Jeffersson A. Agudelo Rueda
We use 3D fully kinetic particle-in-cell simulations to study the spontaneous formation of magnetic reconnection as a self-consistent component of the turbulent cascade under solar-wind-like conditions. We simulate anisotropic decaying Alfvénic turbulence created by counter-propagating Alfvén waves. The initial wavevector anisotropy is consistent with critical-balance theory. We observe the creation of small-scale current-density structures such as current filaments and current sheets as well as the formation of magnetic flux ropes as part of the turbulent cascade. We develop and apply a new set of indicators to find reconnection regions in 3D particle-in-cell simulations. We observe the spontaneous creation of reconnection events in the simulation domain and we analyse one of the reconnection events associated with a twisted flux rope in detail. This event is highly dynamic and asymmetric. We study the plasma bulk quantities near and through the reconnection region and find agreement with reconnection exhausts in the solar wind.
3D magnetic reconnection is fundamentally different from 2D. Therefore, we propose a set of indicators to find reconnection sites in 3D. Our indicators are: C1) High Current-density structures; C2) Non-zero parallel electric fields; C3) Heated particles; C4) Fast ions and electrons and C5) Strong gradients in at least one component of the magnetic field and magnetic null regions. Figure 4 visualises our set of indicators in a subset of our simulation box. This figure shows some regions that satisfy C1, C3, C4, and C5 as well as the presence of a highly twisted magnetic flux rope and a magnetic flux tubes. The white circle marks the reconnection region where 4 of the 5 indicators are present. Since the electric field is highly sensitive to the particle noise due to the finite number of particles, the application of the indicator C2 in 3D PIC simulations is rather limited. Using our indicators, we identify spontaneous formation of reconnection events. In particular we study one in which a highly twisted magnetic flux rope breaks and reconnects with the surrounding magnetic tubes. Afterwards, we study the bulk ion velocity and the magnetic field measured along a 1D trajectory passing through and near the reconnection region. Figure 5 shows the cartesian components and magnitude of the ion velocity and magnetic field. We observe the presence of slow-mode-polarised fluctuations, rotations in the magnetic field and changes in the sign of the correlation between magnetic field and ion velocity consistent with reconnection exhausts observed in the solar wind.
To summarise, we establish a set of indicators for magnetic reconnection in 3D PIC simulations. We observe the spontaneous onset of 3D magnetic reconnection in a PIC simulation of decaying Alfvénic turbulence. The profiles of ion speed and magnetic field are consistent with reconnection events in the solar wind. Our results can be compared with measurements made by PSP and Solar Orbiter.