用PowerBuilder实现仓库管理系统的开发

以 2 35处仓库管理系统为例 ,介绍了利用 Power Builder开发数据库的设计与实现方案 ,并对其设计过程出现的问题进行了分析和解决     

提高熔炼不锈钢电弧炉炉衬寿命的措施

某特钢厂改进熔炼不锈钢电弧炉操作工艺、造渣制度和采用炉渣发泡技术后，使电弧炉炉衬寿命从30炉提高到60炉以上，并保证2台30tEBT电弧炉与l台30tAOD妒相匹配。炉衬寿命进一步提高后，可望l台EBT电弧炉与l台AOD炉相匹配，提高不锈钢产量。     

隐藏的数学--谈数学抽象思维的不完全性

文章从隐藏的数学这一角度对数学的抽象化进行了分析，指出了数学抽象思维不完全性的意义，同时点明了数学普及的迫切需要——走近数学。     

防范跨国公司内部价格转移的对策研究

目前，跨国公司进驻我国已成为客观必然，而且将越来越多。跨国公司在推动我国经济发展的同时，也不可避免地带来了一些负面影响。最主要的方面就是利用其内部贸易，将本该属于我国享有的利润通过价格转移的手段转移到国外的母公司，致使我国的税收减少，既影响了财政收入，也影响了我国正常的经济秩序。这表明，我国防范跨国公司内部价格转移的法律制度还不健全，措施也欠完善。国外尤其是发达国家在防范跨国公司价格转移方面已经颇有成效，因此就防范措施进行国际比较，以期对我国该问题的实践有所启示和借鉴。     

基于仿射变换系的分形图形的交互式生成

提出了基于仿射变换系的分形图形的交互式生成分形图形方法，用此方法可以交互式地设计出各种形状分形图案。通过这些分形图案，可以加深对分形的理解。     

压实黄土的湿陷性与微观结构的关系

由于黄土特殊的工程性质和内部结构的复杂性，黄土地区高等级公路出现了一些湿陷破坏事故。采用扫描电镜、图像处理系统和能谱仪，对压实黄土在湿陷前后的孔隙特征、化学组成等微观结构进行研究，得出压实黄土的湿陷性与微观结构的关系。结果表明：大、中孔隙含量是黄土产生湿陷的主要原因，其与黄土湿陷系数具有定量关系，湿陷后黄土的主要化学元素含量发生了变化。     

嵌入式单片机网络测控系统的设计

介绍一种基于以太网的嵌入式单片机网络测控系统,它采用具有8052内核的高速单片机,通过对专用以太网芯片的控制,在以太网上实现了TCP/IP协议的功能,可作为以太网的一个独立系统,网络上的任何一台计算机都可通过标准的TCP/IP协议对其进行控制,传输控制命令或数据。将该网络测控系统配上数字温度传感器后实际测量工业现场温度,然后通过网络传输给计算机,可获得温度曲线,其测温范围与控温范围均为-10～+125℃,测温精度为上±1℃,分辨力达0.1℃。该系统具有结构简单、通用性强、通过Internet进行通信、使用灵活、成本低等优点,适配多种智能传感器并具有较强的扩展能力,适用于远程数据采集、远程测控等领域。     

Genetic analysis and molecular mapping of a presenescing leaf gene psll in rice （Oryza sativa L.）

A rice psl1 （presenescing leaf） mutant was obtained from a japonica variety Zhonghua 11 via radiation of ^60Co-γ in M2 generation. Every leaf of the mutant began to wither after it reached the biggest length, while the leaves of the wild variety could keep green for 25--35 d. In this study, genetic analysis and gene mapping were carried out for the mutant identified. The SSR marker analysis showed that the mutant was controlled by a single recessive gene （psl1） located on chromosome 2. Fine mapping of the psl1 locus was conducted with 34 new STS markers developed around psl1 anchored region based on the sequence diversity between Nipponbare and 93-11. The psl1 was further mapped between two STS markers, STS2-19 and STS2-26, with genetic distances of 0.43 and 0.11 cM, respectively, while cosegregated with STS2-25. A BAC contig was found to span the psl1 locus, the region being delimited to 48 kb. This result was very useful for cloning of the psl1 gene.     

半干旱区农牧交错带风水交互侵蚀特点研究——以内蒙古四子王旗南部为例

以内蒙古四于王旗南部为例，研究了半干旱区农牧交错带风水交互侵蚀的特点．结果表明，该地区低山丘陵与宽谷相间分布，坡地上有大量疏松的沉积物；夏季降水以暴雨为主，春秋季多大风，形成风水复合侵蚀发育．每年夏秋季节的水蚀为风蚀提供了大量的沙物质，第2年春季的大风将沙物质进一步吹扬扩散，为水蚀的搬运提供了物质基础，如此反复．使水系的上游形成沟谷，中下游沙化迅速．     

Depositional environments of Bathonian sediments from the Jaisalmer Basin, Rajasthan, western India

The pericratonic sedimentary Jaisalmer Basin, west of the Aravalli Ranges, on the westerly dipping eastern flank of the Indus Shelf, is a principal structural element of Rajasthan. Jurassic sediments in the SE comprise non-marine sandstones and conglomerates to nearshore, brackish to marine sands, silts, clays and carbonates, grouped lithostratigraphically into the Lathi, Jaisalmer, Baisakhi, and Bhadasar formations. The Late Bajocian to Oxfordian Jaisalmer Formation is divided, in ascending order, into the Hamira, Joyan, Fort, Badabag, Kuldhar, and Jajiya members. Fossil records providing a Bajocian to Bathonian age for the lower and middle parts of the formation include: a Late Bajocian coral Isastraea bernardiana (d’Orbigny) in the uppermost Joyan Member; Bathonian ammonite Clydoniceras in the basal part of the Badabag Member; Bathonian foraminiferal/bivalve assemblages in the Fort Member. The topmost bed of the Joyan Member represents the peak of first marine transgression of the Jaisalmer Basin, probably contemporaneous with the Late Bajocian one in the neighbouring Kachchh Basin. Based on faunal studies Bajocian to Bathonian sediments of the Jaisalmer Basin can be broadly correlated with those of the Kachchh Basin. The Fort and Badabag members represent the following depositional environments, in chronological order: (a) brackish to shallow fully marine; (b) fully marine with rapidly fluctuating water energy and sedimentation rates; (c) near-shore to lower shoreface with fluctuating energy conditions, salinity and sedimentation rates; (d) near-shore to shoreface channels and storm-dominated marine above fair-weather wave-base; (e) lagoon with fluctuating low to moderate energy, salinity and sedimentation rates; (f) stormdominated shelf to lower shoreface.