Compound-Specific Isotope Analysis of RDX and Stable Isotope

Oct 1, 2008 - Corresponding author phone: 972-8-6820387; fax: 972-8-6596909; email: [email protected]., †. Zuckerberg Institute for Water Research,...
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Environ. Sci. Technol. 2008, 42, 7772–7777

Compound-Specific Isotope Analysis of RDX and Stable Isotope Fractionation during Aerobic and Anaerobic Biodegradation A N A T B E R N S T E I N , * ,†,‡ Z E E V R O N E N , † E I L O N A D A R , †,‡ R O N I T N A T I V , § HARALD LOWAG,| WILLIBALD STICHLER,| AND RAINER U. MECKENSTOCK| Department of Environmental Hydrology and Microbiology, Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede Boqer Campus, 84990, Israel, Department of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva 84105, Israel, Department of Soil and Water Sciences, Faculty of Agricultural, Food, and Environmental Quality Sciences, The Hebrew University of Jerusalem, P.O. Box 12, Rehovot 76100, Israel, and Helmholtz Zentrum Mu ¨ nchen, German Research Center for Environmental Health, Institute of Groundwater Ecology, Ingolsta¨dter Landstr. 1, 85764 Neuherberg, Germany

Received February 28, 2008. Revised manuscript received August 18, 2008. Accepted September 1, 2008.

Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) is a common contaminant at explosives production sites. Here, we report on the use of compound-specific isotope analysis of RDX to obtain δ15N and δ18O enrichment factors during biodegradation in batch cultures. A new preparation method has been developed based on RDX purification using thin-layer chromatography. RDX is then subjected to an elemental analyzer coupled with an isotope-ratio mass spectrometer (EAIRMS). The precision of the method shows standard deviations of 0.13‰ and 1.18‰ for δ15N and δ18O, respectively, whereas the accuracy of the method has been checked routinely, adhering to external standards. The method was applied to RDX samples subjected to biodegradation under aerobic or anaerobic conditions. Enrichment factors under aerobic conditions were -2.1‰ and -1.7‰ for δ15N and δ18O, respectively, and under anaerobic conditions, -5.0‰ and -5.3‰ for δ15N and δ18O, respectively. The results of this study provide a tool for monitoring natural attenuation of RDX in a contaminated environment.

Introduction Hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) is an explosive that is frequently found as a pollutant of soil and groundwater adjacent to its production plants. Subsurface soil and groundwater contamination by RDX is a global problem. It has been reported in the U.S., Germany, the UK, Canada, * Corresponding author phone: 972-8-6820387; fax: 972-8-6596909; email: [email protected]. † Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research. ‡ Department of Geological and Environmental Sciences, BenGurion University of the Negev. § The Hebrew University of Jerusalem. | Institute of Groundwater Ecology. 7772

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Australia, and in Israel. Throughout the rest of the world, the extent of explosives contamination is either unknown or not available to the public (1). Biodegradation is a desirable, natural attenuation process for RDX in soil and groundwater. Different microorganisms have been reported to degrade RDX and various degradation pathways have been suggested (2-7 Figure 1). Under anaerobic conditions, two distinct pathways for the biodegradation of RDX have been proposed: (i) A transformation pathway, accompanied by accumulation of the subsequent nitroso derivates hexahydro-1-nitroso-3,5dinitro-1,3,5-triazine (MNX), hexahydro-1,3-dinitroso-5-nitro-1,3,5-triazine (DNX), and hexahydro-1,3,5-trinitroso1,3,5-triazine (TNX). This pathway was initially presented by McCormick et al. (5). (ii) A pathway that involves initial denitration followed by ring cleavage, formation of methylenedinitramine (MEDINA) and the eventual formation of nitrous oxide as a major end product. This pathway was postulated by Hawari et al. (6) following biodegradation experiments with municipal anaerobic sludge. The mechanism of denitration under anaerobic conditions was further investigated by Jackson et al. (7), who reported the role of the xplA gene in encoding cytochrome P450 under these conditions and the formation of MEDINA. Under aerobic conditions, in contrast to the anaerobic biodegradation of RDX, nitroso derivates are not normally detected. Thus, under aerobic conditions, ring cleavage is identified as an important initial step (8, 9). Early studies by Hawari et al. (2) stated that ring cleavage of the RDX molecule under aerobic conditions is the result of either NsN or CsH bond cleavage, which leads to the formation of unstable intermediates that spontaneously decompose. Later reports provided evidence that NsN bond cleavage and denitration are the initial steps in the RDX-biodegradation pathway by the Rhodococcus strain DN22 (3, 4). This pathway was later documented for Rhodococcus strain YH1 as well (10). Investigation of the mechanism governing the degradation pathway revealed that it is linked to the activation of cytochrome P450 by xplA (7, 11, 12), similar to denitration under anaerobic conditions. Aerobically, however, denitration leads to the formation of 4-nitro-2,4-diazabutanal (NDAB) instead of MEDINA (7). Exceptions for the occurrence of this pathway under aerobic conditions were reported for fungal strains by Sheremata and Hawari (13) and by Bhatt et al. (14) in which MNX was formed followed by ring cleavage and the formation of MEDINA. Van Aken et al. (15) also detected MNX when RDX was biodegraded under aerobic conditions. It was proposed that the polar metabolite produced from the degradation of RDX has the molecular formula O2NNHCH2NHNO2 (i.e., MEDINA). Theoretically, MNX can potentially be degraded to NDAB as well, if ring cleavage occurs following removal of the NO group, rather than the nitro group. This, however, has never been reported. Although the potential of microorganisms to degrade RDX in contaminated field sites may be identified, actual evidence for the occurrence of RDX biodegradation or even quantitative analysis are generally lacking, as distinct degradation products of RDX may not persist, or may not be detectable (16). Moreover, the putative pathways involved in the biodegradation process in the field are usually unknown. Nevertheless, quantifying the extent of biodegradation and defining the process involved remains a desired goal for water-resource management. The use of compound-specific isotope analysis (CSIA) for environmental pollutants is a relatively new concept in terms of quantifying the extent of biodegradation (e.g., refs 17 and 10.1021/es8005942 CCC: $40.75

