首页> 外文期刊>Izvestiya. Physics of the solid earth >Weakly nonlinear stability to large-scale perturbations in convective magnetohydrodynamic systems without the α-effect
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Weakly nonlinear stability to large-scale perturbations in convective magnetohydrodynamic systems without the α-effect

机译:对流磁流体动力学系统中对大扰动的弱非线性稳定性,没有α效应

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The problem of weakly nonlinear stability with respect to large-scale perturbations in 3-D convective magnetohydrodynamic (MHD) states in which the α-effect is absent or insignificant (e.g., because the system has symmetry relative to a center or a vertical axis) is examined. It is assumed that the MHD state whose stability is studied is free from large spatiotemporal scales and is insensitive to perturbations with the same small spatial scale as in the state under study. The equations for mean perturbation fields derived by asymptotic methods generalize the standard equations of magnetohydrodynamics (the Navier-Stokes and magnetic induction equations). A combined eddy diffusion operator, generally anisotropic and not necessarily negative definite, and additional quadratic terms similar to advective terms arise in the inferred generalized equations.
机译:关于缺少α效应或α效应微不足道的3-D对流磁流体动力学(MHD)状态中的大规模扰动的弱非线性稳定性问题(例如,因为系统相对于中心或垂直轴具有对称性)被检查。假设已研究其稳定性的MHD状态没有较大的时空尺度,并且对与所研究状态相同的较小空间尺度的摄动不敏感。通过渐近方法得出的平均摄动场方程,概括了磁流体动力学的标准方程(Navier-Stokes和磁感应方程)。组合的涡流扩散算子通常是各向异性的,不一定是负定的,并且在推断的广义方程中会出现类似于对流项的其他二次项。

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