Abstract
A study was conducted to determine the effects of biodegradability of nonaqueous‐phase liquids (NAPLs) and microbial competition on the biodegradation in soil of a constituent of the NAPLs. The rates of mineralization of phenanthrene dissolved in 8 mg of 2,2,4,4,6,8,8‐heptamethylnonane (HMN), di(2‐ethylhexyl) phthalate (DEHP), or pristane per g of soil were faster than the rates when the compound was dissolved in hexadecane or dodecane. Addition of inorganic N and P to the soil increased the mineralization rate in the first two but not the last two NAPLs. N and P addition did not enhance mineralization of phenanthrene when added in 500 μg of hexadecane, pristane, or HMN per g of soil. Hexadecane was rapidly degraded, pristane was slowly metabolized, DEHP was still slower, and HMN was not mineralized in the test period. Mixing the soil stimulated mineralization of phenanthrene dissolved in HMN but not in hexadecane. Mineralization of phenanthrene dissolved in HMN was the same if the gas phase contained 21%, 2.1%, or traces of O~2~. In contrast, the biodegradation of phenanthrene dissolved in hexadecane, although the same at 21 and 2.1% O~2~, was not observed if traces of O~2~ were present. The mineralization was slower in unshaken soil–water mixtures if phenanthrene was added in hexadecane than in HMN or pristane, but the rates with the 3 NAPLs were increased by shaking the suspensions. We suggest that the biodegradability of major components of NAPLs and microbial competition for N, P, or O~2~ will have a major impact on the rate of transformation of minor constituents of NAPLs.