应用矩量法研究有限长带电直导线的电荷分布

文章采用矩量法数值计算有限长带电直导线的电荷密度分布.结果表明,带电直导线的电荷密度分布不均匀,导线两端电荷密度大,中间电荷密度小,正电荷密度呈"∪"分布,负电荷密度呈"∩"分布,计算结果较为精确并具有良好的收敛性.     

基于COMSOL的磁流变液盘式制动器仿真优化与研究

采用Bingham流体模型分析了磁流变液盘式制动器的制动力矩,设计出一种外绕线圈的单盘式制动器结构,利用COMSOL软件对该结构进行建模、电磁场仿真、制动力矩计算与结构参数优化。研究表明,制动力矩基本与旋转盘的角速度无关,制动过程中制动器可获得相对稳定的制动力矩;在一定的磁动势下,当旋转盘半径增加时,盘式制动器的制动力矩会逐渐增加;增加导磁外壳的厚度有利于约束磁力线,进而提高制动力矩。     

Microscopic mechanism of periodical electroosmosis in reservoir rocks

Based on the electric double layer (EDL) theory and the momentum equation governing the electroosmosis flow, this paper presents an analytical solution to the periodical electroosmosis with a parallel straight capillary bundle model of reservoir rocks to reveal the microscopic mechanism of the electroosmotic flows in rocks. The theory shows that both the frequency dispersion characteristics of the macroscopic electroosmotic Darcy velocity in unsealed rocks and the electroosmotic pressure coefficient in sealed rocks depend on the porosity and electrochemical properties of reservoir rocks. The mathematical simulation indicates that the distribution of the periodical electroosmotic velocity is wavelike in the rock pore. The greater the porosity is, the greater electroosmotic the Darcy velocity and the smaller electroosmotic pressure coefficient are generated. The module values of the electroosmotic Darcy velocity and the electroosmotic pressure coefficient increase with the decreasing solution concentration or the increasing cation exchange capacity without affecting the phase of the electroosmotic Darcy velocity.     

储层岩石周期性电渗流特性的微观机制

以双电层电位理论和电渗流动的动量方程为基础,结合储层岩石平行毛管束模型,推导出岩石孔隙内周期性电渗流的解析式,揭示了储层中电渗效应的微观机制,分析了非密闭储层岩石中宏观电渗Darcy速度及密闭储层中电渗压力系数频散特性的影响因素．数学模拟结果表明:储层岩石孔隙中,周期性电渗流速度剖面在频率较高时呈“波浪”状;孔隙度越大,电渗Darcy速度模值越大,其相位也越大,而电渗压力系数数值越小．储层岩石的溶液浓度越小或阳离子交换量越大,电渗Darcy速度模值和电渗压力系数数值越大,但对电渗Darcy速度的相位没有影响．     

大学物理实验成绩的模糊评价

学生的实验成绩是多因素、多变量、界限模糊的事物,直接进行定量分析难以科学、合理地对其学习进行正确评价.本文采用模糊推理进行评价,科学合理地评估学生的物理实验成绩.