At. Kan et al., IRREVERSIBLE ADSORPTION OF NAPHTHALENE AND TETRACHLOROBIPHENYL TO LULA AND SURROGATE SEDIMENTS, Environmental science & technology, 31(8), 1997, pp. 2176-2185
Several unique features of sorption irreversibility have been investig
ated in this paper. Adsorption has been found to be biphasic with abou
t 30-50% of the adsorbed mass residing in the irreversibly sorbed comp
artment, until this compartment is filled, and the rest of the mass re
sides in the labile compartment. Naphthalene in the reversible compart
ment follows a linear adsorption isotherm with a normal organic carbon
-based partition coefficient. A finite fixed total compartment size is
observed for the irreversible fraction, q(max)(irr) (mu g/g), on both
natural and surrogate solids. In multiple batch adsorption/desorption
experiments, the maximum concentrations that resist desorption are q(
max)(irr) approximate to 10 mu g/g for naphthalene on Lula sediment an
d q(max)(irr) approximate to 0.36 mu g/g for 2,2',5,5'-tetrachlorobiph
enyl (2,2',5,5'-CB) on both Lula and surrogate solids. The concentrati
on in the irreversibly sorbed compartment varied with the initial naph
thalene concentration available for adsorption. In addition, the amoun
t in the irreversibly sorbed compartment increases linearly with the n
umber of adsorption steps until the maximum concentration q(max)(irr)
is reached. After the maximum concentration of the irreversibly sorbed
compartment is satisfied, the adsorption/desorption of naphtha I ene
and 2,2',5,5'-CB becomes reversible. The irreversibly sorbed compartme
nt appears to be at equilibrium with the aqueous phase when the labile
naphthalene or 2,2',5,5'-CB is removed, but the equilibrium concentra
tion is much lower than would be predicted with conventional hydrophob
ic partitioning theory. The aqueous phase concentration in equilibrium
with the irreversibly sorbed compartment is about 2-5 mu g/L for naph
thalene and 0.05-0.8 mu g/L for 2,2',5,5'-CB. Similar adsorption/desor
ption phenomena are observed with both a natural sediment and a well-c
haracterized sorrogate solid.