The chemical release rates from a field-contaminated sediment (Lake Charles
, LA) using Tenax desorption were studied. Two dichlorobenzenes (m-, p-), h
exachlorobutadiene, and hexachlorobenzene were investigated. Contrary to re
ports that sorption rates are inversely related to K-OW, the slow desorptio
n rates were found to be similar for the four compounds. The data were mode
led by a two-compartment irreversible adsorption and radial diffusion model
. Desorption kinetics from the first irreversible compartment can be modele
d by radial diffusion and assume an irreversible adsorption constant and so
il tortuosity of 4.3. The desorption half-life is approximately 2-7 days. D
esorption from the second irreversible compartment is very slow (half-life
of approximately 0.32-8.62 years) presumably caused by entrapment in soil o
rganic matter that increases the constrictivity of the solid phase to chemi
cal diffusion. From the kinetic data, it is deduced that the diffusion pore
diameter of the second irreversible compartment is approximately equal to
the critical molecular diameter. The mass of chemicals in this highly const
rictive irreversible compartment is approximately one-fourth of the maximum
irreversible, or resistant, compartment. The slow kinetics observed in thi
s study add additional support to the notion that the irreversibly sorbed c
hemicals are 'benign' to the environment. (C) 2000 Elsevier Science Ltd. Al
l rights reserved.