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

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donate electrons. The redox potential is positive or high in strongly oxidizing<br />

systems <strong>and</strong> negative or low in strongly reducing systems. Some <strong>of</strong> the common<br />

redox potentials encountered in environmental conditions are presented in Table<br />

5 (Essington, 2004; Bohn et al., 1985):<br />

Table 5. Reduction reactions <strong>and</strong> redox potential for general environmental<br />

conditions.<br />

Reduction Reactions Measured Redox Potential<br />

(V)<br />

O2 → H2O 0.6 – 0.4<br />

NO3 → NO 2- 0.5 – 0.2<br />

MnO2 → Mn 2+ 0.4 – 0.2<br />

FeOOH → Fe 2+ 0.3 – 0.1<br />

SO4 →HS - 0.0 – - 0.15<br />

2H+ → H2<br />

- -<br />

0.15 – 0.22<br />

R → CH4<br />

- -<br />

0.15 – 0.22<br />

In general, for a species to become oxidized, an electron from another species<br />

possessing a higher oxidation state needs to be transferred. Polycyclic aromatic<br />

hydrocarbons have high oxidation states (see Table 6) due to their unique<br />

chemistry previously described. For reference, stable humic acids found in soils<br />

have oxidation potentials near 0.3 – 0.4 V (Stevenson, 1994). Few nonenzymatic<br />

naturally occurring molecules have oxidation potentials that exceed<br />

the oxidation potential <strong>of</strong> <strong>PAH</strong>s. The most common class <strong>of</strong> reactants which<br />

possess oxidation potentials exceeding those <strong>of</strong> the <strong>PAH</strong>s is free radicals. Free<br />

radicals contain an unpaired electron, creating a species having a very high<br />

affinity for electrons (Silberberg, 2006). This leads to very reactive, non-specific<br />

oxidizers, capable <strong>of</strong> attacking benzene rings. (Ferrarese et al., 2008).<br />

33

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