开性度模糊拓扑空间

给出开性度模糊拓扑空间的分解定理和判定定理，引入保度开（闭）映射的概念并讨论其简单性质，最后证明了一个形成新开性度模糊拓扑空间的定理。     

全芳香性螺环正碳酸酯的聚合及其产物的差热分析

研究了邻苯二酚的螺环正碳酸酯、联苯二酚的螺环正碳酸酯以及联苯二酚与邻苯二酚交叉的螺环正碳酸酯在不同条件下的开环聚合。对部分产物进行了差热分析和特性粘度的测定。     

可用于累煤层露天矿山的多周期目标规划模型

本文给出了一个可应用于复合煤层露天矿短期生产计划优化的目标规划模型.模型考虑了与煤质、煤产量及开采程序合理性有关的亏损与盈利.该方法利用了带有客观地确定权重系数的目标规划加权法.文后又给出了一个能说明该模型应用于实际采矿问题的例子.     

无粘结部分预应力混凝土空腹网架结构的设计与分析方法

本文是在文[1]基础上的推广与发展。它除有文[1]的优点外,其刚度将进一步提高,其内力将更趋均匀,从而达到进一步节约建筑材料和降低工程造价的目的。同时在文[2][3]的基础上,提出“预应力混凝土空腹网架结构的近似分析方法”,此法满足结构工程设计要求的计算精度,未知量比空间刚架矩阵位移法大为减少,节约内存、使这种预应力空间刚架结构体系能用低档微机进行计算,以利于这种新型结构的推广。     

弱几乎正规空间

Ｍ．Ｋ．ＳｉｎｙａｌａｎｄＳ．Ｐ．Ａｒｙａ在［１］中定义了几乎正规空间．本文引进了弱几乎正规空间，并指出它是几乎正规空间的一般化，讨论了弱几乎正规空间的性质以及这类空间与其它空间之间的关系．     

海州矿北帮F_（E1）断层变形区稳定性预测

本文分析了海州露天煤矿北帮ＦＥ１断层变形区工程地质条件及滑坡征，采用模型试验方法分析了边坡变形和岩移机理，结合稳定系数计算对边坡稳定状态进行了综合分析，并对该区边坡稳定性进行了初步预测．     

一种新型的开放式图形库OpenGL及其运用

本文简要介绍了一种新型的开放式图形库ＯｐｅｎＧＬ的特点及用途，并表明如何运用ＯｐｅｎＧＬ开发应用软件。     

用等势原理求解网络电阻

本文探讨了用等势原理来求解对称网络的电阻，从而引出短路法和断路法，讨论了两种方法的等效性．     

开放对象代数

本文主要讨论了开放对象的代数操作及其性质，这些操作提供了开放对象理解消息和构造消息的基本手段，同时还定义了偏序关系〖＾ｂ，并在其上讨论了这些操作的单调性，特别是递归查询。     

Linear sand ridges on the outer shelf of the East China Sea

Based on the latest full-coverage high-resolution multi-beam sounding data, the distribution of the linear sand ridges on the outer shelf of the East China Sea （ECS） is studied with quantitative statistical analysis. The study area can be divided into the northeastern part and the southwestern part. Sand ridges in the northeastern area, trending 116°N, show obvious linear character and shrink to the inner shell Sand ridges in the southwestern area, trending 120°N -146°N, tend to have net form. Sand ridges gradually become sand sheets in the center part of study area. Sand ridges are distributed landward to the isobath of 60m, distributed seaward to the water depth of 120 m in the northeast and 150 m in the southwest. Immature sand ridges are observed at water depth of 130-180 m in the southwestern depressions. The acoustic reflection properties of the internal high.angle inclined beddings of the sand ridges are analyzed based on the typical seismic profiles close to the research area. Lithological analysis and dating of 4 boreholes and 12 cores indicate that the widely distributed transgressive sand layer with high content of shell debris which was formed in the early-middle Holocene is the main composition of the linear sand ridges on the outer shelf of the ECS. The dominating factor in formation, developing and burying of the sand ridges is the variation of water depth caused by sealevel change and the rate of sediment supply. In 12400 aBP the cotidal lines of the M2 tidal component were closely perpendicular to the strike-directions of the sand ridges in the study area, and the tidal wave system during 12000-8000 aBP might play a key role in the formation of the linear sand ridges which are widely distributed on the outer shelf of the ECS.