Laser reflectometry has been used for the first time as an in situ real-tim
e monitor of the dissolution of the (0 0 1) face of KClO3 crystals into aqu
eous solution. During the dissolution process the reflected light was subje
ct to constructive and destructive interference caused by the movement of c
rystal boundaries. This produced Fabry-Perot oscillations similar to the wi
dely exploited phenomenon used in the laser reflectometry-based metrology o
f semiconductor surfaces. The method is adapted and theoretical fits to the
observed data are presented. The quality of the data allows dissolution ra
tes of 100 nm s(-1) to be measured accurately. Data gained by this method w
as used to verify the concentration dependence of the dissolution rate and
confirm it as a diffusion-controlled mechanism. The hydrodynamic radius of
the diffusing ions was found to be 0.224 nm, in agreement with literature v
alues. The potential of laser reflectometry for use as an effective probe s
ensitive to changes in crystal surface morphology during dissolution has al
so been demonstrated. (C) 2000 Elsevier Science B.V. All rights reserved.