Biodegradation of 1-naphthol in the presence of humic acid

Biodegradation of l-naphthol by a pure culture was measured in the presence (65 mg C L-1) and absence of a forest soil humic acid (HA). Experiments we re performed under nongrowth conditions and controlled ionic strength (I eq uivalent to 10 mM LiCl) at pH 8.0. I-Naphthol was allowed to react with HA under aerobic conditions in the dark for 7 days to promote sorption prior t o bacterial inoculation. During this abiotic sorption period, 3.7-12% of I- naphthol was transformed into oxidative products (naphthoquinones). At low initial I-naphthol concentrations (<2.7 mg L-1), I-naphthol mineralization (measured by (CO2)-C-14 production) decreased from 25-35% to 9-16% with HA. I-Naphthol was biodegraded to concentrations below HPLC-PDA detection limi t (0.10 mg L-1) except at the highest I-naphthol concentrations tested (>9. 0 mg L-1) with or without HA. Both abiotic and biotic l-naphthol transforma tion pathways accumulated similar products, and these products were more re calcitrant than l-naphthol. The sorption of 1-naphthol abiotic transformati on products and bacterial metabolites to HA (not I-naphthol) reduced l-naph thol mineralization.