A Model of Energetic Ion Effects on Pressure Driven Tearing Modes in Tokamaks

TL;DR

This paper models how energetic trapped ions influence pressure-driven tearing modes in tokamaks, showing that shear profiles determine whether ions stabilize or destabilize these instabilities, aligning with experimental observations.

Contribution

It introduces a reduced model incorporating ion orbit effects and magnetic shear to explain the stabilizing or destabilizing influence of energetic ions on tearing modes.

Findings

Energetic ions stabilize modes in regions of positive shear.

Inner core low/reversed shear can drive mode instability.

Results align with experimental and simulation observations.

Abstract

The effects that energetic trapped ions have on linear resistive magnetohydrodynamic (MHD) instabilities are studied in a reduced model that captures the essential physics driving or damping the modes through variations in the magnetic shear. The drift-kinetic orbital interaction of a slowing down distribution of trapped energetic ions with a resistive MHD instability is integrated to a scalar contribution to the perturbed pressure, and entered into an asymptotic matching formalism for the resistive MHD dispersion relation. Toroidal magnetic field line curvature is included to model trapping in the particle distribution, in an otherwise cylindrical model. The focus is on a configuration that is driven unstable to the m/n = 2/1 mode by increasing pressure, where m is the poloidal mode number and n the toroidal. The particles and pressure can affect the mode both in the core region where there can be low and reversed shear and outside the resonant surface in significant positive shear. The results show that the energetic ions damp and stabilize the mode when orbiting in significant positive shear, increasing the marginal stability boundary. However, the inner core region contribution with low and reversed shear can drive the mode unstable. This effect of shear on the energetic ion pressure contribution is found to be consistent with the literature. These results explain the observation that the 2/1 mode was found to be damped and stabilized by energetic ions in {\delta}f - MHD simulations of tokamak experiments with positive shear throughout, while the 2/1 mode was found to be driven unstable in simulations of experiments with weakly reversed shear in the core. This is also found to be consistent with related experimental observations of the stability of the 2/1 mode changing significantly with core shear.