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Long Term Vortex Flow Evolution around a Magnetic Island in Tokamaks
1Department of Nuclear Engineering, Seoul National University, Seoul 151-742, Korea.
Physical Review Letters
|June 17, 2022
Summary
In tokamak plasmas, vortex flow in magnetic islands initially settles to a neoclassical level. Over time, it shifts to a dipolar flow, enabling turbulence transport across the island.
Area of Science:
- Plasma Physics
- Fusion Energy Research
- Fluid Dynamics
Background:
- Magnetic islands are crucial in tokamak plasmas, influencing confinement and stability.
- Understanding vortex flow dynamics within these islands is key to predicting plasma behavior.
Purpose of the Study:
- To analyze the evolution of vortex flow within magnetic islands in collisionless tokamak plasmas.
- To investigate the impact of finite island width and toroidicity on flow structures.
Main Methods:
- Gyrokinetic analysis of plasma behavior.
- Examination of flow evolution over short (ωD t < 1) and long (ωD t > 1) timescales.
Main Results:
- Short-term: Monopolar vortex flow relaxes to a neoclassical residual level, enhanced by finite island width.
- Long-term: Toroidicity breaks helical symmetry, evolving flow to a dipolar zonal-vortex mixture.
- This mixture creates flow shear layers, enabling turbulence advection across the magnetic island.
Conclusions:
- Small magnetic islands (w≲qρTi/s) favor the formation of the dipolar zonal-vortex mixture.
- Larger islands tend to maintain the simpler monopolar vortex flow.
- The dipolar flow mixture facilitates cross-island turbulence transport, impacting plasma confinement.
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