基于牛顿迭代法的概位修正误差分析

介绍了双信号台测向定位中利用牛顿迭代法进行概位修正的方法,分析了牛顿迭代法对概位修正误差的消除过程。仿真结果表明：在满足舰船导航精度要求下,牛顿迭代法的迭代次数少,且误差很小,达到了概位修正的要求。     

机载光电干扰技术的发展动向与分析

机载光电干扰技术在现代战争中发挥着越来越重要的作用.文章介绍了机载光电干扰技术的发展历程以及装备的研制、改进情况,指出了在现代战争中发展机载光电干扰技术的优势和重要性,重点探讨了几种机载光电干扰技术的性能及其特点,最后论述了机载光电干扰技术的发展动向与分析.     

现代散货码头生产营运信息化管理

在介绍现代散货码头营运管理控制系统建设的目标与原则的基础上,阐述该系统创新技术,以实现码头生产作业自动化、营运管理数字化,最终实现高生产效率、高管理水平、高系统安全、低能耗成本、低设备故障的散货码头营运系统。     

体外预应力主动加固技术施工控制分析

根据某T型刚构桥的病害情况、受力特点,采用有限元软件midas/civil对结构进行三维空间有限元建模计算分析。通过对某特大桥的体外预应力加固全过程进行现场施工监控,分析比较体外预应力筋的索力、结构的应力、挠度改变量等的理论值和实测值,得出有价值的结论,用于指导工程实践。     

硬岩铁路隧道湿喷聚丙烯纤维混凝土支护结构稳定性分析

在隧道支护结构中采用湿喷工艺喷射聚丙烯纤维混凝土技术可以提高隧道围岩的稳定性,符合混凝土向高性能、绿色化、施工注重环境保护的发展趋势。在宝鸡-兰州复线东巨寺沟铁路隧道选取试验段中实施湿喷工艺喷射聚丙烯纤维混凝土,作为支护结构,并作永久性支护结构,免除二次衬砌工作。采用非线性有限元方法,分析了该铁路隧道试验段采用湿喷纤维混凝土支护结构的隧道围岩稳定性,分析了未支护和湿喷纤维混凝土支护的隧道围岩稳定性。分析结果表明：与未支护的隧道相比较,支护后的隧道围岩塑性区分布范围得到了减小,隧道变形微小。隧道变形实测结果表明：隧道的变形微小,处于稳定状态。     

信息化时代武器装备电磁兼容技术发展趋势

在C4ISR系统EMC和防护,EMC“预测分析法”设计与控制,电磁环境效应(E3)验证与评估及防护技术,频谱管理,以及EMC新技术、新材料、新器件开发应用等五个方面论述当前EMC技术的发展趋势。     

BIM与GIS融合技术在航道整治工程中的应用

针对航道整治工程中BIM技术无法管理条带状工程、难以表达工程周边地理信息等难点,通过梳理BIM与GIS数据特点,研究探索BIM与GIS融合技术,提出了通过格式转换、坐标转换和数据关联实现BIM与GIS融合的方法。将研究成果应用在蕲春水道航道整治工程,验证了BIM与GIS融合方法的可行性,实现了BIM与GIS数据一体化浏览、显示、管理、分析等功能,解决了BIM无法管理大范围工程、无法反映工程周边环境的不足,为BIM与GIS技术在航道整治工程中的应用提供了技术支撑。     

渗透球壳流固耦合问题的位移及内力解

在弹性薄壳的线性(非线性)理论和流体力学基本方程的基础上,在小雷诺数的情况下应用相容欧拉-拉格朗日法建立了渗透球壳在流体中流固耦合的基本方程及关系式,并通过摄动法求解了渗透球壳在粘性流体中的流函数从而进一步解出其位移及内力解.通过具体算例,给出了壳的位移变形及内力图,并对有关参数进行讨论,绘出相关曲线.得出渗透系数k和流速越大的情况下,壳体位移也就越大,相应的内力也变大;球壳在三个角度处位移为零.文章能为过滤器问题提供指导.     

高速公路长大纵坡沥青路面施工技术研究

在山区修建高速公路,将面临较平原区更严格的要求。结合当前山区高速公路施工的现状,就山区高速公路长大纵坡路段的施工技术进行了探讨。     

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.