Interaction of magnetic islands with turbulent electron temperature fluctuations in DIII-D and in GENE nonlinear gyrokinetic simulations
L. Bardóczi, C. Sung, A. Bañón Navarro, T. L. Rhodes, Troy Carter, F. Jenko
Abstract
Open-access reader
L. Bardóczi, C. Sung, A. Bañón Navarro, T. L. Rhodes, Troy Carter, F. Jenko
Abstract
Open-access reader
Abstract We present localized measurements of interactions between neoclassical tearing modes (NTMs) and turbulent electron temperature fluctuations ( T ˜ e ) in the expected k θ ρ s = 0–0.5 wave-number range of the ion temperature gradient (ITG) instability measured via correlation electron cyclotron emission ( k θ and ρ s are the poloidal wave-number and ion-sound Larmor radius, respectively). Comparison to GENE gyrokinetic simulations, shows qualitative agreement with T ˜ e being reduced (increased) inside (outside) of the islands due to modified local gradients, and T ˜ e being higher (lower) in the region outside the island where lower (higher) flow shear is expected due to radially asymmetric island shape. These results are consistent with previously reported modifications of long and intermediate wavelength turbulent density fluctuations and cross-field electron thermal diffusivity reduction at the O-point of magnetic islands. Interestingly, a 30% increase of T ˜ e is detected at the NTM rational surface when the island width is a few times ρ s , which is replicated by GENE through zonal flow damping due to the destroyed magnetic field topology of the NTM rational surface.
OpenAlex reports 9 citations for this work. Citation counts describe recorded attention and do not establish research quality.
A contribution statement is not available in the OpenAlex record.
Method details are not available in the OpenAlex metadata.
Findings are not separately available in the OpenAlex metadata.
Limitations are not available in the OpenAlex metadata.
Application details are not available in the OpenAlex metadata.
Abstract We present localized measurements of interactions between neoclassical tearing modes (NTMs) and turbulent electron temperature fluctuations ( T ˜ e ) in the expected k θ ρ s = 0–0.5 wave-number range of the ion temperature gradient (ITG) instability measured via correlation electron cyclotron emission ( k θ and ρ s are the poloidal wave-number and ion-sound Larmor radius, respectively). Comparison to GENE gyrokinetic simulations, shows qualitative agreement with T ˜ e being reduced (increased) inside (outside) of the islands due to modified local gradients, and T ˜ e being higher (lower) in the region outside the island where lower (higher) flow shear is expected due to radially asymmetric island shape. These results are consistent with previously reported modifications of long and intermediate wavelength turbulent density fluctuations and cross-field electron thermal diffusivity reduction at the O-point of magnetic islands. Interestingly, a 30% increase of T ˜ e is detected at the NTM rational surface when the island width is a few times ρ s , which is replicated by GENE through zonal flow damping due to the destroyed magnetic field topology of the NTM rational surface.
Key concepts: DIII-D, Turbulence, Nonlinear system, Physics, Electron, Gyrokinetics, Electron temperature, Computational physics