基于交错并联的Ⅱ型五电平逆变器电路的仿真研究

研究了一种基于交错并联的Ⅱ型五电平逆变器电路。该拓扑是双BUCK电路的一种变形,可以视为双BUCK拓扑和交错并联技术结合的产物。这种拓扑减少了开关器件,降低了系统复杂度,而且提高了输出频率,大幅度减小了用于滤波的无源器件的体积。介绍了该拓扑存在的7种状态和4种模态。介绍了Ⅱ型五电平的单向仿真,详细阐述了其正弦脉宽调制.仿真结果符合之前的理论研究,说明该拓扑在大功率变换场合有其前景。     

短距离无线通信系统中信道编码技术

介绍了短距离无线通信系统中信道编码技术方案的具体实现过程。原始数据通过卷积编码和交织等差错控制编码技术后传输,很好的解决了实际应用中误码率高、硬件解决成本高的技术难题,为在现有窄带设备上进行高速数据传输提供了一种新方法。     

集通铁路长大隧道GSM-R冗余方案研究

针对集通铁路的长大隧道,论述分布式基站和数字光纤直放站的两种冗余方案,通过分析比较两种方案的单网交织以及同站址双网冗余覆盖方式,推荐采用分布式基站单网交织冗余方案.     

云浮市区典型交叉口通病诊断

结合云浮市区典型交叉口现状,剖析通病所在,从技术和管理层面提出症结的解决方案,可供相关技术人员参考和借鉴.     

On the parameterization of interleaving and turbulent mixing using CTD data from the Azores Frontal Zone

CTD-data obtained in the Azores Frontal Zone using a towed undulating vehicle are analyzed to study the relationship between characteristics of intrusions and mean parameters of the thermohaline field. A self-similar dependence between intrusion intensity and hydrological parameters is obtained. The most well-founded interpretation of the empirical dependence is as follows: (a) the main source supporting intrusive layering is the salt finger convection; (b) the abrupt decrease of intrusion intensity with the reduction of geostrophic Richardson number obtained from the analysis is explained by the beginning of turbulence when salt fingers do not work any longer, so the “driving force” for intrusive motion disappears. These results are consistent with the conclusions of the paper [Kuzmina N.P., Rodionov V.B., 1992. About the influence of baroclinicity upon generation of the thermohaline intrusions in the oceanic frontal zones. Izvestiya Akad. Nauk SSSR, Atmosperic and Oceanic Physics 28 (10–11), 1077–1086]. These conclusions imply that there are three main mechanisms of intrusive layering at oceanic fronts, namely the 2D baroclinic instability of geostrophic flow, the vertical shear instability and the thermohaline instability where the driving source of intrusive motion is double diffusive convection. The baroclinic and thermohaline instabilities can generate intrusions of large vertical scale, while vertical shear instability usually gives rise to thin turbulent layers. Turbulence in these thin layers can prevent salt finger convection and thus destroy the energy source of the intrusive motion conditioned by thermoclinicity. Therefore, the baroclinicity plays two parts in the processes of the intrusive layering: (1) it prevents double-diffusion interleaving by means of turbulence, and (2) it generates intrusions due to the 2D baroclinic instability of geostrophic current. Using features of thermohaline interleaving as a specific tracer of turbulent mixing, we have estimated turbulent mixing coefficient as k_tRi^−0.8 (Ri>1), where Ri is the geostrophic Richardson number. Application of the proposed approach to other frontal zones is discussed.     

铁路线路缓和曲线路段附近导线点的中线投影里程计算

通过对缓和曲线解析坐标公式的分析，利用曲线外导线点在曲线上的投影点的几何特性，依据现行铁路规范推导出了它在曲线上的投影长度和里程的计算公式，并评价了计算精度和收敛情况。大量和严格工程算例证明，该计算公式是可靠的、计算方法是可行的。