也谈“用惠斯通电桥测电阻”实验

本文主要对杨介信、陈国英编写《普通物理实验(二、电磁学部分)》“用惠斯通电桥测电阻”实验中δR_(x0)=(R_4/R_3)δR_2的含意等五个问题,提出自己的不同看法。     

层流中粉尘的火焰传播速度

建立了筛落式粉尘火焰试验装置和火焰信的号光电测量系统。提出确定火焰前沿位置的“最大斜率切线法”和判定火焰传播稳定性的“相对入射能量法”。测定了硅钙粉和煤粉的火焰传播速度和火焰厚度。结果表明数据合理,测量装置和方法可用于速度范围很宽的粉尘火焰传播研究,用修正的田中达夫模型计算的硅钙粉层流火焰传播速度与实验值接近。     

负载扰动观测器在SF型矢量控制系统中的应用

文章提出广义逆矩阵来设计离散型状态观测器的方法,用该法设计的观测器,可对SF型矢量控制系统的负载力矩进行估计,再进行前馈补偿。实验证明,该法可有效改善系统的动态性能。     

枪口火焰光电测量方法探讨

该文简述了常用枪口火焰测量的几种方法,对各方法存在的问题下作了系统分析,类比于枪口噪声的测量科学地提出了评价枪口火焰大小及强弱的评价指标,在此基础上提出了一种行之有效的光电测试方法,文中阐明了该方法的原理及系统组成,通过枪口火焰的实弹实验,证明了该方法的可行性。     

The v-v energy transfer of highly vibrationally excited states (I)

The relaxation of the highly vibrationally excited CO (v = 1–8) by CO₂ is studied by timeresolved Fourier transform infrared emission spectroscopy (TR FTIR). 193 nm laser photolysis of the mixture of CHBr₃ with O₂ generates the highly vibrationally excited CO(v) molecules. TR FTIR records the intense infrared emission of CO(v→v-1). The vibrational populations of each level of CO(v) have been determined by the method of spectral simulation. Based on the evolution of the time resolved populations and the differential method, 8 energy transfer rate constants of CO(v = 1–8) to CO₂ molecules areobtained: (5.7±0.1), (5.9±0.1), (5.2±0.2), (3.4±0.2), (2.4±0.3), (2.2±0.4), (2.0±0.4) and (1.8±0.6) (10¹⁴ cm³ · molecule⁻¹ · s⁻¹), respectively. A two-channel energy transfer model can explain the feature of the quenching of CO(v) by CO². For the lower vibrational states of CO, the vibrational energy transfers preferentially to the u³ mode of CO² For the higher levels, the major quenching channel changes to the vibrational energy exchange between CO(v→v-1) and the u¹ mode of CO².     

The v-v energy transfer of highly vibrationally excited states (II)

The vibrational energy transfer from highly vibrationally excited CO to H₂O molecules is studied by time-resolved Fourier transform infrared emission spectroscopy (TR FTIR). Following the 193 nm laser photolysis of CHBr₃ and O₂ the secondary reactions generate CO(v). The infrared emission of CO(v → v−1) is detected by TR FTIR. The excitation of H₂O molecules is not observed. By the method of the spectral simulation and the differential technique, 8 rate constants for CO(v)/H₂O system are obtained: (1.7 ±0.1), (3.4 ±0.2), (6.2 ±0.4), (8.0 ±1.0), (9.0 ±2.0), (12 ±3), (16 ±4) and (18 ±7) (10¹³cm³ · molecule^-1· s^-1). At least two reasons lead to the efficient energy transfer. One is the contributions of the rotational energy to the vibational energy defect and the other is the result of the complex collision. With the SSH andab initio calculations, the quenching mechanism of CO(v) by H₂O is suggested.     

伴随矩阵的若干性质

从特殊矩阵的伴随矩阵的关系考察了伴随矩阵的性质。     

利用真实砂岩微观孔隙模型研究粘性不稳定指进

利用真实砂岩微观孔隙模型进行了不同油水粘度比下的油水两相驱替试验,研究了粘性不稳定指进;提出了控制注入水粘性指进的注入速度及油水粘度比的要求,对指导油田生产有一定的意义。     

盛冰期南京石笋δ18O与年纹层厚度的对比

根据南京葫芦洞一支石笋高精度^230Th年龄及纹层计数，建立年际精度时标．在21800～21180aBP时段内，石笋纹层厚度与δ^18O的良好相关性，支持纹层厚度反映夏季风降水效应的观点．两种代用指标提供了末次盛冰期持续620年的十年际分辨率季风降水信息．年纹层及δ^18O序列的功率谱分析结果表明全球冰量最大背景下十年-百年尺度的季风气候变化与太阳活动周期基本一致．     

地板送风静压层内气流的数值模拟与送风特性实验

采用计算流体力学(CFD)技术,对地板送风静压层的空气流动进行了数值模拟,并进行了典型的实验来验证计算结果.通过对计算结果与实验结果的比较,说明对于地板送风静压层内空气流动的CFD模拟,采用0 1 m的网格划分间距、标准k ε湍流模型是合理的.实验和计算结果一致表明,对于高度为170 mm的地板送风静压层,地板送风口的速度和送风量分布受到入口射流的影响,处于不同位置的地板送风口,其速度分布不同,有的均匀,有的速度值相差10倍.由数值模拟的地板送风静压层内空气流动特征,可展示和分析地板送风静压层的以上送风特性.