Abstract

In this article we aim to investigate the kinetic turbulence in a reconnecting current sheet (RCS) with X- and O-nullpoints and to explore its link to the features of accelerated particles. We carry out simulations of magnetic reconnection in a thin current sheet with 3D magnetic field topology affected by tearing instability until the formation of two large magnetic islands using particle-in-cell (PIC) approach. The model utilizes a strong guiding field that leads to the separation of the particles of opposite charges, the generation of a strong polarization electric field across the RCS, and suppression of kink instability in the “out-of-plane” direction. The accelerated particles of the same charge entering an RCS from the opposite edges are shown accelerated to different energies forming the “bump-in-tail” velocity distributions that, in turn, can generate plasma turbulence in different locations. The turbulence-generated waves produced by either electron or proton beams can be identified from the energy spectra of electromagnetic field fluctuations in the phase and frequency domains. From the phase space analysis we gather that the kinetic turbulence may be generated by accelerated particle beams, which are later found to evolve into a phase-space hole indicating the beam breakage. This happens at some distance from the particle entrance into an RCS, e.g. about 7di (ion inertial depth) for the electron beam and 12di for the proton beam. In a wavenumber space the spectral index of the power spectrum of the turbulent magnetic field near the ion inertial length is found to be −2.7 that is consistent with other estimations. The collective turbulence power spectra are consistent with the high-frequency fluctuations of perpendicular electric field, or upper hybrid waves, to occur in a vicinity of X-nullpoints, where the Langmuir (LW) can be generated by accelerated electrons with high growth rates, while further from X-nullponts or on the edges of magnetic islands, where electrons become ejected and start moving across the magnetic field lines, Bernstein waves can be generated. The frequency spectra of high- and low-frequency waves are explored in the kinetic turbulence in the parallel and perpendicular directions to the local magnetic field, showing noticeable lower hybrid turbulence occurring between the electron’s gyro- and plasma frequencies seen also in the wavelet spectra. Fluctuation of the perpendicular electric field component of turbulence can be consistent with the oblique whistler waves generated on the ambient density fluctuations by intense electron beams. This study brings attention to a key role of particle acceleration in generation kinetic turbulence inside current sheets.

Highlights

  • IntroductionThe processes of magnetic reconnection are often observed during eruptive events in the Sun (flares and coronal mass ejections (CMEs)) (Antiochos et al, 1994; Antiochos, 1998; Vilmer et al, 2011; Zharkova et al, 2011; Benz, 2017), heliospheric current sheet (Zharkova & Khabarova, 2012; Zank et al, 2014; Khabarova et al, 2015, 2017), and Earth magnetosphere (Øieroset et al, 2002; Angelopoulos et al., 2008; Chen et al, 2008)

  • The goal of the current research is to explore kinetic turbulence generated by accelerated particles in reconnecting current sheets with multiple X-an O-nullpoints based on the specifics of particle acceleration on 3D magnetic field topologies

  • To understand the physical nature of the turbulence generated inside reconnecting current sheet (RCS) with magnetic islands, let us use the models described in our previous papers (Xia & Zharkova, 2018; 2020), which compared particle acceleration in a single X-nullpoint and in coalescent and squashed magnetic islands

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Summary

Introduction

The processes of magnetic reconnection are often observed during eruptive events in the Sun (flares and coronal mass ejections (CMEs)) (Antiochos et al, 1994; Antiochos, 1998; Vilmer et al, 2011; Zharkova et al, 2011; Benz, 2017), heliospheric current sheet (Zharkova & Khabarova, 2012; Zank et al, 2014; Khabarova et al, 2015, 2017), and Earth magnetosphere (Øieroset et al, 2002; Angelopoulos et al., 2008; Chen et al, 2008). The recent space observations of current sheets in the magnetosphere and heliosphere (Fujimoto & Sydora, 2008; Zhou et al, 2009; Huang et al, 2016; Pucci et al, 2017; Eastwood et al, 2018; Phan et al, 2020) and 2D/3D full kinetic and Hall-MHD simulations (Daughton et al, 2004; Matthaeus & Velli, 2011; Roytershteyn et al, 2012; Boldyrev et al, 2013; Franci et al, 2017; Loureiro & Boldyrev, 2017; Papini et al, 2019; Pezzi et al, 2021) had already pointed to a link between reconnection and turbulence. At larger scales (low frequencies), there is the characteristic inertial range of the turbulent cascade, while below ion scales the turbulent spectra show a clear power law with spectral indices close to −2.7–2.8

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