The sediment-to-air fluxes of two polycyclic aromatic hydrocarbons (phenant
hrene and pyrene) and a heterocyclic aromatic hydrocarbon (dibenzofuran) fr
om a laboratory-contaminated sediment and those of three polycyclic aromati
c hydrocarbons (naphthalene, phenanthrene, and pyrene) from three field sed
iments were investigated in experimental microcosms. The flux was dependent
on the sediment moisture content, air-filled porosity, and the relative hu
midity of the air flowing over the sediment surface. The mathematical model
predictions of flux from the laboratory-spiked sediment agreed with observ
ed values. The fluxes of compounds with higher hydrophobicity were more air
-side resistance controlled. Conspicuous differences were observed between
the fluxes from the laboratory-spiked and two of the three field sediments.
Two field sediments showed dramatic increases in mass-transfer resistances
with increasing exposure time and had significant fractions of oil and gre
ase. The proposed mathematical model was inadequate for predicting the flux
from the latter field sediments. Sediment reworking enhanced the fluxes fr
om the field sediments due to exposure of fresh solids to the air. Variatio
ns in flux from the lab-spiked sediment as a result of change in air relati
ve humidity were due to differences in retardation of chemicals on a dry or
wet surface sediment. High moisture in the air over the dry sediment in cr
eased the competition for sorption sites between water and contaminant and
increased the contaminant flux.