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．     

柴达木盆地东部"走廊域"中新生代构造特征及构造演化

通过横穿柴达木盆地东部的“走廊域”剖面地表地质、航磁、重力、大地电磁测深和地震资料的综合分析，认为在东昆仑构造带与南祁连构造带之间，包括巴颜喀拉地块北缘，柴达木地块和祁连地块南缘等3个一级构造单元，柴达木地块内则包括了昆中构造带、昆北构造带和柴达木盆地3个二级构造单元。受东昆仑构造带和南祁连构造带相向挤压作用，柴达木盆地东部持续沉降，但由于具有稳定的花岗质基底，盆地坳陷幅度较小，且断裂及褶皱构造不发育。由此造就了柴达木盆地东部中新生代地层厚度小，烃源岩不发育，构造圈闭缺乏，除第四系天然气外，中生界、古近系和新近系油气资源前景受到极大限制。     

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.     

应用彗星试验研究两种农药对小鼠DNA的损伤

探讨采用当前国际上较先进的DNA损伤检测技术-单细胞凝胶电泳技术(SCGE,又名彗星试验),来检测农药对小鼠DNA的损伤,尝试建立小鼠的单细胞凝胶电泳技术来评价农药对生态环境和人体健康的影响.结果表明两种新型杀虫剂吡虫啉和抑食肼在一定的剂量范围内对小鼠的DNA均有一定程度的损伤作用,各浓度组与阴性对照组相比具有显著性差异(P<0.01),且具有明显的剂量效应关系.认为小鼠单细胞凝胶电泳技术能敏感地检测农药对细胞DNA的损伤,并认为细胞的DNA损伤可作为农药等化学品致突变性检测的生物标志物.     

生态遗传算法在模糊系统辨识中的应用

给出一类模糊系统的模糊神经网络模型 .提出一种实用的生态算子 ,构建的生态遗传新算法有效解决了基本遗传算法的“早熟”问题 .采用新算法实现模糊神经网络模型的辨识 ,提高了辨识精度 .实例仿真结果验证了新算法在模糊系统辨识中的有效性