Abstract
This paper surveys theory issues associated with inducing convective cells through divertor tile biasing in a tokamak to broaden the scrape-off layer (SOL). The theory is applied to the Mega-Ampere Spherical Tokamak (MAST), where such experiments are planned. Criteria are presented for achieving strong broadening and for exciting shear-flow turbulence in the SOL; these are shown to be attainable in practice. It is also shown that the magnetic shear present in the vicinity of the X-point is likely to confine the potential perturbations to the divertor region below the X-point, with little impact on the main SOL. The current created by the biasing and the associated heating power are found to be modest.
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