相互作用电子平衡分布函数的新双曲统计

IF 0.6 Q4 GEOCHEMISTRY & GEOPHYSICS
Y. Zelenin, T. A. Bilyi
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引用次数: 0

摘要

本文提出了一种新的低参数分布的统计量sech (ε,µ)型,它高精度地再现了多粒子动力学方法(DMP)等离子体模拟的结果。该分布基于双组分等离子体-负能量(激子相位ε0)虚准粒子的概念模型。根据DMP实验结果,对sech (ε,µ)分布统计量的适用性进行了优化和初步估计。sech (ε,µ)分布将三段DMP分布的参数从4个能量扩散系数(D1, D2, D3, D4)减少到2个-化学势µ和不对称系数α。在sech (ε,µ)分布中,D1, D2, D3, D4与体系化学势µ的泛函关系与迁移率和能量扩散常数之间的爱因斯坦关系类似。该微分方程的泛函变量属于椭圆函数族。它比给出的双曲解宽得多,对于能量ε的复值具有重要的物理应用。提出的简化方案以负能量的物理解释为基础,可用于大气的电测电子,这在以前提出了重大的方法困难。流体(亚稳态)和气相的化学势是等离子体缺陷参数的函数。这个问题是作为大气中电测电子问题的一个应用而提出的。所提出的分布在数理统计和统计物理中没有表示;这是全新的,非常相关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New hyperbolic statistics for the equilibrium distribution function of interacting electrons
New statistics of a low-parameter distribution of the sech (ε, µ) type are presented, which reproduce the results of plasma simulation by the method of dynamics of many particles (DMP) with high accuracy. The distribution is based on a conceptual model of a two-component plasma — virtual quasiparticles of negative energy (exciton phase ε<0); the scattering region of positive energy (gas phase ε>0). Optimization and elementary estimates of the applicability of the sech (ε, µ) distribution statistics were made after the results of DMP experiments. The sech (ε,µ) distribution reduces the number of parameters of the three-piece DMP distribution from 4 energy diffusion coefficients (D1, D2, D3, D4) to two — the chemical potential µ and the asymmetry coefficient α. The functional relationship D1, D2, D3, D4 with the chemical potential of the system µ in the sech (ε, µ) distribution is introduced in a similar way to the Einstein relation between mobility and energy diffusion constants. The functional variety of the differential equation belongs to the family of elliptic functions. It is much wider than the hyperbolic solution given, which has significant physical application for complex values of the energy ε. The proposed simplified scheme grounded in the physical interpretation of negative energies can be written for the electrometric electrons of the atmosphere, which previously presented significant methodological difficulties. The chemical potentials of the fluid (metastable states) and gas phases are presented as functions of the plasma imperfection parameter. The problem is posed as an application to the problem of electrometric electrons in the atmosphere. The proposed distribution is not represented in mathematical statistics and statistical physics; it is new and extremely relevant.
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来源期刊
Geofizicheskiy Zhurnal-Geophysical Journal
Geofizicheskiy Zhurnal-Geophysical Journal GEOCHEMISTRY & GEOPHYSICS-
自引率
60.00%
发文量
50
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