Batch and column experiments were conducted to assist in elucidation of the
mechanism and rates of slow diffusion of 1,2,4-trichlorobenzene into Borde
n sand. Batch rate experiments were;conducted at three concentration levels
, and a full isotherm was developed over 550 d. The equilibrium isotherm sh
owed significant nonlinearity (Freundlich exponent = 0.75). Three column ex
periments were conducted-two at low velocity (each at a different input con
centration) and one at high velocity. The data were analyzed with four diff
erent models; the two most, successful are described in detail here. These
two models divided sorption between instantaneously equilibrating and diffu
sion-limited domains, with either a linear or nonlinear sorption isotherm a
ssumed for the instantaneously equilibrating fraction of sorption sites. Ei
ther model could simulate any single dataset by adjustment of two parameter
s; however, no single parameter set could simulate all data sets. The model
with a linearly sorbing instantaneous fraction described the batch data be
tter than the model with a nonlinearly sorbing instantaneous fraction; howe
ver, a nonlinearly sorbing instantaneous fraction described the slow column
experiments much better than a linearly sorbing instantaneous fraction. Th
e high-flow-rate column experiment indicated that the assumed instantaneous
fraction is actually influenced by-rate limitations, suggesting that more
complex models are needed in order to simulate this shorter time scale beha
vior. Overall, our work illustrates how one needs to include a wide variety
of experimental conditions in order to fully test the complex set of sorpt
ion equilibrium and rate mechanisms that are present in natural solids.