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Quasilinear theory for inhomogeneous plasma

Published online by Cambridge University Press:  09 August 2022

I.Y. Dodin*
Affiliation:
Princeton Plasma Physics Laboratory, Princeton, NJ 08543, USA Department of Astrophysical Sciences, Princeton University, Princeton, NJ 08544, USA
*
Email address for correspondence: idodin@princeton.edu
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Abstract

This paper presents quasilinear theory (QLT) for a classical plasma interacting with inhomogeneous turbulence. The particle Hamiltonian is kept general; for example, relativistic, electromagnetic and gravitational effects are subsumed. A Fokker–Planck equation for the dressed ‘oscillation-centre’ distribution is derived from the Klimontovich equation and captures quasilinear diffusion, interaction with the background fields and ponderomotive effects simultaneously. The local diffusion coefficient is manifestly positive-semidefinite. Waves are allowed to be off-shell (i.e. not constrained by a dispersion relation), and a collision integral of the Balescu–Lenard type emerges in a form that is not restricted to any particular Hamiltonian. This operator conserves particles, momentum and energy, and it also satisfies the $\smash {H}$-theorem, as usual. As a spin-off, a general expression for the spectrum of microscopic fluctuations is derived. For on-shell waves, which satisfy a quasilinear wave-kinetic equation, the theory conserves the momentum and energy of the wave–plasma system. The action of non-resonant waves is also conserved, unlike in the standard version of QLT. Dewar's oscillation-centre QLT of electrostatic turbulence (Phys. Fluids, vol. 16, 1973, p. 1102) is proven formally as a particular case and given a concise formulation. Also discussed as examples are relativistic electromagnetic and gravitational interactions, and QLT for gravitational waves is proposed.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.
Copyright
Copyright © The Author(s), 2022. Published by Cambridge University Press
Figure 0

Table 1. Interpretation of the individual terms in (7.87) and (7.89). The wave energy–momentum is understood as the canonical (‘Minkowski’) energy–momentum, which must not be confused with the kinetic (‘Abraham’) energy–momentum (Dewar 1977; Dodin & Fisch 2012). Whether the terms with $\smash {\varDelta _s F_s}$ should be attributed to OCs or to the wave is a matter of convention, because $\smash {\varDelta _s F_s}$ scales linearly both with $\smash {F_s}$ and with $\smash {J}$. In contrast, the wave energy density is defined unambiguously as $\smash {\mathcal {E}_s \doteq \int \mathrm {d}{\boldsymbol {p}}\,H_{0s} F_s}$ and does not contain $\smash {\varDelta _s}$. This is because $\smash {\int \mathrm {d}{\boldsymbol {p}}\,\varDelta _s F_s}$ is a part of the wave energy density $\smash {\mathcal {E}_{\text {w}}}$ (Dodin & Fisch 2010a). Similarly, $\smash {\int \mathrm {d}{\boldsymbol {p}}\,(\partial _{{\boldsymbol {v}}_s}\varDelta _s) F_s}$ is a part of the wave momentum density (Dodin & Fisch 2012).