动力学模拟中的自洽热点追踪:一种改进测试粒子法的方法

A. Esmaeili
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引用次数: 0

摘要

与流体模拟相比,粒子模拟最重要的优点之一是能够处理和跟踪粒子。在粒子模拟中,通常使用测试粒子方法来了解等离子体或其他物质的行为。该方法首先在固定电磁场的框架内注入少量粒子;然后,利用粒子电场的模式研究了粒子的运动。这种方法很有用;然而,由于我们需要在系统中使用固定字段,因此它缺乏精确性。在这项工作中,我们采用了粒子模拟方法,增加了直接来自模拟的动态场的灵活性。在这里,我们试图研究粒子从具有北行星际磁场(IMF)的太阳风进入磁层尖端。正如我们的初步结果所示,粒子的自洽路径不跟随磁场线走向尖端,这与传统的测试粒子方法的非自洽结果略有不同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Self-Consistent Hot Spot Tracing in Kinetic Simulations: A Method to Improve the Test Particles Method
One of the most important advantages of particle simulation as compared to fluid simulation is the capacity for working with and tracing particles. In particle simulations, the test particle method is usually used to get some idea of the behavior of plasma or other substances. In this method, first, a small number of particles are injected into the frame of fixed electromagnetic fields. Then, movement of particles is investigated using the pattern of their electric fields. This method is useful; however, as we need to work with fixed fields in our system, it lacks precision. In this work, we adapted the particle simulations method, adding the flexibility of working with dynamic fields that come directly from the simulation. Here we have tried to investigate particle entry from the solar wind with northward Interpanetary Magnetic Filed (IMF) to the magnetospheric cusp. As our initial results shows, self consistent path of particles does not follow the magnetic field lines going to the cusp that is slightly in contrast to the conventional non self consistent results from test particle method.
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