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<p>We investigate plasma turbulence generated during particle acceleration in magnetic islands within 3D Harris-type&#160;reconnecting current sheets (RCSs),using the particle-in-cell approach.&#160;&#160;RCSs with a strong guiding magnetic field &#160;ar shown to lead to&#160;separation of electrons and ions into the opposite sides from the current sheet mid-plane that significantly reduces kink instability along the guiding field direction.&#160;Particles with the same&#160;charge also have asymmetric trajectories forming&#160;two distinct populations of beams: &#8216;transit&#8217; particles, which pass through RCS from&#160;one edge to another, become strongly energised and form nearly unidirectional beams;&#160;and &#8216;bounced&#8217; particles, which are reflected from the diffusion region and move back to&#160;the same side they entered the current sheet, gaining much less energy and forming more&#160;dispersive spatial distributions. Thes&#160;transit and bounced particles form the &#8216;bump-on-tail&#8217; velocity distributions that naturally generate plasma&#160;turbulence. Using the wavelet analysis of electric and magnetic field fluctuations in the&#160;frequency domain, we identified some characteristic waves produced by particle beams.&#160;In particular, we found thre are Langmuir waves near X-nullpoints produced by two electron beam instabilities, while the presence of anisotropic temperature variations inside&#160;magnetic islands lead to whistler waves. The lower-hybrid waves are generated&#160;inside the magnetic islands, owing to the two-stream instabilities of the ions. While the&#160;high-frequency fluctuations, upper hybrid waves, or electron Bernstein waves, pile up near&#160;X-nullpoints.&#160;The results can be beneficial for&#160;understanding in-situ observations with modern space missions of energetic particles in&#160;the heliosphere.</p>
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