Abiotic oxidation of pentachlorophenol (PCP) by manganese(IV) oxide (MnO2) was examined in order to understand the physiochemical environment(s) where PCP oxidation occurs. An Eh−pH potentiostat was used to simulate natural groundwater environments where MnO2 (0.025 g L-1) and PCP (0.020 g L-1) suspensions were incubated from Eh −300 to 300 mV and pH 4.5 to 7.0. The pH−Eh region where maximum PCP sorption occurred corresponded to the same region where the greatest concentrations of soluble Mn(II) where measured (Eh \u3e −100 mV and pH 2 surface. A greater transformation of PCP to primarily tetrachloro-1,4-benzoquinone (p-chloranil) and smaller amounts of lesser chlorinated phenols occurred under increasing pH and Eh conditions
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