关于生物能量在生命体系中的传递研究（Ⅱ）

介绍了蛋白质分子的分子结构和生物功能以及Ｄａｖｙｄｏｖ等人在这系统中建立的生物能量传递的孤立子理论的特点及其存在的几个严重问题．针对这些问题，提出了一个新理论．阐明了这个理论的物理和生物学基础、理论的内容、理论的正确性、孤立子性质、理论的特点和它的运用情况．一系列的研究结果表明，孤立子能承担起传递生物能量的生物功能，在生命科学和生物学过程中是很有用的     

府谷县土地类型彩红外航片解译

以1:5万彩红外航片为主要信息源,划分出府谷县土地类型,分析了各土地类型在彩红外航片上的影像特征,探讨了土地类型遥感制图的基础与技术路线.     

顺序程序并行转换系统中程序中间表示的管理与维护

研究了基于并行分布式环境下的顺序程序转换系统中有关程序中间表示的管理与维护，讨论了顺序程序的转换过程的可视性与可干预性，并讨论了用图定义引导生成对程序相关图（ＰＤＧ）的操作等方面的问题     

电工实验教学系统的综合优化设计

ＴＳ－Ｂ型通用电工实验台是一种新型、综合的实验教学系统，本文论述了系统的基本设计思想和采用的技术方法。     

关于代数体函数的亏值

本文的主要内容有：设ｗ（ｚ）是ρ（＜∞）级２－值超代数体函数。Σδ（ａ，ｗ）＝４，则ｉ）。ρ为１／２的整数倍且ρ≥１；ｉｉ）．ｗ（ｚ）的亏值个数ｖ（ρ≤４ρ．ｉｉｉ）。ｗ（ｚ）的每一个亏值的亏量是１／ｐ的整数倍。     

用FTIR研究甲基六氢苯酐/环氧树脂体系的促进作用

本文通过5DX-FTIR 光谱仪,采用“原位”测定法,对甲基六氢苯酐(MEHHPA)固化双酚 A 型环氧树脂反应动力学进行了研究.用 Kamal 模型处理得到体系的反应级数皆为2,并求得了 E-51/MEHHPA 和E-51/MEHHPA/DMP-30两个体系在三个不同反应温度下的反应速率常数.研究发现,促进剂的加入,可以降低反应活化能,提高速率常数,从而使固化反应加速.     

稀土制剂对感染性皮肤病的疗效观察

通过临床试用 RDD-1型稀土制剂对脓疱疮、虫咬皮炎、多发性疖疮等174病例的疗效观察,说明该制剂县有一定杀菌消炎作用,对由细菌感染引起的浅表性皮肤病具有一定疗效。在174病例中痊愈85例、有效64例、无效26例,总有效率为85.1%。与白霉素制剂比较无明显差异。这种稀土制剂副作用小,无明显不良反应,使用时间短,一般在5～7天便可见效,可作为浅表性感染性皮肤病的外用药物。     

姜瘟病生物防治试验初报

用青枯病假单胞菌的拮抗微生物B130和MA—7制成的泥炭制剂具有良好的姜瘟病防治效果。B130制剂的防病及增产效果均很显著,防病效果为100.00％,增产率为34.87—48.15％;MA—7制剂仅能降低病情指数82.99—95.00％。     

Variations of optic properties of water under action of static magnetic field

Effects of static magnetic field on optic properties of water are investigated by infrared spectroscopy, ultraviolet spectroscopy and X-ray diffraction, respectively. The ultraviolet spectroscopy experiments show the changes of properties of water under action of static magnetic field, in the region of 191 to 400 nm. The infrared experiment shows that the water exposed in a magnetic field had saturation and memory effects. The magnetized effects increased with increasing exposed time, but were weakened with increasing of time when the magnetic field was removed. In the X-ray experiment, the strength of diffraction increased also, after the water was exposed in magnetic field. Meanwhile, the shift of peak and increase of strength of X-ray diffraction of magnetized water added with nanoFe3O4 occurred as compared with that of pure water added with nano Fe3O4. This result suggests that the magnetized wa- ter has certain magnetism. Finally, these phenomena are simply explained by the molecular structure of water and the theory of magnetization of water.     

Geochronolosic constraints on masmatic intrusions and mineralization of the Zhunuo porphyry copper deposit in Gansdese, Tibet

In situ zircon U-Pb ages for the recently discovered Zhunuo porphyry copper deposit in the western part of the Gangdese metallogenic belt in Tibet were determined by sensitive high-resolution ion microprobe （SHRIMP）. The ages can be divided into two separate groups, reflecting more than four major tectono-magmatic events in the area. The 62.5±2.5 Ma age of inherited zircons may be related to the volcanic eruption of the Linzizong Group formed shortly after the India-Asia continental collision. The 50.1±3.6 Ma age most likely corresponds to the time of underplating of mantle-derived mafic magma in Gangdese. The 15.6±0.6 Ma age obtained from magmatic zircons is interpreted as the age of crystallization of the Zhunuo ore-forming porphyry. Finally, a molybdenite Re-Os isochron age of 13.72±0.62 Ma is consistent with another zircon U-Pb age of 13.3±0.2 Ma, representing the time of copper mineralization. These ages, in combination with available literature data, indicate that magmatic crystallization and copper mineralization in the Gangdese metallogenic belt became gradually younger westward, and further suggest that the Zhunuo porphyry copper deposit was formed in the same tectonic stage as other porphyry copper deposits in the eastern and central Gangdese belt. This conclusion provides critical information for future exploration of porphyry copper deposits in western Gangdese.