Fractionation of stable isotopes in perchlorate and nitrate during in situ biodegradation in a sandy aquifer
Paul B. Hatzinger A F , John Karl Böhlke B , Neil C. Sturchio C , Baohua Gu D , Linnea J. Heraty C and Robert C. Borden E
A Shaw Environmental, Inc., Lawrenceville, NJ 08648, USA.
B US Geological Survey, Reston, VA 20192, USA.
C University of Illinois at Chicago, Chicago, IL 60607, USA.
D Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA.
E North Carolina State University, Raleigh, NC 27695, USA.
F Corresponding author. Email: firstname.lastname@example.org
Environmental Chemistry 6(1) 44-52 http://dx.doi.org/10.1071/EN09008
Submitted: 15 January 2009 Accepted: 2 February 2009 Published: 3 March 2009
Environmental context. Perchlorate (ClO4–) and nitrate (NO3–) are common co-contaminants in groundwater, with both natural and anthropogenic sources. Each of these compounds is biodegradable, so in situ enhanced bioremediation is one alternative for treating them in groundwater. Because bacteria typically fractionate isotopes during biodegradation, stable isotope analysis is increasingly used to distinguish this process from transport or mixing-related decreases in contaminant concentrations. However, for this technique to be useful in the field to monitor bioremediation progress, isotope fractionation must be quantified under relevant environmental conditions. In the present study, we quantify the apparent in situ fractionation effects for stable isotopes in ClO4– (Cl and O) and NO3– (N and O) resulting from biodegradation in an aquifer.
Abstract. An in situ experiment was performed in a shallow alluvial aquifer in Maryland to quantify the fractionation of stable isotopes in perchlorate (Cl and O) and nitrate (N and O) during biodegradation. An emulsified soybean oil substrate that was previously injected into this aquifer provided the electron donor necessary for biological perchlorate reduction and denitrification. During the field experiment, groundwater extracted from an upgradient well was pumped into an injection well located within the in situ oil barrier, and then groundwater samples were withdrawn for the next 30 h. After correction for dilution (using Br– as a conservative tracer of the injectate), perchlorate concentrations decreased by 78% and nitrate concentrations decreased by 82% during the initial 8.6 h after the injection. The observed ratio of fractionation effects of O and Cl isotopes in perchlorate (ε18O/ε37Cl) was 2.6, which is similar to that observed in the laboratory using pure cultures (2.5). Denitrification by indigenous bacteria fractionated O and N isotopes in nitrate at a ratio of ~0.8 (ε18O/ε15N), which is within the range of values reported previously for denitrification. However, the magnitudes of the individual apparent in situ isotope fractionation effects for perchlorate and nitrate were appreciably smaller than those reported in homogeneous closed systems (0.2 to 0.6 times), even after adjustment for dilution. These results indicate that (1) isotope fractionation factor ratios (ε18O/ε37Cl, ε18O/ε15N) derived from homogeneous laboratory systems (e.g. pure culture studies) can be used qualitatively to confirm the occurrence of in situ biodegradation of both perchlorate and nitrate, but (2) the magnitudes of the individual apparent ε values cannot be used quantitatively to estimate the in situ extent of biodegradation of either anion.
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