In this study we investigated the kinetics of Zn sorption and desorption us
ing a short column or thin disk method. The method is based on continuous n
ow through a thin soil layer (1 mm) where the effluent was collected using
a fraction collector. Two soils were used: a Windsor soil and Mahan soil, B
reakthrough results (BTCs) for different now velocities indicated that Zn s
orption is instantaneous and equilibrium retention is dominant when a pulse
of Zn with a concentration of 2.62 x 10(-5) M is applied. However, based o
n now interruption, time-dependent Zn sorption-desorption processes were mo
st pronounced when the applied Zn pulse concentration was two orders of mag
nitude lower (2.51 x 10(-7) M), This confirms earlier findings of concentra
tion-dependent kinetics from batch experiments on Windsor soil (Hinz et al,
, 1992), The removal of organic matter and iron oxide, based on peroxide an
d peroxide/dithionite-treatments, resulted in doubling and quadrupling Zn r
etention, respectively, compared with the untreated Windsor soil. Differenc
es between the untreated, peroxide-, and peroxide/dithionite-treated Windso
r soils were most pronounced at low input Zn concentrations, suggesting tha
t more specific sites became available as a result of the different treatme
nts. At high input Zn concentrations, increases of specific sites may not b
e significant. For the treated soil, stronger sorption and desorption kinet
ic behavior was exhibited compared with the untreated soil. Diffusion into
soil minerals or surface-controlled reactions may cause such behavior.