射流悬浮床气固两相流动的数值模拟

从多相流多流体模型、气相湍流k-ε模型与颗粒湍流k_p模型出发,对底部向上射流悬浮床内气固两相流动进行数值模拟,得到了不同入口气速下各截面的颗粒相速度场、颗粒相脉动速度场的分布,结果与实验定性一致。计算结果与实验值对比的结果表明,数值模拟对进一步的研究有指导意义。数值结果与实测值间存在的差异则有待于进行直接三维流动模拟、进一步考察更为合理的边界条件及应用更先进的模型来解决。     

铝/硅橡胶交织复合材料压缩力学行为的研究

制备了铝/硅橡胶交织复合材料,并对其进行静态压缩实验,分析了其压缩力学行为及吸能性.铝/硅橡胶交织复合材料的压缩应力 应变曲线呈现双阶段平台的特征,平台区总的长度远大于与复合材料中相同结构参数的泡沫铝压缩曲线上的平台区长度,且压缩曲线没有明显的压实区.在相同的应力峰值下,铝/硅橡胶交织复合材料的压缩吸能性和吸能效率均高于参数相同的泡沫铝,因而可作为性能优异的吸能材料.     

空气水两相段塞流的跟踪模拟及试验研究

分析了前人提出的段塞跟踪模拟方法的优缺点 ,根据液塞头部的加速压降和入口液塞长度分布特征对段塞跟踪模型进行了改进。采用面向对象技术 ,实现了水平和倾斜管道段塞流的跟踪模拟 ,并与多相流试验环道的空气水试验数据进行了对比。模拟结果表明 ,当不考虑加速压降时 ,用跟踪模型预测的压降低于实测值 ;当考虑加速压降时 ,用跟踪模型预测的压降高于实测值。在管道上固定位置测出的压力信号符合正态分布 ,管道上某一固定点处液塞头部和尾部的速度分布也符合正态分布。当不考虑气泡尾波作用时 ,液塞长度沿管线增长较慢 ,分布形状无变化 ;但是考虑气泡尾波作用时 ,在入口附近液塞长度平均值增长较快 ,统计分布沿管轴向呈对数正态分布。     

论FDI对西部制度变迁的影响及对策

本文首先对我国西部地区利用FDI的现状进行了描述 ,然后运用回归分析的方法分析了FDI和制度变迁的关系 ,指出FDI是影响区域制度变迁的重要因素 ,FDI在区域分布上的不均衡严重制约着西部地区制度变迁的进程。西部地区应该加快体制改革的步伐 ,改善投资环境 ,吸引FDI ,进而通过FDI带动西部地区制度变迁的进程 ,最终形成FDI和制度变迁相互推动、相互促进的良性循环。     

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.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

1,3-苯二氧基二乙酸二芳酯的合成及植物生长调节活性

以PEG 4 0 0为催化剂 ,在液 液相转移催化条件下合成了一系列新的 1,3 苯二氧基二乙酸二芳酯 .用元素分析、IR以及1 HNMR确定了它们的结构 .初步生物活性试验表明 ,该类化合物对小麦幼苗的生长有一定的促进作用 .     

改变水分子簇的结构及诱发的生物效应研究

概述了水分子簇理论研究的基本状况,以及改变水分子团簇结构的4种方法,包括外加磁场、外加电场、激光辐射以及直接加热法;最后简要介绍了改变水分子团簇结构所诱发的生物效应.     

并联电压负反馈输入、输出电阻的讨论

电路中引入负反馈,使输入、输出电阻均发生变化,并且输入、输出电阻对放大电路有很大的影响.从并联电压负反馈的角度,对输入电阻和输出电阻给出了下列4种方法的定量讨论.     

形变条件对热变形过冷奥氏体相变的影响

热变形造成的奥氏体组织结构的变化将影响到热变形奥氏体在随后冷却过程中的相变．依据热模拟试验结果，研究了变形温度、变形速率、变形量和变形后高温停留影响相变过程的微观物理本质，认为变形促进热变形奥氏体的相变，提出变形温度、变形速率和变形后高温停留时间对热变形奥氏体转变过程没有直接联系，但可以通过对再结晶过程的控制影响相变过程．再结晶虽然可能细化了晶粒，但大量消耗了热变形奥氏体中的晶体缺陷，其结果是迟滞了相变过程．