腾飞。     

发展海员队伍 扩大就业服务

2009年3月3日,全国政协十一届二次会议在北京举行,2000多位政协委员就关系我国改革发展稳定大局和人民群众切身利益的重要问题积极建言献策,切实履行职责。全国政协委员、交通运输部海事局常务副局长刘功臣此次向大会提交了《关于加快海员队伍发展,为扩大就业和新农村建设服务》的提案,建议加快海员队伍发展,为扩大就业和新农村建设服务。     

基于加权最小二乘法的武器装备批量生产成本费用研究

加权最小二乘法考虑了现实情况下普遍存在的异方差性,在经济预测中有着更为广泛的应用。在系统研究我国武器装备批量生产规律和状况的基础上,结合计量经济的相关理论,提出基于加权最小二乘法的费用预测模型,并辅以实例进行分析,结果表明,该方法移植性好,由于消除了异方差性的影响,模型的拟合和预测性能较一般最小二乘法更佳。     

海底输气管道泄漏风险定量分析

由于海底管道工作环境的恶劣性,其失效概率较高,一旦发生泄漏事故,后果严重．本文以某一海洋平台周围海底输气管道为背景,运用海洋工程领域风险评估软件NEPTUNE对不同破损情况下天然气泄漏扩散的情况进行了模拟,计算了泄漏气体点燃概率,预测了泄漏天然气爆炸事故的危害半径,其分析结果对海底管道油气泄漏扩散范围的预测及油气点燃概率计算方法的研究具有一定的参考作用．     

中国港口信息化30年辉煌建设及其展望

回顾了中国港口信息化建设30年的主要历程,阐述了中国港口信息化领先水平的表现和用高新技术改造传统产业的成绩。介绍了中国港口信息化的典型成果——电子政务和港航企业信息化对港口生产管理的促进作用,证实了我国港口建设坚持用“高新技术改造传统产业,提高管理水平”这一发展原则的正确性。     

港口产业集群与区域经济关系分析

介绍了港口产业集群的定义和内涵,通过分析港口产业集群对区域竞争力、区域品牌、资源以及经济增长等的影响,说明它对区域经济具有促进作用。同时也指出区域经济对港口产业集群的形成和发展中起了重要作用。     

燃烧室外冷却热防护数值模拟研究

本文建立了夹套式外冷却燃气发生器燃烧室热防护的CFD数值模拟模型,并用该模型对影响热防护效果的各因素进行了研究。用有限容积法离散二维轴对称N-S方程,用标准k-ε模型模拟湍流,用可压缩耦合求解器求解控制方程。研究了燃烧室内壁材料热导率、燃烧室内壁壁厚以及冷却水流量对热防护效果的影响。结果表明材料热导率对热防护效果的影响较大,高热导率的材料能够明显降低燃烧室内壁壁温和温度梯度;当燃烧室内壁为高热导率材料时,壁厚和冷却水流量对热防护效果的影响相对较小。     

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.