电流型GTR有源无功补偿器的研究

介绍了以电流波形补偿理论为根据，由ＧＴＲ电流型四象限变流器构成的有源无功功率补偿器。详细叙述了补偿器的补偿原理、主电路工作方式、控制系统的结构及其控制策略。实验表明该系统能实时地、完全地补偿电网上的基波和谐波无功，并且具有系统简单、控制方便、体积小等优点。     

混合型并联有源滤波器的研究

为实现对非线性负载的谐波补偿和电压调节功能,提出了一种混合型并联有源滤波器.综合考虑系统稳定性和谐波补偿效果,采用了反馈加前馈的控制策略,对比研究了系统补偿特性,并讨论了容性和感性无功补偿问题.仿真与试验结果证明了该混合型并联有源滤波器工作的有效性.     

200km／h动力分散型电动车组主变压器辅助绕组电压的选定

针对我国用于客运专线的200km/h动力分散型电动车组，通过对网压波动的讨论和主变压器辅助绕组电压与电流的计算，说明了主变压器辅助绕组电压选择790V的理由。     

铝电解晶闸管整流系统的谐波抑制与无功补偿

论述了铝电解大功率晶闸管整流系统电能质量问题，分析了该系统的无功补偿装置容量的选取与抑制谐波电流谐振的关系。其分析结论对类似的工程设计，尤其对滤波器的设计和电力系统的安全运行起到一定的参考作用。     

船舶电站物理仿真实验装置典型故障分析

阐述了最新研制开发的船舶电站物理仿真实验装置的仿真原理,分析并排除了该装置调试运行过程中出现的典型故障,为电站操作人员提供参考。     

基于阻抗匹配平衡变压器和AT供电方式的新型同相牵引供电系统

电气化铁道的牵引供电系统三相严重不平衡，存在大量的谐波和无功，各供电区段需要用分相绝缘器分隔，从而制约了高速、重载铁路的发展。基于阻抗匹配平衡变压器和AT供电方式的新型同相牵引供电系统，不仅可以解决以上问题，还继承了AT供电方式所特有的通信防护效果好、综合经济技术性能优越的特点；同时在有源滤波器的作用下，实现了单台双绕组工作变压器的接线方式，比原系统结线简单、维护方便。文中分析了系统平衡变换原理，讨论了系统的平衡方式、补偿电流检测与有源滤波器控制方法。分析和仿真证实本文提出的平衡方式和检测方法是正确的，同相供电系统方案是可行的。     

楼宇自备电站微机集控系统

结合具体的工程实例,阐述楼宇自备电站常规控制系统存在的主要问题,以及通过采用微机集控系统, 提高系统可靠性和稳定性的做法.     

电力电子技术与铁路机车牵引动力的发展

回顾了铁路机车牵引技术发展历程及电力电子技术对铁路机车技术进步的巨大推动作用,着重分析了交流传动的特点和优越性,结合国内铁路机车牵引传动技术的现状,对我国交流传动技术的发展方向提出一些设想.     

瘫船启动在COSCOQMC-Ⅰ型轮机模拟器中的实现

本文探讨了SOLAS公约关于船舶瘫船状态的定义、瘫船启动的概念以及船舶原始动力源的型式,阐述了瘫船启动在COSCOQMC-Ⅰ型轮机模拟器中是如何实现的,强调轮机管理人员应加强对船舶原始动力源的维护和管理,确保船舶的适航性和营运安全。     

On the fresh balance of the Adriatic Sea

The long-term mean fresh water balance of the Adriatic Sea is studied by ananalysing evaporation, precipitation and river runoff. Evaporation is computed from May latent heat flux and by means of bulk formula. In the latter case two wind speed data sets are used, namely those from the NMC and May. The sea surface temperature is taken from a historical Adriatic data set, and the air temperature and relative humidity come from the NMC data set. Two precipitation data sets are considered, namely the Legates and Willmott climatology and a data set consisting of data measured at 62 rain-gauge stations located on the Adriatic coasts. Runoff contribution to the fresh water balance is estimated from the long-term average flow rates of 39 rivers and the horizontal distribution of salinity in the upper mixed layer.The spatial distribution of the fresh water balance, as well as of its components, is analysed by means of monthly objective maps, from which averages and standard deviations are computed. The results obtained from the different computations are not always univocal, particularly in the evaluation of Summer evaporation, and are affected by relatively large statistical errors. Significant spatial and seasonal variability occurs, with a noticeable fresh water gain along the coastline of the northern and middle basins, while small areas of fresh water loss are found in the middle and southern basins. Nevertheless, on an annual basis, the difference between the fresh water losses by evaporation and the gains by precipitation and runoff is clearly negative, indicating that, unlike the whole Mediterranean, the Adriatic Sea is generally a dilution basin.