硫代双乙醇的超临界水热分解过程

在等温管式平推流反应器中研究了超临界水中硫代双乙醇 (TDG)的水热分解反应 ,反应温度为 42 5～ 5 2 5℃ ,压力为 2 2～ 30 MPa,反应停留时间为 0 .6～ 6 3.2 s。结果表明 ,TDG可在超临界水中快速、彻底分解。TDG分解产物为甲烷、一氧化碳、二氧化碳、乙烯、氢气、乙醇、乙醛、硫化氢和单质硫。 TDG转化率随停留时间增加而增大。随温度和压力升高 ,TDG分解速率加快。分析表明 ,TDG的水热分解过程是通过水解和热解两条反应路径进行的     

掺纳米Al2O3的纳米8YSZ相变及电导率

掺8mol%Y2O3的纳米ZrO2粉体中加入0－5wt%纳米Al2O3，在1100℃、1200℃、1300℃不同温度下烧结2h，烧结样品在烧结温度达1200℃以上，掺1wt%以上的纳米Al2O3的四方相完全转变为立方相。初步探讨掺纳米Al2O3的8YSZ陶瓷烧结体相变机理及纳米Al2O3对8YSZ烧结体的晶参数和电导率影响。     

核密度估计的中偏差

在一些正则性条件下，使用Gaer-Ellis定理和尾概率估计的某些技巧，得到了核密度估计在点态和一致范数下的两个中偏差定理。     

Loess in the Tian Shan and its implications for the development of the Gurbantunggut Desert and drying of northern Xinjiang

Eolian loess is widely distributed on the various geomorphic surfaces between 700–2400 m a.s.l. on the northern slope of the Tian Shan. It is formed in a synchronous manner with dust transported from the Gurbantunggut Desert in the Junggar Basin. The thickest section of loess was found in the Shawan and Shihezi regions. Paleomagnetic and climatic proxy analyses of over 71 m of a loess-paleosol sequence on the highest terrace of the Qingshui He (River) in the Shawan show that the paleomagnetic Bruhues/Matuyama (B/M) boundary lies at the bottom of paleosol S8, at a depth of 69.5 m, and the bottom of the sequence was estimated to be ∼0.8 Ma. This implies that the extremely dry climatic conditions in the Junggar Basin and the initial Gurbantunggut Desert were present at least by 0.8 Ma. High-resolution grain size series demonstrate that this area and desert expansion experienced two dramatic periods of desert expansions that occurred at ∼0.65 Ma and 0.5 Ma, respectively; and the subsequent continuous enhancement led to the environment presently observed. This tremendous environmental effect, caused by large-scale expansion of the desert and arid region of inner Asia, might be an important driving force for the global temperature drop that occurred in the mid-Pleistocene.     

PGE patterns of ores of Dajing Cu-polymetallic deposit in Linxi County,Inner Mongolia: Indicator to source of metallogenic elements

By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and the black ores composed mainly of sphalerite and galena, reflecting affinity of their source. The PGE patterns of the yellow ores composed basically of chalcopyrite, arsenopyrite and pyrite are actually different. One is close to the pattern of the mantle lherzolite, and others resemble the pattern of the basic rocks. However, the concentrations of Ru are higher in the yellow ores, reflecting that sulfur attains or approaches saturation in their parent magma. The PGE characteristics of ores and dikes show that the magmas derived from the deep of crust and the metallogenic elements were supplied mainly by growth material of the crust. In addition, the mantle-derived magma also offered some elements.     

组合夹具计算机辅助设计系统研究

本文介绍了一种基于MDT的组合夹具计算机辅助装配系统 ,简要介绍了组合夹具元件图库的建立 ,组合夹具的装配与定位误差分析。采用面向对象开发环境VC ++作为界面开发工具 ,利用ODBC技术实现数据库链接 ,采用Autodesk公司自身提供的ARX接口实现在MDT下应用程序的加载。     

SIMPLE算法的一个新的改进方案

提出了SIMPLE算法的一个新的改进方案－－MSIMPLE。该采用SIMPLEC中的方法对速度主程进行处理，同时对压力的确定采用SIMPLER中的方法来完成。通过对2个典型的流动传热问题（圆管突扩通道内的流动，正方形空腔内的自然对流）的计算，将该改进方案与SIMPLE，SIMPLEC，SEMPLER算法进行了初步对比，结果表明，改进方案有着更好的收敛特性，并且能节省数值计算的计算时间。