脉冲放大器功放级的研究

用大功率高频场效应管作为单向脉冲放大器的功放级的设计，在文献上尚未见到，作者根据需要，针对大功率高频场效应管的特点，完成这一设计。实验证明，设计是正确的，设计的关键是怎样计算场效应管的输入电容来实现推动级的设计。     

聚丁二炔（PDH＇s）中光致变色机理的探讨

基于聚丁二炔（Ｐｏｌｙｄｉａｃｅｔｙｌｅｎｅｓ）（简写为ＰＤＡ＇ｓ）中光致变色伴随Ｒａｍａｎ谱的显著改变这一事实，认为其先致变色是光诱导相结构转变的结果．建立了描述光诱导相结构转变的数学模型；对于光致变色的微观机理进行了深入的探讨；数值计算了光诱导相结构转变系数对入射光子能量的依赖关系，与实验符合。     

等面积法则的真实意义

对于等面积法则的证明有不少争议，本文阐明等面积法则的真实意义．     

壳管式储能换热器中传热特性的分析

对一种可用于储存高温余热及电厂电网谷期电力的相变储能换热器装置进行了理论和实验研究，对装置在多种工况下工作进行了模拟实验，并用数值法从理论上求解了非稳态条件下相变储能换热器中凝固与强迫对流耦和的问题，分析了热交换流体入口温度、流量、相变材料厚度、流道长度等多种参数对装置换热性能的影响。     

试论厄尼诺与山东降水作物产量的关系

厄尼诺现象使山东夏季降水偏少，强度越大，干旱越重，用降水与分离的气候产量进行回归分析的到需水量，进而评价其满足程度。厄尼诺强年所有作物减产，弱年与发生时间有关。     

投影带变换对长度变形的影响

文章对晋城矿区由矿区独立坐标系改用部定3°带平面坐标系后引起的边长影响进行了分析和计算,提出了应采取的对策及相关注意事项。     

基于3S的土地利用时空特征研究——重庆市北部新区为例

在3S（GIS，RS，GPS）技术的支持下，通过建立数学模型对城市土地利用时空特征进行研究，并以重庆市北部新城为试验区域，对该区域土地利用类型、土地利用程度、城市扩展等时空特征进行了动态分析，取得了良好的效果，为定性定量研究区域土地利用、土地覆盖的时空演变提供了一种新思路和新方法。     

新疆塔里木河湿地保护和建设的研究

新疆塔里木河湿地是我国最长的内陆河流湿地,是多种鸟类栖息与多种候鸟迁徙中转、繁殖的重要区域.本文对塔里木河湿地的基本特征、生态功能、近代变化和其保护与建设的现实意义进行了研究,指出应该重视科学研究,拯救珍稀濒危物种,并提出了相应对策.     

Some evidence of drying trend over northern China from 1951 to 2004

The surface wetness index, Palmer drought sererity index and the retrieval of soil moisture over China were calculated using monthly precipitation and monthly mean surface air temperature. Based on the contrast analysis of the variation of the above three indices and precipitation, the dry/wet spatio-temporal pattern of northern China in the last 54 years was revealed, and the evidence of drying trend over northern China was analyzed, especially. The results show the following four facts: (1) The drying trend is the main characteristic of the eastern part of Northwest China and the central part of North China since the 1980s and it was enhanced in the last 15 years mainly due to the precipitation decrease and the temperature increase; (2) During the last 54 years, there was only one dry/wet shift at the interdecadal scale occurring in the eastern part of Northwest China and the central part of North China in the late 1970s, which was related to 1977/1978 global abrupt change, whereas there were three shifts in Northeast China, one was in the mid 1990s and the other two were in 1965 and 1983, respectively; (3) Unlike the variation trend of other subregions of northern China, the western part of Northwest China is currently located in a relatively wetting period, which is weak-ened due to the temperature increase; (4) The extreme drought frequency is obviously increasing in the eastern part of Northwest China, the central part of North China and Northeast China since the 1980s, which is closely related to the precipitation decrease and temperature increase in these subregions.