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.     

功率集成光激MOS控制交流多路开关模拟设计

介绍了一种新型功率集成光激MOS控制多路开关，它由双向晶闸管，MOS器件，光电器件组成。此开关通过光电转换来实现强电与弱电之间的隔离，可工作在交流状态，其通态压降低，约在1．5－3V之间，并对其阻断特性，电流特性，开关特性进行了全面的模糊分析，此开关适用于开发各种电源开关产品。     

求解非线性问题的修正弧长增量法

本文介绍的修正弧长增量法是求解非线性问题的一种新思路 ,在弧长增量法的基础上 ,引进虚拟弹性系统及虚拟弹性刚度的概念 ,且弧长增量不为常数 ,根据每次迭代所得的残余荷载计算下次的位移增量。从而免去解线性方程组的繁复过程 ,大大提高了计算速度     

黄鳝雌雄个体间LDH和EST同工酶的比较研究

用聚丙烯酰胺凝胶垂直板电泳技术,比较分析了黄鳝雌雄个体间6种组织的乳酸脱氢酶(LDH)和酯酶(EST)的同工酶谱。结果表明:这两种同工酶仅在雌雄个体的肾和性腺中的表达同时存在显著差异;黄鳝和其它硬骨鱼一样,其同工酶的表达有明显的组织特异性。     

Cauchy弹性的次弹性形式表述

本文利用张量函数梯度的定义,解析地导出了Cauchy弹性的次弹性本构表达形式,并应用于一类软组织材料和Mooney—Rivlin等橡胶材料。     

猪颌下腺活性肽对大鼠应激性溃疡形成的影响

实验选用体重200—250g S.D.系健康大鼠27只.雌雄不拘。浸水应激6小时后致大鼠产生应激性胃溃疡,并观察猪颌下腺活性肽在其中的作用。结果如下:对照组动物胃溃疡面积密度为17.9±1.43%(平均值±标准误.下同);应激前30分钟腹腔注射颌下腺活性肽0.1mg 组溃疡面积密度为19.1±2.62%;0.2mg 组溃疡面积密度为10.7±1.78%,较对照组减少40.2%(P<0.01);0.5mg 组溃疡面积密度为5.3±0.96%。分别较对照组和0.2mg 组减少70.4%(P<0.001)和50.5%(P<0.01)。统计表明,大鼠胃溃疡面积密度与活性肽注射剂量呈明显的负相关(r=-0.9302,P<0.05)。本工作提示,猪颌下腺活性肽具有阻止或减轻大鼠应激性溃疡形成的作用。     

全局性隐函数定理及其应用

得到两个全局性隐函数定理:定理1设D_1是第一可数的拓扑空间E_1的开子集.D_2是Banach空间E_2的开子集.映象f:(?)_1×(?)_2→Y(?)E关于第一变元连续且满足条件:1°|f(x,y_1)-f(x,y_2)|≤L(x)|y_2-y_1|.Ax∈(?)_1.y_1.y_2∈D_2.其中Y=D_2或D_2=Y=E_2,L(x)<1.L:(?)_1→R~+连续.则方程f(x.y)=y有连续解y:(?)_1→Y,即f(x.y(x))=y(x).(?)x∈(?)_1.定理2 设f:(?)_1×(?)_2→C((?)_2)满足条件:1°d(f(x,y_1).f(x,y_2))≤k|y_2-y_1|.(?)x∈(?)_1.y_1.y_2∈(?)_2.其中k<1是常数.d(·,·)表示:对有界闭子集A_1,A_2(?)(?)_2d(A_l,A_2)=sup{|y_1-y_2||y_1∈A_1,y_2∈A_2}2°(?)y∈(?)_2,多值映象,f(·,y)弱下半连续.C((?)_2)为(?)_2的有界闭凸子集类.则包含方程y∈f(x,y)有连续单值解y;(?)_1→(?)_2即y(x)∈f(x,y(x)) (?)x∈(?)_1还给出了对随机映象不动点存在性的一个应用.     

具有基的Banach空间弱收敛

本文给出具有Shrinking基的Banach空间中序列弱收敛的等价条件.