Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

A carbon- and oxygen-isotope record of recent environ- mental change from Qinghai Lake, NE Tibetan Plateau

An understanding of natural climatic variability is essential for evaluating anthropogenic impacts on recent and future climate[1—3]. Due to the lack of lengthy instrumental records, such an understanding must be gained from natural archives of climate change. Palaeolimnological indicators of past lake levels may provide a sensitive record of changes in effective precipitation in closed basins. This approach is particularly relevant on the Tibetan Plateau, where instrumental records are very…     

泥石流危险性动量分区方法与应用

运用泥石流运动数值模拟和GIS相结合的方法模拟泥石流出山口后的运动全过程, 求得泥石流流速和流深分布, 确定泥石流过程中泛滥范围内任一点的最大动量, 建立了泥石流危险性动量分区模型Z = Khv. 根据考察和实验资料对委内瑞拉首都加拉加斯的Chacaito沟百年一遇泥石流运动过程进行了模拟, 利用动量分区方法划分出泥石流危险区.     

连续系统振动特征值摄动问题的统一解法

将离散系统振动分析中的通用的矩阵摄动法推广到连续系统。采用弹性结构理论算子，对连续系统的振动特征值摄动问题进行统一描述。根据特征函数子空间缩聚法和正交分解的基本原理，推导了统一的摄动公式。该方法能同时有效地处理孤立、重及密集特征值3种不同情况。以薄膜振动和变厚度薄板弯曲振动的特征值问题为例，阐明了方法的实际应用。     

两种线分维及线分维与面分维间关系

分别用二次电子扫描线法和垂直抛面法对不同回火制度的３０ＳｉＭｎＣｒＮｉＭｏＢ钢的冲击断口表面的分维数进行了数量。通过研究发现：平行裂纹扩展方向的分维更适合于描述材料韧性的变化。     

卟吩质子化过程结构变化的理论研究

用ＡＭ１ＭＯ方法计算了质子化卟吩的构型，并通过结构分析、电荷布局分析和前线轨道分析，讨论了其质子化过程的构型变化及Ｒａｍａｎ光谱变化的原因。     

复杂载荷下的疲劳寿命估算

从疲劳过程本质上是材料静强度不断退化过程的观点出发，建立了一个强度退化模型．将模型应用于两级、多级和随机载荷下疲劳寿命估算，经试验和算例验证，表明该方法是合理可行的     

合成TiN膜的俄歇电子能谱研究

采用离子束增强沉积方法（ＩＢＥＤ），在Ｆｅ基上制备了ＴｉＮ薄膜。通过划痕仪，透射电镜（ＴＥＭ），俄歇电子能谱（ＡＥＳ），粘着力测量仪的观测，分析和计算，给出了膜的形貌，组分和机械特性；发现ＴｉＮ膜与衬底之间存在一过渡区，膜中含氧量比气相真空沉积（ＣＶＤ）明显减小。在ＡＥＳ定量计算中，本文采用一种与文献不同的方法，较为简便地处理了俄歇谱中Ｔｉ和Ｎ峰的重叠现象