A self-consistent analysis of a pulsed direct-current (DC) N2 glow discharge is presented. The model is based on a numerical solution of the continuity equations for electron and ions coupled with Poisson's equati...A self-consistent analysis of a pulsed direct-current (DC) N2 glow discharge is presented. The model is based on a numerical solution of the continuity equations for electron and ions coupled with Poisson's equation. The spatial-temporal variations of ionic and electronic densities and electric field are obtained. The electric field structure exhibits all the characteristic regions of a typical glow discharge (the cathode fall, the negative glow, and the positive column).Current-voltage characteristics of the discharge can be obtained from the model. The calculated current-voltage results using a constant secondary electron emission coefficient for the gas pressure 133.32 Pa are in reasonable agreement with experiment.展开更多
流体替换是了解和预测地震波速度和波阻抗如何依赖孔隙流体变化的有效工具,参数多、不确定性大是流体替代的特点,其中,干岩石模量是链接流体和饱和岩石的关键,也是Gassmann方程的基础,因此干岩石模量值的确定是流体替代的难点.前人对干...流体替换是了解和预测地震波速度和波阻抗如何依赖孔隙流体变化的有效工具,参数多、不确定性大是流体替代的特点,其中,干岩石模量是链接流体和饱和岩石的关键,也是Gassmann方程的基础,因此干岩石模量值的确定是流体替代的难点.前人对干岩石模量也进行了大量的研究,提出了许多经典模型:疏松砂岩模型、Kuster-Toksoz模型、自相容模型(selfconsistent模型)、微分有效介质模型(DEM模型)等,但这些模型都具有一定的局限性,本文通过对Gassmann方程图形分析方法(Mavko and Mukerji,1995)的研究,提出了一种计算干岩石模量的新方法.通过实际的岩样数据分析这几种算法的应用效果,研究结果认为求取干岩石模量时,本文提出的新方法具有很好的应用效果.展开更多
基金The project supported by the National Nature Science Foundation of China (No. 10275010)
文摘A self-consistent analysis of a pulsed direct-current (DC) N2 glow discharge is presented. The model is based on a numerical solution of the continuity equations for electron and ions coupled with Poisson's equation. The spatial-temporal variations of ionic and electronic densities and electric field are obtained. The electric field structure exhibits all the characteristic regions of a typical glow discharge (the cathode fall, the negative glow, and the positive column).Current-voltage characteristics of the discharge can be obtained from the model. The calculated current-voltage results using a constant secondary electron emission coefficient for the gas pressure 133.32 Pa are in reasonable agreement with experiment.
文摘流体替换是了解和预测地震波速度和波阻抗如何依赖孔隙流体变化的有效工具,参数多、不确定性大是流体替代的特点,其中,干岩石模量是链接流体和饱和岩石的关键,也是Gassmann方程的基础,因此干岩石模量值的确定是流体替代的难点.前人对干岩石模量也进行了大量的研究,提出了许多经典模型:疏松砂岩模型、Kuster-Toksoz模型、自相容模型(selfconsistent模型)、微分有效介质模型(DEM模型)等,但这些模型都具有一定的局限性,本文通过对Gassmann方程图形分析方法(Mavko and Mukerji,1995)的研究,提出了一种计算干岩石模量的新方法.通过实际的岩样数据分析这几种算法的应用效果,研究结果认为求取干岩石模量时,本文提出的新方法具有很好的应用效果.
