磁浮力隔音模型的自伴随性

IF 1.1 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
J. Moss, T. Wood, P. Bushby
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引用次数: 0

摘要

理想磁流体,无论完全可压缩还是不可压缩,都是一个哈密顿系统。这意味着描述任何静态扰动的方程都是自伴随的,这一事实对获得稳定性判据很有用。为了描述弱可压缩流,有许多“隔音”模型,它们通过近似控制方程来消除声波。然而,这种近似可能违反系统的哈密顿结构。在最近的一项工作中,我们介绍了一个非常一般的隔音模型,并确定了它非常接近磁浮力不稳定的线性状态的条件,这是由太阳内部的条件引起的。在目前的工作中,我们采取了一种互补的方法,通过推导线性化隔音系统自伴随的约束。我们证明了存在一组独特的自伴随隔音方程,它与完全可压缩系统保存相同的能量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Self-adjointness of sound-proof models for magnetic buoyancy
An ideal magneto-hydrodynamic fluid, whether fully compressible or incompressible, is a Hamiltonian system. This implies that the equations describing perturbations to any static state are self-adjoint, a fact that is useful in obtaining stability criteria. To describe weakly compressible flows, there are a number of “sound-proof” models that eliminate sound waves by making approximations to the governing equations. However, such approximations may violate the Hamiltonian structure of the system. In a recent work, we have introduced a very general sound-proof model and determined conditions under which it closely approximates the linear regime of magneto-buoyancy instability, motivated by conditions in the solar interior. In the present work, we take a complementary approach, by deriving constraints under which the linearised sound-proof system is self-adjoint. We show that there is a unique set of self-adjoint sound-proof equations that conserves the same energy as the fully compressible system.
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来源期刊
Geophysical and Astrophysical Fluid Dynamics
Geophysical and Astrophysical Fluid Dynamics 地学天文-地球化学与地球物理
CiteScore
3.10
自引率
0.00%
发文量
14
审稿时长
>12 weeks
期刊介绍: Geophysical and Astrophysical Fluid Dynamics exists for the publication of original research papers and short communications, occasional survey articles and conference reports on the fluid mechanics of the earth and planets, including oceans, atmospheres and interiors, and the fluid mechanics of the sun, stars and other astrophysical objects. In addition, their magnetohydrodynamic behaviours are investigated. Experimental, theoretical and numerical studies of rotating, stratified and convecting fluids of general interest to geophysicists and astrophysicists appear. Properly interpreted observational results are also published.
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