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Remediation of PAH-Contaminated Soils and Sediments: A ...

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Table 6. Oxidation potentials for select <strong>PAH</strong>s (Dabestani <strong>and</strong> Ivanov, 1999).<br />

Compound Oxidation Potential<br />

( E ox 1/2)<br />

Acenaphthene 1.21<br />

Acenaphthylene 1.21<br />

Anthracene 1.09<br />

Benz[a]anthracene 1.18<br />

Benzo[a]pyrene 0.94<br />

Benzo[ghi]perylene 1.01<br />

Chrysene 1.35<br />

Dibenz[ah]anthracene 1.26<br />

Fluoranthene 1.45<br />

Naphthalene 1.54<br />

Phenanthrene 1.50<br />

Pyrene 1.16<br />

There are many molecules which can become free radicals <strong>and</strong> several<br />

pathways exist for their presence in natural ecosystems. The most common <strong>and</strong><br />

reactive group <strong>of</strong> free radicals is that <strong>of</strong> the oxides (Figure 6) <strong>and</strong> nitrates (NO3 • ),<br />

both <strong>of</strong> which are readily created in the troposphere by absorption <strong>of</strong> sunlight<br />

radiation (λ =290-335nm) (Arey <strong>and</strong> Atkinson, 2003). Nonbiological radical<br />

oxidation is most important for volatile <strong>PAH</strong>s or particle associated <strong>PAH</strong>s in the<br />

atmosphere because <strong>of</strong> the low concentration <strong>of</strong> free radicals in sediments <strong>and</strong><br />

their very quick reaction time (less than 1 second) time in aqueous systems.<br />

Figure 6. Common ozone reactions that occur in the atmosphere (Miller <strong>and</strong><br />

Olejnik, 2004)<br />

Nonbiological oxidation reactions induced for the purposes <strong>of</strong> <strong>PAH</strong> degradation<br />

have been accomplished by the following advanced oxidation processes (Rivas,<br />

2006; Alderman et al., 2007; Isosaari et al., 2007; Ferrarese et al., 2008):<br />

34

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