论文标题

电气流作为非线性不稳定性:模型详细信息

Electric streamers as a nonlinear instability: the model details

论文作者

Lehtinen, Nikolai G.

论文摘要

我们提出了一种新的方法来明确确定正电流排放和负电气排放的参数。从流体动力方程式中,假设流媒体形状的解决方案,可以在流媒体参数之间得出几个关系,该参数形成了代数方程(SAE)系统。由于实现了近似值,因此该系统解决方案的误差可能会达到几百分之几。求解SAE使我们能够以流式长度$ l $,恒定统一的外部电场$ e_e $和流媒体半径来表达所有流媒体参数。具有不同半径的溶液是流体动力方程的有效溶液,类似于具有不同横向波长的平坦前扰动的传播模式。我们将流媒体解释为非线性不稳定性,其行为是通过选择速度最大化的半径来确定的,因为在我们显示的情况下,速度与线性不稳定性的情况下的角色与指数增长率相同。 因此,流媒体行为以相对经济的方式由$ e_e $和$ l $明确决定。相反,求解微观方程的数值方法(例如流体动力模拟)在计算上是更要求的,并且由于数值波动而自动出现首选解决方案。在海平面条件下空气的计算为常见的流媒体参数提供了合理的值。计算出的阳性流质速度和负阈值场与实验测量兼容。还讨论了正阈值场的物理原因。一个简化的分析模型(附录B)至少在定性上再现了许多提出的结果。

We propose a new approach to unambiguous determination of parameters of positive and negative electric streamer discharges. From hydrodynamic equations, in the assumption of a solution in the shape of a streamer, it is possible to derive several relations between streamer parameters, which form a system of algebraic equations (SAE). Because of the made approximations, the error in the solution of this system is expected to be probably up to a few tens of percent. Solving the SAE allows us to express all streamer parameters in terms of the streamer length $L$, the constant uniform external electric field $E_e$, and the streamer radius. The solutions with different radii are valid solutions of the hydrodynamic equations, and are analogous to the propagation modes of flat-front perturbations with different transverse wavelengths. We interpret the streamer as a nonlinear instability, whose behavior is determined by choosing the radius at which the velocity is maximized, because, as we show, the velocity plays the same role as the exponential growth rate in the case of linear instabilities. Thus, streamer behavior is unambiguously determined by $E_e$ and $L$, in a relatively computationally economical way. In contrast, numerical methods of solving the microscopic equations, such as hydrodynamic simulations, are more computationally demanding, and the preferred solution in them arises automatically because of numerical fluctuations. The calculations for air at sea level conditions produce reasonable values for commonly observed streamer parameters. The calculated positive streamer velocities and negative threshold fields are compatible with experimental measurements. The physical reason for the positive threshold fields is also discussed. A much simplified analytical model (Appendix B) reproduces many of the presented results, at least qualitatively.

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