Lejosne Solène
Space Sciences Laboratory, University of California, Berkeley, CA, 94720.
J Geophys Res Space Phys. 2019 Jun;124(6):4278-4294. doi: 10.1029/2019JA026786. Epub 2019 Jul 4.
I briefly review, compare and contrast two theoretical works that have significantly influenced radial diffusion research thus far, namely, the works of Fälthammar (1965, https://doi.org/10.1029/JZ070i011p02503) and the works of Fei et al. (2006, https://doi.org/10.1029/2005JA011211). Leveraging Fälthammar's model for magnetic field disturbances, I demonstrate that Fei et al's formulas are incorrect: they underestimate radial diffusion by a factor two in the presence of magnetic field disturbances. This underestimation comes from the erroneous assumption that radial displacements driven by magnetic field disturbances are statistically independent from radial displacements driven by induced electric fields while in fact both displacements are proportional to each other. Fei et al.'s approach is similar to Fälthammar's approach in that they both analyze radial diffusion by pieces, depending on the nature of the driver. Yet, the Fokker-Planck equation requires only one radial diffusion coefficient to characterize statistically a trapped radiation belt population cross drift shell motion. Thus, it is worth questioning the practice that consists of defining the coefficient as a sum of independent contributions. In addition, both theoretical models rely on the assumption that the background magnetic field is primarily dipolar, leading to flawed estimates. To overcome these limitations and to improve radial diffusion quantification, I use a general formulation for the variation of the third adiabatic invariant (1) to describe how to compute a radial diffusion coefficient in the most general way and (2) to highlight the assumptions that need to be questioned.
我简要回顾、比较并对比了迄今为止对径向扩散研究产生重大影响的两篇理论著作,即法尔塔马尔(1965年,https://doi.org/10.1029/JZ070i011p02503)的著作以及费等人(2006年,https://doi.org/10.1029/2005JA011211)的著作。利用法尔塔马尔的磁场扰动模型,我证明了费等人的公式是不正确的:在存在磁场扰动的情况下,他们对径向扩散的估计低了两倍。这种低估源于一个错误的假设,即由磁场扰动驱动的径向位移与由感应电场驱动的径向位移在统计上是相互独立的,而实际上这两种位移是成正比的。费等人的方法与法尔塔马尔的方法相似,因为他们都根据驱动因素的性质分块分析径向扩散。然而,福克 - 普朗克方程只需要一个径向扩散系数就能从统计上表征被困辐射带粒子穿过漂移壳的运动。因此,将该系数定义为独立贡献之和的做法值得质疑。此外,这两种理论模型都依赖于背景磁场主要是偶极场的假设,这导致了有缺陷的估计。为了克服这些局限性并改进径向扩散的量化,我使用了第三绝热不变量变化的一般公式:(1)描述如何以最一般的方式计算径向扩散系数;(2)强调需要质疑的假设。