Deposition and H-isotope retention in JET is highly asymmetric, with deposi
tion predominantly in the inner divertor, where flaking deposits form on wa
ter-cooled louvres shadowed from the plasma, The asymmetry implies drift in
the SOL of JET from outboard to inboard under normal operating conditions,
which has been measured. In order to model the amounts of deposition, assu
mptions have to be made about the transport at the inner target, Analysis o
f divertor tiles shows that material from the main chamber travels along th
e SOL to the inner divertor wall, from where carbon is preferentially remov
ed leaving a beryllium-rich film. The carbon travels to shadowed areas (suc
h as the louvres) where deposits with high H-isotope content accrue. The an
alysis indicates that chemical processes must be important. (C) 2001 JET Jo
int Undertaking. Published by Elsevier Science B.V. All rights reserved.