电路特性的PSpice仿真方法比较

应用PSpice仿真软件的两种仿真方法,分析了串联型直流稳压电源的性能,比较了这两种仿真分析方法各自的优点.电路仿真实验表明,熟练掌握数种电路仿真方法是十分必要的,仿真方法对电路分析具有实际意义和作用.     

浅谈铁和碱反应

文献［１～６］报道：“铁同强碱不发生作用”．我们用干燥的铁粉和氢氧化钠进行实验．实验证明：铁能跟强碱反应，反应的化学方程式为     

电负性及其在无机化学上的应用

从用电负性来衡量元素在化合物分子中吸引电子的能力的必要性出发，阐述电负性的概念以及阿莱－罗周（Ａｌｌｒｅｄ－Ｒｏｃｈｏｗ）计算电负性标的方法，重点论述了电负性在无机化学上的某些应用．     

基于峭度的组分分析方法解析重叠峰

基于峭度的组分分析方法用来解析重叠峰．其优点是半盲源分离，即只要确定出重叠峰所含组分的数目，就能从混合波谱中分离出纯组分谱．采用CABK来解析模拟两组分重叠峰体系和酒样的GC-MS混合谱，得到了令人满意的结果．     

集成有源负载放大器的研究

本文重点介绍了集成有源负载放大器的分析方法,并以镜像电流源为例详细介绍、对比了两种方法(图解分析法和微变等效电路分析法)。此外,介绍了用厄雷电压计算 Av 的简便方法。     

气相Lys分子体系捕获双电子单重激发态的特性

采用密度泛函理论（DFT）中的B3LYP方法, 在6-311+G(2df)基组水平上, 对气相赖氨酸（Lys）分子和Lys^2-的基态稳定构型进行优化, 并用含时密度泛函理论（TD DFT)方法考察气相Lys分子和带电离子体系单重激发态的特性. 结果表明： Lys分子体系捕获双电子时, 其体系能量有所增加； S1单重激发态与S0基态能量差值变小； 分子体系的荧光波长增加； S7单重激发态跃迁轨道数减少.     

液压支架压力变送器的电路设计

分析了液压支架的压力特性并提出对压力变送器的技术要求，阐述了压力传感器的选择和外围电路的设计，对压力变送器的信号调理电路进行了仿真分析。     

中水回用前景及其实际意义

概述了中水及中水回用的概念,分析了目前中水回用中存在的问题,探讨了水源热泵技术的应用。     

Influence of Microstructure and Sintering Routes on Transport Properties of Apatite Materials for Fuel Cells

1 Results Oxy-apatite materials are thought as zirconia-substitutes in Solid Oxide Fuel Cells due to their fast ionic conduction. However, the well known difficulties related to their densification prevent them from being used as such. This study presents strategies to obtain oxy-apatite dense materials and the influence of elaboration route on transport properties. Particular emphasis is put on the microstructure effect on ion conduction. By the combined use of freeze-drying and conventional or spark p...     

Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.