Influence of initial heeling angle on ship roll motion response北大核心CSCD

[目的]系统地研究初始横倾角对随机横浪下船舶横摇运动响应的影响。[方法]以路径积分法为基础,通过数值求解控制横摇运动微分方程概率属性的Fokker-Planck方程,得到横摇运动响应的概率分布。[结果]结果显示,初始横倾角对船舶横摇运动响应谱的影响有限,但对横摇角概率分布以及横摇运动响应极值分布的影响十分明显,且会造成船舶安全性的显著恶化。[结论]路径积分法可作为研究随机海浪下船舶横摇运动特性的有效数值方法。     

小半径曲线桥30m预应力T梁的预制

结合云南省保山(大官市)至龙陵(龙山卡)高速公路9标段小半径(R=250 m)曲线桥30 m预应力T梁的预制,介绍T梁模板的设计制作、T梁的施工工艺以及施工中应注意的问题。     

企业经营呼唤精细管理

针对我国目前存在的管理粗放、忽视细节这一现象,比照西方先进企业在细节上追求完美的意识,指出对细节的忽视已经给企业经营带来了严重影响,认为提高企业经营水平、加强政府管理和转变经济增长模式都离不开对细节的关注和改善。同时,分析了管理者和被管理者忽视细节的原因,并对如何改变忽视细节这一现象提出了一些看法。最后指出关注和改善细节是时代的迫切要求。     

融合RCM、PHM和数据挖掘的城市轨道交通车辆维护决策技术研究

提出了一种用于轨道交通车辆系统维修决策的RCM(以可靠性为中心的维修)可靠性评估的新方法。针对轨道交通车辆系统故障机理复杂,影响因素冗多,提出基于RCM、PHM(故障预测与健康管理)和数据挖掘算法相融合的方法来构建系统的维护决策模型。与传统方法的区别在于,该方法能够更精准地定义维护模型,并获得系统的最优维护间隔,计算效率高,适用于复杂状态系统的可靠性计算。该方法可有效降低传统RCM的维护不足现象,降低运维成本,具有一定的推广应用价值。     

湿陷性黄土地区地下连续墙施工技术

结合浐河站地下连续墙施工实例,从工程概况、具体施工方案、劳动力设备配置、施工进度、质量保证措施等方面介绍了湿陷性黄土地区地下连续墙的施工技术。     

基于捷联惯性系统的轨道长波不平顺检测

将航空航天飞行器制导中的捷联惯性系统应用于轨道长波不平顺的检测。利用四阶龙格-库塔法求解四元素姿态矩阵微分方程;采用积分滤波器对加速度信号进行二次积分,从而实时获取物体的运动轨迹。为提高系统的稳定性和抗噪性,在积分前利用小波变换对加速度信号进行去噪处理。最后采用XW-IMU5250惯性测量单元实测一个物体的运动,得到了物体精确的运动轨迹,通过对比不同时期测量结果即可得到轨道的长波不平顺信息。     

马房大桥钢桥面的沥青混凝土铺装研究

结合钢桥面铺装工程实际问题，讨论马房大桥钢桥面铺装处治工程中沥青混凝土铺装层施工工艺。     

基于数理统计方法的铁路隧道衬砌质量缺陷分析

目前,利用地质雷达法检测隧道衬砌质量时,通常仅对隧道衬砌缺陷进行描述,较少深入分析这些缺陷的内在分布规律.采用数理统计的方法,对某在建铁路工程14座隧道共285个衬砌质量缺陷样本的分布规律进行分析.研究表明,(1)在不同测线部位,其缺陷率、不同缺陷类型占该测线缺陷比例、缺陷径向尺寸的最大值、平均值及样本标准差均不同;(...     

遥感图像融合最新进展及展望

文章综述了遥感图像融合的基本概念,研究了遥感图像融合的分类及常用方法,对遥感图像融合评价进行了探讨,系统深入地分析了遥感图像融合面临的问题,指出了未来的发展趋势及解决问题的方向。     

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.