Can conduction induce convection? The non-linear saturation of buoyancy instabilities in dilute plasmas
Michael McCourt, Ian J. Parrish, Prateek Sharma, Eliot Quataert

TL;DR
This study investigates how anisotropic thermal conduction influences buoyancy instabilities in dilute astrophysical plasmas, revealing that the magnetothermal instability (MTI) can generate turbulence and act as a magnetic dynamo, affecting plasma dynamics.
Contribution
It demonstrates that the MTI drives turbulence and dynamo action in dilute plasmas, and clarifies the nonlinear saturation mechanisms of buoyancy instabilities, with implications for astrophysical environments.
Findings
MTI drives strong turbulence and acts as a magnetic dynamo.
The turbulent and magnetic energies contribute up to ~10% of plasma pressure.
The MTI drives a convective heat flux of about 1.5% of rho c_s^3.
Abstract
We study the effects of anisotropic thermal conduction on low-collisionality, astrophysical plasmas using two and three-dimensional magnetohydrodynamic simulations. For weak magnetic fields, dilute plasmas are buoyantly unstable for either sign of the temperature gradient: the heat-flux-driven buoyancy instability (HBI) operates when the temperature increases with radius while the magnetothermal instability (MTI) operates in the opposite limit. In contrast to previous results, we show that, in the presence of a sustained temperature gradient, the MTI drives strong turbulence and operates as an efficient magnetic dynamo (akin to standard, adiabatic convection). Together, the turbulent and magnetic energies contribute up to ~10% of the pressure support in the plasma. In addition, the MTI drives a large convective heat flux, ~1.5% of rho c_s^3. These findings are robust even in the…
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