We hypothesized that retarded diffusion in coatings
controls
the rate of sorption of hydrophobic organic compounds
(HOCs) on quartzitic aquifer sands. Microscopic
examination
of three sands was used to quantify the coating
thicknesses.
With measures of the coatings' organic contents and
porosities, we predicted the relative sorption rates for
(a)
multiple HOCs on one sand and (b) one HOC with three
sands. The predicted relative rates and equilibrium
coef
ficients were assessed using observations of HOC transport
through short sand columns operated at varying flow rates.
We found that the column K
d values were
always much
less than predicted from
K
oc
f
oc or observed in
batch tests.
This suggests that diagenetically produced sorbents
may
include organic matter that is completely inaccessible for
HOC sorption; procedures that disaggregate these sands
could expose organic matter that does not sorb HOCs in the
environment. Second, by modifying our retarded
diffusion
expectations with the inferred fraction of available
organic carbon, f
avail, all observed sorption
rates were
consistent (within a factor of 4) with k
r ≈
0.001D
aq/δ2(1
+
K
oc
f
avail),
where k
r is the desorption rate
constant, D
aq is the HOC's aqueous diffusivity,
δ is the coating
thickness,
is the ratio of solids-to-water in the
coatings,
is the organic carbon content of the coating
solids, and all other factors affecting sorption rates
(e.g.,
tortuosity) were set equal to 0.001. Since oxide
coatings
are ubiquitous in aquifer sands, the model described
here should have wide applicability.