Collisionless conduction in a high-beta plasma: A collision operator for whistler turbulence

Evan L. Yerger, Matthew Walter Kunz, Archie F.A. Bott, Anatoly Spitkovsky

Research output: Contribution to journalArticlepeer-review

Abstract

The regulation of electron heat transport in high-, weakly collisional, magnetized plasma is investigated. A temperature gradient oriented along a mean magnetic field can induce a kinetic heat-flux-driven whistler instability (HWI), which back-reacts on the transport by scattering electrons and impeding their flow. Previous analytical and numerical studies have shown that the heat flux for the saturated HWI scales as. These numerical studies, however, had limited scale separation and consequently large fluctuation amplitudes, which calls into question their relevance at astrophysical scales. To this end, we perform a series of particle-in-cell simulations of the HWI across a range of and temperature-gradient length scales under two different physical set-ups. The saturated heat flux in all of our simulations follows the expected scaling, supporting the robustness of the result. We also use our simulation results to develop and implement several methods to construct an effective collision operator for whistler turbulence. The results point to an issue with the standard quasi-linear explanation of HWI saturation, which is analogous to the well-known scattering problem in the cosmic-ray community. Despite this limitation, the methods developed here can serve as a blueprint for future work seeking to characterize the effective collisionality caused by kinetic instabilities.

Original languageEnglish (US)
Article numberE20
JournalJournal of Plasma Physics
Volume91
Issue number1
DOIs
StatePublished - Jan 9 2025

All Science Journal Classification (ASJC) codes

  • Condensed Matter Physics

Keywords

  • astrophysical plasmas
  • plasma instabilities
  • plasma simulation

Fingerprint

Dive into the research topics of 'Collisionless conduction in a high-beta plasma: A collision operator for whistler turbulence'. Together they form a unique fingerprint.

Cite this