<p>Sorption-desorption hysteresis (SDH) may control distributions
of chemicals between diverse environmental phases, including soils and
sediments. Formation of metastable states caused
by pore deformation or inelastic swelling of a sorbent and their
persistence during desorption were considered in the literature as one reason
for "true" SDH. Such metastable states persisting during desorption lead
to the lack of closure of sorption-desorption loop at non-zero sorbate concentrations,
which is often observed in soil and environmental literature. Also, SDH was often characterized using single-point desorption isotherms
(DIs) combining sorbed states reached during single desorption steps started
from different points along a sorption isotherm (SI). The objective of this
contribution is to demonstrate how the single-point DIs could be used to
characterize SDH in liquid phase sorption experiments in terms of Gibbs free
energy. This free energy is accumulated in some non-relaxed sorbed states
belonging to DI as compared with the states of the same composition (sorbed
concentration) belonging to SI. Using the literature
data on SIs and single-point DIs of some polycyclic aromatic hydrocarbons and
pesticides on soils and sediments, it is shown how these
extra free energies could be obtained and how they could change in the selected
sorbate-sorbent systems. When the extent of SDH decreases with increasing
solute concentration, these additional free energies decline. They may remain
constant or even increase, suggesting in the latter case that a larger work is
needed to perturb a sorbent structure at higher sorbed concentrations. This paper
proposes a novel approach for quantifying and understanding liquid phase SDH in
the cases when a thermodynamic justification is sought, and, therefore, it advances
the ability to predict the fate and activity of multiple chemicals in typical soil/sediment
environments. </p><p><br></p>