不同碳材料对挥发性有机气体的吸附性能研究

本文以苯、正庚烷、1,2-二氯乙烷、氟利昂22(F22)作为VOCs代表物质,考察了不同碳材料对VOCs的吸附能力。试验结果表明:不同碳材料对苯、正庚烷、1,2-二氯乙烷的吸附呈现出相似规律。在相同的吸附条件下,吸附能力是球形活性炭>常规活性碳>改性活性碳纤维>活性炭纤维,同一种碳材料对三种代表物质的吸附能力为:正庚烷>苯>1,2-二氯乙烷。几种碳材料对F22的吸附能力很差。     

富春江船闸扩建改造工程创新设计与实践

针对碍航闸坝瓶颈问题,以富春江船闸为例,全面总结已建枢纽实施船闸扩建改造工程的主要关键技术与创新设计,包括保留原船闸并紧接新建一座大尺度船闸的总体布置、船闸结构设计、新老船闸衔接输水系统、老船闸加固改造、坝下施工围堰等,达到既满足通航安全要求,又避免对大坝安全、防洪安全、电站发电等不利影响,对解决我国众多枢纽船闸碍航问题具有典型示范作用。     

铁矿尾矿砂在公路基层中的应用研究

对铁尾矿砂及尾矿砂加入石灰水泥后的物理力学性能进行了试验研究,并与石灰土进行对比。结果表明：铁尾矿砂掺加石灰、水泥后,其强度随着龄期而增长,具有半刚性材料的特性,用石灰、水泥稳定尾矿砂作为路面基层材料具有很好的路用性能,同时用石灰和水泥稳定的效果更佳。     

弹性基础上的三维编织复合材料板的非线性振动分析

基于宏-细观力学分析,考虑编织纱线连续性对材料性能的影响,建立了三维编织复合材料板的单胞模型.采用Reddy高阶剪切板理论,给出四边简支编织材料矩形板在不同几何参数、纤维体积含量和弹性地基参数情况下的vonKármán-Donnell型振动方程的解,并讨论了弹性基础刚度、面内载荷、边厚比和编织角等对编织复合材料板的振动频率的影响.理论分析结果与文献结果吻合较好.     

C^4ISR作战系统仿真建模方法研究

对于建设C^4ISR系统来说,系统需求工程的出发点之一应该是基于对作战的描述,同时对目前作战过程进行描述的若干方法进行分析对比,结合实际情况对作战过程描述进行讨论并给出新的切入点。文章给出了一种实现C1ISR仿真系统和实装模拟系统互联的设计方案。该方案使用基于HLA的代理联邦将分布在仿真系统网络上的各个仿真节点和实装系统连接到C^4ISR仿真系统中,并通过HLA／RTI完成仿真系统与实装系统间的交互。     

短波并行组合扩频通信系统研究

对短波环境下并行组合扩频系统进行研究,提出一种适合短波并行组合扩频通信的MPSK软解调方法。该调制方式比并行组合扩频常采用的MASK调制方式性能更好。在扩频增益相同条件下,短波并行组合扩频通信选取结构参数r值较小（r=2）的短波并行组合扩频系统为宜。在所选择系统结构的接收端应用RAKE接收技术,仿真表明RAKE接收技术能有效抵抗多径影响,改善短波并行组合扩频系统的误码率性能。     

简化UKF算法在SINS／GPS组合导航中的应用

针对SINS／GPS组合导航系统的特点,建立了系统的非线性误差模型。根据系统状态方程为非线性而观测方程为线性的特点,将一种简化的UKF方法（Rao-Blackwellisation Additive Unscented Kalman Filter,RBAUKF）用于SINS／GPS组合导航系统中,RBAUKF采用较少的采样点数目和简化的更新算法,降低了计算复杂度。最后,在机动条件下,进行了SINS／GPS组合导航实验仿真。仿真结果表明,RBAUKF相比EKF具有更高的滤波精度,更适合在SINS／GPS组合导航系统中应用。     

基于混和法的齿轮箱基座动力学特性全频域计算

统计能量法(SEA)在航空航天和船舶领域进行动力学环境预报方面有着广泛应用,适用于大型、复杂结构与高频率激励环境.但该方法在计算中低频振动噪声时,由于众多子系统动力特性差异,动力响应计算将产生很大误差,出现SEA失效问题.近年来出现的FE-SEA混合模型方法可有效解决这一问题,并能实现大型复杂结构的全频域一体化建模,在统一平台上进行低频、中频和高频计算及结果输出,简化建模和不同软件下模型转换,是非常适用于工程的一种方法.本研究探索采用具有上述功能的VA One软件进行舰艇基座全频域混和法动力学预报,这是国内外的首次探索,具有重要学术与工程价值.     

三类边界条件下隔水套管涡激非线性振动的比较分析

考虑流及波流联合作用,研究了套管的涡激非线性振动.将套管简化为梁模型,考虑3类不同的边界条件,计及莫里森非线性流体动力和涡激荷载,建立套管的涡激振动方程.应用克雷洛夫函数求解套管的固有频率和模态,采用了计算涡激非线性动力响应的迦辽金方法.以东海勘探3号钻井隔水套管为例,研究了不同边界条件下流引起的主共振和波流联合引起的组合共振.计算结果表明：流对套管的动力响应占主导地位,而波的影响不大.分析了3类不同边界条件下隔水套管的涡激非线性动力响应,揭示了波流联合激励下套管复杂的动力响应特性.     

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.