Remediation of PAH-Contaminated Soils and Sediments: A ...
Remediation of PAH-Contaminated Soils and Sediments: A ...
Remediation of PAH-Contaminated Soils and Sediments: A ...
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Ideal biodegradation <strong>of</strong> <strong>PAH</strong>s, where they are the sole bioavailable carbon<br />
source, can be broken into three distinct phases based on diffusion <strong>of</strong> <strong>PAH</strong> into<br />
the aqueous phase as shown in Figure 4 (Johnsen et al., 2005):<br />
I. Exponential growth phase<br />
II. Pseudo-linear growth as the dissolved <strong>PAH</strong> concentrations stabilize but<br />
microbial biomass still increases linearly<br />
III. Pseudo-stationary phase where biomass, <strong>PAH</strong> dissolution <strong>and</strong><br />
concentrations all stabilize<br />
This ideal situation is somewhat complicated in soil because <strong>of</strong> adsorption <strong>of</strong><br />
<strong>PAH</strong> to organic matter <strong>and</strong> diffusion into small pores (both mechanisms <strong>of</strong> <strong>PAH</strong><br />
sequestration). It is suspected that microbial communities in soils remain in<br />
Phase III (pseudo-stationary) as a result <strong>of</strong> the rate limiting diffusion <strong>of</strong> <strong>PAH</strong>s into<br />
the aqueous phase (Johnsen et al., 2005). Transfer to the aqueous phase is<br />
especially important for HMW hydrophobic compounds with low aqueous<br />
solubility which tend to partition to the solid phase (especially organic matter) in<br />
soils <strong>and</strong> sediments.<br />
Figure 4. Schematic diagram for microbial biomass, specific microbial growth<br />
rate, <strong>PAH</strong> dissolution rate <strong>and</strong> dissolved <strong>PAH</strong> concentration <strong>of</strong> bacterial batch<br />
grown on solid <strong>PAH</strong>s (Johnsen et al., 2005).<br />
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