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arXiv 1402.2640astro-ph.SR
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磁通绳作为矢势的奇点

Flux Ropes as Singularities of the Vector Potential

M Kleman

摘要:

磁通绳是磁场$\textbf{B}$的集中域。由于在这样一个区域之外的$\textbf{B}$被认为是非常小的,所以磁通绳可以被描述为外部矢量势$\textbf{A}$的奇异性的核心,其拓扑不变量是通过绳的磁通量。“拓扑”是指$\oint_C\textbf{A}\cdot\mathrm d\textbf{s}$沿着围绕磁通绳的任何回路$C$测量相同的恒定磁通$Φ$。电流强度是该理论的另一个不变量,但不是拓扑的。我们表明,在这个理论框架中,线性无力场(LFFF)的Lundquist模型和非线性(NLFFF)的Gold-Hoyle模型的磁通绳表现出稳定的解决方案,分布在量子化层的能量增加(无限数量的层在第一种情况下,只有一个层在第二种情况下),每个层是由一组连续的稳定状态。最低的LFFF地层和独特的NLFFF地层在数值上彼此接近,并且以合理的精度匹配航天器穿越磁云收集的数据。其他LFFF层与这些数据完全不匹配。在现阶段,还不可能声称哪种模型更适合磁云数据。我们还详细分析了合并属于同一层的管,与磁螺旋度的守恒,和过渡的一个管从一个层到另一个,它不守恒磁螺旋度。

英文摘要:

A flux rope is a domain of concentration of the magnetic field $\textbf{B}$. Insofar as $\textbf{B}$ outside such a domain is considered as vanishingly small, a flux rope can be described as the core of a singularity of the outer vector potential $\textbf{A}$, whose topological invariant is the magnetic flux through the rope. By 'topological' it is meant that $\oint_C\textbf{A}\cdot\mathrm d\textbf{s}$ measures along any loop $C$ surrounding the flux rope the same constant flux $Φ$. The electric current intensity is another invariant of the theory, but non-topological. We show that, in this theoretical framework, the linear force-free field (LFFF) Lundquist model and the non-linear (NLFFF) Gold-Hoyle model of a flux rope exhibit stable solutions distributed over quantized strata of increasing energies (an infinite number of strata in the first case, only one stratum in the second case); each stratum is made of a continuous set of stable states. The lowest LFFF stratum and the unique NLFFF stratum come numerically close one to the other, and match with a reasonable accuracy the data collected by spacecrafts travelling across magnetic clouds. The other LFFF strata do not match these data at all. It is not possible at this stage to claim which model fits better the magnetic cloud data. We also analyze in some detail the merging of tubes belonging to the same stratum, with conservation of the magnetic helicity, and the transition of a tube from one stratum to another one, which does not conserve magnetic helicity.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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