多连通域的相对磁螺旋度

David MacTaggart, Alberto Valli
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引用次数: 0

摘要

摘要磁螺旋度是理想磁流体力学(MHD)的守恒量,与磁场的拓扑结构有关,在实验室和天体物理等离子体中都得到了广泛的研究。当磁场边界上有非平凡法向分量时,螺旋度的经典定义必须用相对磁螺旋度来代替。本工作的目的是回顾相对螺旋度的各种定义,并表明它们有一个共同的起源-在多连通域的相对螺旋度的一般定义。我们证明了这个一般定义在理想MHD下是规范不变的,并且在时间上是守恒的,仅受封闭和线系边界条件的约束。文献中经常使用的其他更具体的相对螺旋度公式,是通过对磁场或其矢量势施加额外条件而得出的。
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Relative magnetic helicity in multiply connected domains
Abstract Magnetic helicity is a conserved quantity of ideal magnetohydrodynamics (MHD) that is related to the topology of the magnetic field, and is widely studied in both laboratory and astrophysical plasmas. When the magnetic field has a non-trivial normal component on the boundary of the domain, the classical definition of helicity must be replaced by relative magnetic helicity . The purpose of this work is to review the various definitions of relative helicity and to show that they have a common origin—a general definition of relative helicity in multiply connected domains. We show that this general definition is both gauge-invariant and is conserved in time under ideal MHD, subject only to closed and line-tied boundary conditions. Other, more specific, formulae for relative helicity, that are used frequently in the literature, are shown to follow from the general expression by imposing extra conditions on the magnetic field or its vector potential.
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