This paper reports on the first use of quartz crystal microbalances as
a useful diagnostic for plasma-wall interaction studies in tokamaks.
Two quartz microbalance systems were installed recently in the TdeV to
kamak. Reliable mass measurements are obtained when a correction is ap
plied to the frequency response of the crystal, owing to its temperatu
re rise during the discharges. Particle fluxes in the scrape-off layer
(SOL), perpendicular and parallel to the magnetic field lines along t
he ion drift or electron drift directions were measured. As expected,
a larger erosion rate was measured in the ion drift direction, while d
eposition was observed on the quartz surfaces facing up and facing dow
n but not facing the plasma (i.e. field lines at grazing incidence), R
adial displacement of the set-up permitted the measurement of the radi
al dependence of the erosion-deposition processes. An increase of the
plasma current induces a slight increase of the deposit thickness. A d
etachment of the plasma in the divertor doubles the thickness of the d
eposit. The quartz microbalance showed that the deposition rate is str
ongly increased for a few discharges following a disruption. This diag
nostic method is also sensitive to the atomic number of injected impur
ities.