不同周围流速和电压下的绝缘子积污特性

为了研究绝缘子在不同电压下表现的积污特性，利用流体力学的相关知识和电场理论，建立了模拟风沙的多物理场仿真模型.研究结果表明，周围流动速度较小时，绝缘子两端的电压增大，积污质量发会有一定程度的增加，且积污与电场力的变化密切相关，结合静电场分析会更准确；周围流动速度较大时，即使电压增大，积污质量也不会发生太大的变化.     

Reconsideration on Homogeneous Quadratic Riemann Boundary Value Problem

The homogeneous quadratic Riemann boundary value problem (1) with Hoelder continuous coefficients for the normal case was considered by the author in 1997. But the solutions obtained there are incomplete. Here its general method of solution is obtained.     

电磁场中带电粒子束运动的力学模拟

研究以不同初速度进入互相垂直的匀强磁场和均强电场中的带电粒子束的运动情形，并同相似的力学运动相比拟，建立了直观的力学模型。     

两指标鞅的一致收敛速度及对于平稳随机场的应用

根据平面格点序:(s_1,s_2)≤(t_1,t_2)当且仅当s_1相似文献   

用实二次型理论解多元函数的极值问题

文章以二次型理论为依据,提出了解决多元函数极值问题的另一种方法.     

电磁场问题光滑样条函数解法

利用一类二元样条函数，对任意给定区域的任意三角剖分，导出了光滑有限元方法，此方法求解二维电磁场问题，不仅可保护场域中位函数的连续性，而且可保证场量（位的导函数）的连续性，此方法与常规线性插值有限元相比，具有三角剖分数少及初始输入数据量小等优点。     

下层为多目标的两人两层决策问题的模型及优化方法

本文针对上层为单目标,下层为多目标的两人两层决策问题,建立了它的数学模型和决策机制,然后将其转化为单层的非凸优化问题。采用外部逼近算法求解此非凸优化问题的全局最优解,这为两层决策问题提供了一种求解的途径,同时为该类问题的决策支持系统的研究是有意义的。     

A theoretical model for mid-and low-latitude ionospheric electric fields in realistic geomagnetic fields

The geomagnetic fields, which play important roles in the ionospheric dynamo, can greatly affect the global distribution of ionospheric electric fields, currents and other ionospheric electrodynamics phenomena. In the study of ionospheric electrodynamics phenomena, such as the longitudinal variations of ionospheric electric fields, the non-dipolar component of the geomagnetic fields must be taken into account. In this paper, we deduce a theoretical electric field model for ionospheric dynamo at mid- and low-latitude which adopt a modified magnetic apex coordinates system. In the new electric field model, the geomagnetic fields can be calculated from either the IGRF model or the dipole field model, and the neutral winds and conductivities are calculated based on empirical models. Then the dynamo equation for the electric potential is finally solved in terms of the line-by-line iteration method, and the ionospheric electric fields and currents are derived from the calculated potential. Our model can reproduce the main features of the ionospheric electrodynamics processes, so it will be a useful tool for the investigation of the upper atmosphere and ionosphere.