Extreme heating of minor ions in imbalanced solar-wind turbulence

TL;DR

This study demonstrates that imbalanced Alfvénic turbulence in the solar wind leads to extreme, non-thermal ion heating and distinct wave signatures, emphasizing the importance of turbulence imbalance in solar wind models.

Contribution

The paper introduces a hybrid-kinetic simulation showing how the helicity barrier in imbalanced turbulence causes unique ion heating and wave features not present in balanced turbulence.

Findings

Development of a helicity barrier in imbalanced turbulence

Observation of oblique ion-cyclotron-wave heating signatures

Enhanced proton-to-electron heating ratios and anisotropic ion temperatures

Abstract

Minor ions in the solar corona are heated to extreme temperatures, far in excess of those of the electrons and protons that comprise the bulk of the plasma. These highly non-thermal distributions make minor ions sensitive probes of the underlying collisionless heating processes, which are crucial to coronal heating and the creation of the solar wind. The recent discovery of the "helicity barrier" offers a mechanism where imbalanced Alfv\'enic turbulence in low-beta plasmas preferentially heats protons over electrons, generating high-frequency, proton-cyclotron-resonant fluctuations. We use the hybrid-kinetic particle-in-cell code, Pegasus++, to drive imbalanced Alfv\'enic turbulence in a 3D low-beta plasma with additional passive ion species, He$^{2+}$ and O$^{5+}$. A helicity barrier naturally develops, followed by clear phase-space signatures of oblique ion-cyclotron-wave heating and Landau-resonant heating from the imbalanced Alfv\'enic fluctuations. The former results in characteristically arced ion velocity distribution functions, whose non-bi-Maxwellian features are shown by linear ALPS calculations to be critical to the heating process. Additional features include a steep transition-range electromagnetic spectrum, the presence of ion-cyclotron waves propagating in the direction of imbalance, significantly enhanced proton-to-electron heating ratios, anisotropic ion temperatures that are significantly more perpendicular with respect to magnetic field, and extreme heating of heavier species in a manner consistent with empirically derived mass scalings informed by measurements. None of these features are realized in an otherwise equivalent simulation of balanced turbulence. If seen simultaneously in the fast solar wind, these signatures of the helicity barrier would testify to the necessity of incorporating turbulence imbalance in a complete theory for the evolution of the solar wind.