The bioavailability of hydrophobic organic chemicals decreases with aging i
n soil because of sequestration. However, assessments of the risk of exposu
re to contaminated soils are usually dependent on either chemical concentra
tions, which are measured using vigorous extraction methods, or models that
assume an equilibrium without considering the actual conditions. The objec
tive of this research was to determine the availability and desorption kine
tics of freshly added and aged naphthalene from a peat and a mineral soil;
naphthalene was desorbed into solutions with pH levels that approximate tho
se found in different gastric regions. Soil and peat samples were spiked wi
th radiolabeled and unlabeled naphthalene at 2 and 20 mu g/g and were aged
from 0 to 135 d. Desorption kinetics were determined using a simulated stom
ach solution (0.1 M NaCl, 0.1 M HCl, 0.01 M NH4Ac, pH = 1.0) and a neutral
solution (0.2 M NaCl, pH = 6.7) that represented the pH of intestinal condi
tions and most soils. Feat sorbed much more naphthalene than did soil, and
it allowed little desorption. Though both acidic and neutral extracting sol
utions could desorb naphthalene, little apparent effect of aging was observ
ed in peat, whereas desorption from soil declined markedly with aging. In a
ddition, the percentage of naphthalene that desorbed from soil was greater
for the higher incubation concentration. The desorption of naphthalene from
the pear and soil was higher into the neutral solution than into the gastr
ic solution. These results suggest that aging, exposure conditions, concent
ration effect, and organic matter content should be taken into account in p
redictive models and risk assessments.