固体工质电热化学炮膛内两相流模型与计算

该文建立了固体工质电热化学炮（SPETCG）内弹道一维两相流模型。对常规火炮两相流模型的主要改进包括：在初期点火阶段,建立了描述等离子体射流分布的积分近似数学模型;在燃烧阶段,引入了描述等离子体射流的混合长度模型和燃烧增强因子。并且考虑了高温等离子体环境对相间换热的强化效应。根据SPETCG环境中等离子体射流注入特点,在计算网格设计中引入了自适应方法。通过与常规弹道作比较,指出了SPETCG内弹道过程与常规弹道不同的特点,为SPETCG的弹道设计提供了理论依据。     

过滤管道作为第二阳极的磁过滤阴极真空弧沉积系统

建立了一台磁过滤脉冲阴极真空弧沉积装置,通过在90度磁过滤管道和阴极之间加30－60V的正偏压使系统沉积速率得到了大幅度提高,研究和观察表明,此时在过滤管道和阴之间产生了阴极真空弧放电,并因此使阴极消耗率大幅度增大,对此放电回路及其和MEVVA阳极－阴极之间弧放电的相互影响进行了初步的实验研究。     

TiO_(2-x)纳米粒子薄膜型氧敏元件的性能

以钛酸丁酯和无水乙醇分别为前驱体和溶剂 ,添加适量稳定剂制成稳定溶胶 ,用浸涂法在 Al2 O3基片上制备 Ti O2 薄膜 ,经在 10 0 0℃氢气氛下还原制得 Ti O2 - x薄膜 .通过 SEM照片发现薄膜颗粒在几十纳米左右 ,颗粒分布均匀 .由 XRD分析 ,薄膜的 x值在 0～ 0 .5之间 .实验结果表明 ,Ti O2 - x薄膜在 80 0℃下具有良好的氧敏感性和响应特性 ,薄膜在 N2 条件下具有很好的电阻 -温度特性     

有害废气的低温等离子体脱出研究

对低温等离子体脱出以甲苯为代表物的空气中有机挥发物进行了研究,考察了气体流速、进口浓度等因素对脱出效果的影响。结果表明,采用低温等离子体技术,在室温及较高流速下,对模拟废气中的甲苯有较高的脱除净化能力。     

转炉炼钢综合自动化系统

研究设计了转炉炼钢综合自动化系统,介绍了其结构和原理,讨论工业现场经常出现的调试难点及相应的解决方法。     

铸铁等离子束淬火区的特点

通过观察铸铁材料等离子束淬火的组织,并结合等高子束的温度分布,分析了等离子束淬火区的组织转变特点及硬度分布特点。结果表明：铸铁材料等离子束淬火时,淬硬层与基体之间基本没有过渡区,整个淬硬层的组织近乎全部为隐针马氏体,故硬度高,且硬度在整个硬化层没有明显的变化;淬硬层略有凸起,并受到来自未淬火的基体的挤压力,这对于提高硬化带的接触疲劳强度是有利的。     

低气压放电中的弧光放电发展及其抑制方法

在高频直流脉冲放电的条件下,对低气压放电过程中存在的弧光放电的发展过程进行了研究,揭示了脉冲放电频率的提高对抑制弧光放电的发展是有效的,而快速的弧光放电检测和保护电路是不可缺少的.为一种新型等离子体高频激励电源的研制提供了有效的依据.     

极端相对论电子对横等离子体波的散射

计算了极端相对论电子对横等离子体波的Compton散射与非线性散射,给出了极端相对论电子对横等离子体波的散射概率及散射谱,该谱与真空中极端相对论电子对单色入射光的逆Compton散射谱有着明显的不同,且出射波极大频率与入射波频率之比也与真空中逆Compton散射不相同。     

Adsorption and reaction of CO and O2 on the Ag/Pt(110) surface studied by photoemission electron microscopy

The Ag/Pt(110) model catalyst was prepared by evaporating silver on Pt(110). Adsorption and reaction of CO and O₂ on Ag/Pt(110) surface were studied in situ by photoemission electron microscopy (PEEM) during the pressure range of 10^-5——10^-2 Pa at 480 K. The Ag/Pt(110) surface consisted of Pt(110), AgPt interface and Ag area after annealing at 500 K. The dosing pressure of CO and O₂ had a larger influence on their adsorption on the Ag area than on the Pt(110) and AgPt interface. Small Pt clusters formed on the Ag area and AgPt interface, which had a stronger ability to adsorb CO than Pt(110) terrace. The existence of Ag had an obvious influence on the kinetic of CO oxidation on Pt(110). No pattern was observed on the AgPt interface under the same condition when the formation of reaction-diffusion waves occurred on Pt(110).     

Oxygen isotope evidence for two-stage water-rock interactions of the Nianzishan A-type granite in NE China

The oxygen isotope ratios of whole-rock, common rock-forming minerals and zircon from Mesozoic A-type granitic pluton at Nianzishan in northeastern China were analyzed by the conventional BrF5 method and the laser-probe technique, respectively. Both whole-rock and rock-forming minerals show large δ18O variations up to 5.5%. with significant oxygen isotope disequilibrium between zircon and the other minerals, whereas the δ18O values of zircon are tightly clustered between 3.12%. and 4.19%. and thus lower than the normal-mantle δ18O values. These results indicate that the Nianzishan A-type granite experienced two-stage water-rock interactions subsequentially. The remarkably low zircon δ18O values are genetically due to sea-water exchange with granite protolith in the first stage, and the oxygen isotope disequilibrium fractionations between zircon and rock-forming minerals are caused by meteoric-hydro thermal alteration in the second stage. It is inferred that the 18O-depleted A-type granitic magma was derived from partial melting of subducted lower oceanic crust which was isotopically exchanged with seawater at high temperatures. In the process of granite emplacement into the upper crust, meteoric-hydrothermal circulation was triggered to overprint crystallizing granite under subsolidus conditions.