The Statistical Mechanics of Ideal Magnetohydrodynamic Turbulence and a Solution of the Dynamo Problem

Fluids Pub Date : 2024-02-12 DOI:10.3390/fluids9020046
J. Shebalin
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Abstract

We review and extend the theory of ideal, homogeneous, incompressible, magnetohydrodynamic (MHD) turbulence. The theory contains a solution to the ‘dynamo problem’, i.e., the problem of determining how a planetary or stellar body produces a global dipole magnetic field. We extend the theory to the case of ideal MHD turbulence with a mean magnetic field that is alignedwith a rotation axis. The existing theory is also extended by developing the thermodynamics of ideal MHD turbulence based on entropy. A mathematical model is created by Fourier transforming the MHD equations and dynamical variables, resulting in a dynamical system consisting of the independent Fourier coefficients of the velocity and magnetic fields. This dynamical system has a large but finite-dimensional phase space in which the phase flow is divergenceless in the ideal case. There may be several constants of the motion, in addition to energy, which depend on the presence, or lack thereof, of a mean magnetic field or system rotation or both imposed on the magnetofluid; this leads to five different cases of MHD turbulence that must be considered. The constants of the motion (ideal invariants)—the most important being energy and magnetic helicity—are used to construct canonical probability densities and partition functions that enable ensemble predictions to be made.These predictions are compared with time averages from numerical simulations to test whether or not the system is ergodic. In the cases most pertinent to planets and stars, nonergodicity is observed at the largest length-scales and occurs when the components of the dipole field become quasi-stationary and dipole energy is directly proportional to magnetic helicity. This nonergodicity is evident in the thermodynamics, while dipole alignment with a rotation axis may be seen as the result of dynamical symmetry breaking, i.e., ‘broken ergodicity’. The relevance of ideal theoretical results to real (forced, dissipative) MHD turbulence is shown through numerical simulation. Again, an important result is a statistical solution of the ‘dynamo problem’.
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理想磁流体动力湍流的统计力学和发电机问题的解决方案
我们回顾并扩展了理想的、均质的、不可压缩的磁流体动力学(MHD)湍流理论。该理论包含 "发电机问题 "的解决方案,即确定行星或恒星体如何产生全局偶极磁场的问题。我们将这一理论扩展到平均磁场与旋转轴对齐的理想 MHD 湍流情况。我们还以熵为基础发展了理想 MHD 湍流的热力学,从而扩展了现有理论。通过对 MHD 方程和动力学变量进行傅里叶变换,建立了一个数学模型,从而产生了一个由速度场和磁场的独立傅里叶系数组成的动力学系统。这个动力学系统有一个很大但有限维的相空间,在理想情况下,相流是无发散的。除能量外,还可能存在多个运动常数,这些常数取决于磁流体是否存在平均磁场或系统旋转,或两者兼而有之;这导致必须考虑五种不同的 MHD 湍流情况。这些预测与数值模拟的时间平均值进行比较,以检验系统是否具有遍历性。在与行星和恒星最相关的情况下,在最大长度尺度上观察到了非遍历性,当偶极子场的分量变得准稳态,偶极子能量与磁螺旋成正比时,就会出现非遍历性。这种非极性在热力学中是显而易见的,而偶极子与旋转轴的对齐可被视为动力学对称性破缺的结果,即 "破缺极性"。通过数值模拟显示了理想理论结果与真实(强迫、耗散)MHD 湍流的相关性。同样,一个重要的结果是 "动力学问题 "的统计解。
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