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Abstract This study explores the use of multiple isotopic tracers to evaluate the processes involved in nitrate attenuation in ground water. δ 15 N and δ 18 O are used to provide information about the role of denitrification on nitrate attenuation, and δ 34 S, δ 18 O, and δ 13 C are used to evaluate the role of reduced sulfur and carbon as electron donors for nitrate reduction. The focus of this study is a zone of significant NO 3 −1 attenuation occurring in a sand aquifer impacted by septic system contamination. The NO 3 −1 pattern, the ground water flow system, and changes in other chemical parameters suggest that the NO 3 −1 depletion is caused by denitrification. This is supported by the nitrate δ 15 N and δ 18 O data which both show significant isotopic enrichment as NO 3 −1 depletion proceeds along the flow path. The increase of sulfate and dissolved inorganic carbon observed in the zone of nitrate attenuation suggests that reduced sulfur in addition to carbon is also involved in denitrification. This is supported by a trend toward depleted sulfate δ 34 S and δ 18 O values in the zone of sulfate increase, which reflects the input of sulfate formed by the oxidation of biogenic pyrite present in the aquifer sediments. The trend toward depleted δ 13 values in the zone of increasing dissolved inorganic carbon reflects the input of organic carbon into this carbon pool. Chemical mass balance indicates that carbon is the dominant electron donor; however, this study demonstrates the effectiveness of using multiple isotopic tracers for providing insight into the processes affecting nitrate attenuation in ground water.
Aravena et al. (Sun,) studied this question.