U.S. Geological Survey Toxic Substances Hydrology Program--Proceedings
of the Technical Meeting, Colorado Springs, Colorado, September 20-24, 1993,
Water-Resources Investigations Report 94-4015
Sorption of Polycyclic Aromatic Hydrocarbons to Aquifer Materials
Containing a Low-Organic Carbon Content from Bemidji, Minnesota
by
Joseph J. Piatt (Dept. of Soil and Water Science, Univ. of Arizona,
Tucson, AZ), Steven J. Eisenriech (Gray Freshwater Biological Institute,
Univ. of Minnesota, Navarre, MN), Debera A. Backhus (School of Public and
Environmental Affairs, Indiana Univ., Bloomington, IN), and Paul D. Capel
(U.S. Geological Survey, Navarre, MN)
Abstract
Three polycyclic aromatic hydrocarbons, naphthalene, phenanthrene, and
pyrene -- were sorbed to a single sample of aquifer material containing
a low-organic carbon content at two different temperatures, 5°C and
25°C, using batch and column experimental techniques. Controls on batch
and column techniques were incorporated to ensure that the experimental
vessels were organic-carbon free, biological and photolytic activity was
absent, and solution supernates were colloid-free. The sorptive uptake curves
indicated a two-step approach to equilibrium. The data were modelled using
a two-site sorption kinetic model. Times to equilibrium were at least 40
hours. Small increases in equilibrium distribution coefficients were observed
with decreased temperature which resulted in enthalpy of sorption values
which were consistent with a partitioning mechanism. Small decreases in
rate constants were occurred as temperature decreased. The values of the
solids/water distribution coefficients for the batch experiments were consistently
4 to 60 times larger than those obtained from the column experiments, probably
because of differences in experimental boundary conditions or to creation
of fine particles in the batch experiments that would increase the surface
area available for sorption. Although the relative effects of organic-carbon
phase sorption versus mineral phase sorption were not isolated directly,
the magnitude of the observed distribution coefficients and rate constants
are consistent with sorption controlled by the organic-carbon content of
this aquifer material.
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