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.     

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   

SrFCl:Eu~(2+)晶体的电子自旋共振谱研究

用程序降温法生长了SrFCl:Eu~(2+)晶体,并测量了它的电子自旋共振谱。应用最小二乘法拟合技术对g因子及自旋哈密顿参数进行了精确拟合。报道了各向异性的g因子及有关自旋哈密顿参量。发现并归属了Eu~(2+)的高阶禁阻跃迁。     

中能区反质子与原子核散射的极化度

在已获得的中能区反质子与核的中心势的光学势基础上,把光学势扩大到包含自旋轨道耦合势.在反质子能量为179.8,294.8和508MeV各情况下,分别计算和分析与~(12)C靶核的微分截面(dσ)/(dΩ),极化度P(θ)和自旋转动函数Q(θ).在与极化度的实验比较中,得到中能区普遍形式的反质子光学势.     

磁畴形成的原理探索

本文运用量子力学和固体物理学分析铁磁物质及其磁畴形成的原理     

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.     

点态化Fuzzy域及其性质

本文从点的角度重新定义了Ｆｕｚｚｙ域，并讨论了它的一些性质。     

Magnetic order in Cr73.7(Fe0.83Mn0.17)26.3 alloy

Conclusions  The results we obtained in the present investigations can be summarized as follows.

毡体密度对C/C复合材料增密和结构的影响

用液化石油气作碳源、针刺炭毡作增强体,在自行设计的多元耦合物理场CVI炉中制备炭/炭(C/C)复合材料,在毡体内部设置石墨纸作发热体,并研究了一次性沉积15 h后,毡体密度对增密速度和材料结构的影响.采用偏光显微镜研究了沉积炭的显微结构,用XRD均峰位法研究了材料的石墨化度,并用排水法测量材料的表观密度.研究表明, CVI工艺增密速度随毡体密度的增加呈下降趋势,而较高的毡体密度有利于获得较高石墨化度的高织构的粗糙层结构(RL)热解炭.图4,参15.