边界控制方法在DVR样机研制中的应用

动态电压恢复器（DVR）可在供电电压发生电压下陷时维持负载电压稳定,以保护敏感负载。由于在正常电力系统中,电压下陷故障出现的频率相对不高,使得DVR的利用率较低。将一种基于二阶开关平面理论的边界控制器应用于DVR系统,使其既可用于电压下陷补偿又能用于稳态下电压电能质量控制,大大提高了设备利用率。通过预测DVR逆变器的某次开关动作后,其系统状态矢量的运动轨迹可得到上述二阶开关平面。将该平面作为状态轨迹沿理想开关平面运动的上界,可约束轨迹使其趋向理想工作点。为考察其动态特性,应用上述控制器的DVR样机针对源端谐波畸变和伴有畸变的下陷电压波形进行了补偿试验。结果证实上述边界控制方案可获得优于其它一些控制策略的谐波补偿效果。     

基于二值HT的多LFM信号检测

Wigner-Ville分布对于单分量LFM信号有很好的时频聚集性,但WVD是二次型变换,故对信号环境中复杂的多LFM信号不可避免的存在交叉项的干扰。HT可以消除交叉项的影响,能够很好的对多个LFM信号进行检测,但存在大信号淹没小信号的现象。提出二值HT能够很好的解决上述问题,为多LFM信号的检测技术提供理论依据。     

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。     

鱼雷内弹道特征参数估计的回归分析

论述了以建立回归方程为中心,利用有限的实验数据建立舰艇鱼雷发射内弹道特征参数（鱼雷出管速度、膛压极值）的线性回归方程。通过实验数据计算,证明这是一种舰艇鱼雷发射内弹道特征参数估算的有效方法。在回归分析法基础上,提出了如何进行实验的优化。     

宽带LFM信号的子带脉冲干扰技术

宽带线性调频信号具有高的处理增益,与信号不相关的噪声干扰难以奏效,而利用全脉冲信息形成的应答式延迟转发干扰或移频干扰虽然具有与雷达信号极高的相关性,并能得到很高的处理增益,但需要雷达信号的精确参数,且最少延迟目标回波一个脉冲宽度,在大脉宽情况下容易造成干扰失效。为此,提出了子带脉冲相关干扰技术,利用部分相干的子带脉冲干扰信号可以获得一定的处理增益,同时有降低了干扰延迟时间。理论分析和仿真试验都说明该方法可以对宽带LFM信号形成有效的干扰,具有较好的应用前景。     

水下目标深度测量误差源分析

首先研究了在深海环境下,采用基于三阵元垂直线列阵的水声探测系统进行水下目标深度测量的基本原理.然后从随机误差和阵元配置偏差的角度,对水下目标深度测量的误差源进行了理论分析,并推导了相关公式.此外,对于相干多途水声信道干扰给水下目标深度测量精度的影响,也作了初步的理论分析.通过仿真实验,总结出各误差源对水下目标深度测量精度影响的规律,研究结果为进一步开展水下目标深度测量研究、提高测量精度奠定了基础.     

船摇前馈控制补偿效果及优化方法研究

雷达隔离船摇的主要手段之一.针对船摇前馈在实际工程应用中补偿效果不理想的问题,通过对前馈复合控制原理、船摇前馈实现方法和效果影响因素的研究,提出了工程实现的优化方法.采用时间序列分析方法进行船摇数据预报可以提高近一个数量级的预报精度,从而直接提高船摇前馈补偿量的计算精度和补偿效果.通过在前馈补偿环节中加入自适应设计以实现船摇前馈信息有效平稳地加入控制环路.此外,选择适宜的时机加入船摇前馈也是工程应用的一个重要因素.     

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.     

基于多层动网格技术的流固耦合方法研究

从弱耦合的角度出发,对某型跨声速风扇叶片做了第一阶扭转振动模态下的流固耦合验证计算,采用三维线性插值方法,通过商用软件ANSYS和CFX实现了计算结构动力学和计算流体力学之间的数据交换,从而使固体域与流体域顺序祸合.应用多层动网格技术解决了固体域模型在流场中运动受到流体网格尺寸制约的问题.计算结果表明,模拟结果可以预估叶轮系统的模态气动阻尼系数,具有工程参考价值.