Influence of environmental factors on denitrification in sediment contaminated with JP-4 jet fuel

Abstract

In 1975, the loss of approximately 83,000 gallons of JP-4 grade jet fuel resulted in contamination of the shallow aquifer near North Charleston, South Carolina. To identify those factors likely to influence microbial activity under denitrifying conditions, we examined the fate of amended NO 3 , the effect of pH, NO 3 , and PO 4 on denitrification, and the variability of denitrification in sediments collected at the site. Denitrification (N 2 O-N production) accounted for 98% of the depletion of NO 3 -N under anaerobic conditions. Both carbon mineralization and denitrification rates increased asymptotically with increasing NO 3 to a maximum at approximately 1 mM NO 3 . Addition of up to 1 mM PO 4 did not significantly increase N 2 O and CO 2 production. Denitrification rates were at least 38% lower at p H = 4 than observed at p H = 7. Comparison of samples with differing degrees of hydrocarbon contamination indicated that at least a tenfold variation in sediment denitrification occurs at the North Charleston site.