In the bioremediation of low-permeability soils, pollutant and, especially,
the oxygen bioavailability are often the rate limiting steps. In cases whe
n a biopile treatment can represent an applicable technique, pretreatment o
f the excavated soil is often necessary to attain an adequate air-filled po
rosity in the soil and to avoid the presence of large soil aggregates.
The present work was performed to evaluate the influence of soil aggregate
size in the bioremediation of a silt-clay type soil contaminated by PAHs. M
icrocosms were arranged with spherical soil aggregates of different diamete
r in near water-saturation conditions, concentration of two and three aroma
tic ring PAHs, total biomass, and respiration rates were monitored. PAH con
centration profiles inside the particles were also obtained. A simple and q
uick way to estimate the critical dimension of the soil aggregates was deve
loped based on the evaluation of an oxygen penetration depth, that is, the
distance from the external surface to the aggregate core beyond which oxyge
n concentration is practically zero.
A very different time course of PAHs consumption was found in the external
layer and the inner core of the aggregates as well as in aggregates of diff
erent dimensions. The results suggest that only the 3 mm external layer of
the sphere is not limited by oxygen diffusion.