齐格勒-纳塔催化剂催化苯乙烯淤浆预聚合

通过淤浆预聚对齐格勒-纳塔催化剂催化的苯乙烯预聚动力学规律和预聚条件对预聚物粒子形态的影响进行了系统的研究。结果表明苯乙烯在石油醚中的聚合速率是衰减型的，但随着溶液中甲苯含量的增加聚合速率曲线会出现增长型。聚苯乙烯的粒子形态与溶剂种类和单体浓度有很大关系。较适宜的预聚条件是在石油醚中单体浓度为0．6mol／L、温度为40℃和反映时间问40min。但由于受扩散控制严重，在石油醚中的聚合速率比较慢。     

多层升降横移式立体停车库的结构和控制系统

介绍了立体停车库的主要形式 ,着重分析了多层升降横移式立体停车库的结构及控制系统原理 ,编制了多层升降横移式立体停车库控制系统的程序 .经调试、运行证明 :采用可编程序控制器 (PLC)作为控制系统可行、简单且易于实现     

麦克斯韦速度分量分布分析

一般教材对麦克斯韦速度及速率分布均做了较详细的分析^[1-3]，但对速度分量分布却较少讨论，这里应用一般统计法和比较法，以速度x分量分布为例，给出了气体分子热运动的速率分量分布的特征值及温度分界值，分析了气体温度对麦克斯韦速率分量分布函数的影响，并对结论做了讨论。     

基于Fourier变换非一致间距阵列的一种合成法

基于阵列图及其分布间的Fourier关系，作者提出了非一致间距阵列的一种合成方法。在Fourier关系下，通过抽样一个给定的阵列图，就能使用FFT(快速Fourier变换)得到其近似连续的阵列分布。为提高改善阵列图的性能，提出一个算式用于决定非一致间距阵列的空间间隔，从而在合成的阵列中保持更多的能量。该方法简单且易于应用。     

在物理实验教学中开发学生的非智力因素

充分发挥学生的主观能动性,变被动教育为主动教育历来是教师面临的一大难题,在大力提倡素质教育的今天这显得尤为重要,本文讨论了如何于物理实验教学中,有效地开发学生的非智力因素,从而使学生“要学”、“乐学”、“会学”。     

Inhibitory effect of the adenovirus type 5 E1A protein expressed in the yeast system

The human adenovirus type 5 E1A, a tumor- suppressor gene[1], codes for two major related proteins of 243 amino acids (12S) and 289 amino acids (13S) by al-ternative splicing in two exons[2]. Studies have been shown that E1A can regulate expression of many genes and cell cycle[3]. Both in vitro and in vivo experiments indicated that E1A could induce tumor cells differentia-tion, convert tumor cells into an epithelial phenotype, in-hibit tumor cell growth and metastasis and strongly en-ha…     

A complete sequence and comparative analysis of a SARS-associated virus(Isolate BJ01)

Severe Acute Respiratory Syndrome (SARS) is a newly identified infectious disease[1—5]. The global outbreak of SARS has been threatening the health of people worldwide and has killed 353 people and infected more than 5462 in 27 countries, as reported by WHO on April 29, 2003 (http://www.who.int/csr/sarscountry/en). Although it has been recognized that a variant of virus from the family of coronavirus might be the candidate pathogen of SARS[1—5], its identity as the unique pathogen sti…     

辽河盆地东部凹陷北部地区Es1+2/Es3不整合面与油气运聚的关系

根据 2 2 4口井的实际资料 ,结合地层沉积特征和地震剖面解释结果对辽河盆地东部凹陷北部地区Es1+ 2 /Es3 不整合面的上、下地层的接触关系及岩性组合特征进行了平面规划及分类 ,探讨了该不整合面与油气运聚的关系。研究结果表明 ,不整合面在油气运聚过程中所起的作用主要是由不整合面上、下地层的接触关系及岩性配置所决定。研究区凹陷北部茨 5 9井—茨 80井、龙 12井—龙 2 4井等区域为寻找不整合面之下遮挡油气藏的有利地区 ,茨 6 7—茨 6 15区域是该不整合面之上油气聚集的有利区     

A surface-based DNA algorithm for the minimal vertex cover problem

Abstract DNA computing was proposed for solving a class of intractable computational problems, of which the computing timewill grow exponentially with the problem size. Up to now, many achievements have been made to improve its performance and increase itsreliability. It has been shown many times that the surface-based DNA computing technique has very low error rate, but the technique hasnot been widely used in the DNA computing algorithms design. In this paper, a surface-based DNA computing algorithm for minimal ver-tex cover problem, a problem well-known for its exponential difficulty, is introduced. This work provides further evidence for the abilityof surface-based DNA computing in solving NP-complete problems.     

Nd isotopic characteristics of Proterozoic metasedimentary rocks and constraints on their provenance in the eastern segment of Central Tianshan Belt, Xinjiang

Sm-Nd isotopic characteristics, εNd(t) values and Nd model ages (TDM) of Proterozoic metasedimentary rocks in the eastern segment of Central Tianshan Belt (ESCTB), Xinjiang, are used to constrain the sedimentary provenance as well as to evaluate their tectonic implications. εNd(t) and TDM values of these samples range from -4.00 to +6.36 and from 1.29 to 2.29 Ga, respectively. These feature values are distinguished from those of Archean Tarim Craton. Their average εNd(t) values of the Weiya, the Kumishi and the south to the Dikar samples are -2.46, +2.06 and +1.37, respectively. Nd model ages of the Weiya samples vary between 1.86 and 2.29 Ga, but those of the Kumishi and the south to the Dikar samples show a significant concentration at 1.6～1.9 Ga and the youngest Nd model age is 1.29 Ga. Those Nd isotopic characteristics suggest that these metasedimentary rocks could be derived from a significant proportion of Paleoproterozoic crustal source and a participation of young arc materials, rather than Archean Tarim Craton. Furthermore, the data also indicate that these two sources were paleogeographically separated. Thus we can deduce that the Kumishi and the south to the Dikar metasedimentary rocks were formed proximal to the arc side of the back-arc basin, but the Weiya metasedimentary rocks were closer to the continental side of the back-arc basin.