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Abstract. COMPASS-D is a compact, adaptable, D-shaped tokamak equipped
with powerful heating (ECRH) and current drive (LHCD/ECCD) systems allowing
access to both H-mode (ELMy and ELM-free) and quasi-stationary high beta
regimes under conditions of dominant electron heating (
Te > Ti),
negligible external momentum input and no central fuelling. Control and
avoidance of neo-classical tearing modes (NTMs) has enabled quasi-stationary
high beta (
2,
> 1) discharges to be sustained
for sim 20 energy confinement times and a duration corresponding to 20%
of that of a nominal ITER discharge, when normalised to the current
diffusion time. Controlled seeding of NTMs by external application of
resonant magnetic perturbations has enabled NTM onset criteria to be
carefully explored and compared with theory; observed island evolutions
follow theoretical expectations. Off-axis lower hybrid current drive (LHCD)
has been reliably used to completely stabilise NTMs in high beta discharges.
Detailed modelling has shown that the stabilising effect is consistent with
a reduction in the stability index
, although other stabilisation
mechanisms may also contribute. High frequency energetic particle driven
instabilities (
400kHz), which exhibit frequency-sweeping (`chirping'),
have, for the first time, been observed with high power ECRH as the sole
source of auxiliary heating.
IAEA 2001