 2008 American Chemical Society

Published on Web 10/01/2008

FIGURE 1. Biodegradation pathways of RDX. (A) Aerobic denitration pathway (3, 4). (B) Anaerobic transformation pathway accompanied by the accumulation of nitroso derivates (5). (C) Anaerobic ring-cleavage pathway (6). Compounds in brackets are postulated, but have not been isolated. 18) and gaining information on the degradation pathway involved (e.g., ref 19). The rationale underlying this concept is that as biodegradation proceeds, the remaining pool of pollutants becomes enriched in the heavier isotopes due to chemical bonds of lighter isotopes reacting at a minutely faster rate. The remaining substrate fraction therefore changes its isotopic composition. The extent of isotope enrichment of the remaining contaminant pool enables further quantification of the extent of biodegradation along a contamination plume (20). If stable isotope compositions of several elements of a given compound are analyzed simultaneously, one can obtain information on the initial biochemical steps in the biodegradation pathway or even distinguish between the different possible pathways involved. The increasing use of CSIA in recent years is closely related to the development of analytical capabilities, enabling the isotopic analysis of a specific organic compound. The analytical procedure for CSIA normally comprises gas chromatographic separation of individual compounds, which are then transformed on line to analyte gases for the different elements, such as CO2 for carbon, N2 for nitrogen, H2 for hydrogen, or CO for oxygen. The analyte gases are subsequently transferred on line to an isotope-ratio mass spectrometer (GC-C-IRMS; ref 21). To date, the CSIA concept has focused mainly on aromatic hydrocarbons and chlorinated solvents (18). Although RDX is found worldwide to be an environmental pollutant, its isotopic composition and isotope fractionation have received only scant attention. In the forensic literature, some publications relate to the isotope composition of RDX (22, 23). However, the environmental aspects of RDX isotope composition have rarely been considered. DiGnazio et al. (24) related δ15N values of nitrate in the groundwater to RDX degradation, but noted that they had no other isotopic data to confirm this correlation. Lately, Bordeleau et al. (25) related δ15N values of nitrate in the groundwater to RDX degradation as well. Beller et al. (26) reported isotope signatures of NO2and NO3- formed by RDX photolysis. Hoffsommer et al. (27) reported δ2H isotope effects following RDX alkaline hydrolysis. The use of CSIA of RDX in environmental case studies

is not documented in the literature. Among other reasons, this is probably due to the difficult analysis of explosives such as RDX with CSIA because of the requisite GC separation step: explosives usually decay at elevated temperatures such as those applied in GC separations. Furthermore, even fragments cannot be used for stable isotope analysis (a concept which is usually applied in GC/MS analysis of explosives concentrations), because the decay reaction into fragments is connected with stable isotope effects, which make isotopic analysis difficult. Nevertheless, the application of stable isotope fractionation analysis to quantify the extent of degradation, and to gain information on the degradation pathways involved in RDX-contaminated field sites, may be very promising. Therefore, the objectives of this study were to develop a suitable method for δ15N and δ18O stable isotope analysis in RDX and to define δ15N and δ18O fractionation factors in the aerobic and anaerobic biodegradation of RDX by microorganisms originating from an RDX contaminated site.

Materials and Methods Biodegradation Experiments. Batch biodegradation experiments were conducted to analyze isotope fractionation effects in aerobic and anaerobic degradation pathways of RDX. A sterile 2 L volume of aqueous medium was prepared in a 3 L Erlenmeyer flask for aerobic experiments and in 2.5 L glass bottles for anaerobic experiments. In both cases, the mineral medium consisted of a phosphate buffer (1.0 g/L K2HPO4 and 0.5 g/L KH2PO4, pH 7.1), 0.2 g/L MgSO4, and 2.5 mL/L of trace elements solution (2.5 mg/L FeSO4, 5 mg/L CaCl2, 1.25 mg/L MnSO4, 0.25 mg/L CuSO4, and 0.25 mg/L Na2MoO4). Under aerobic conditions, cyclohexanone served as the carbon source (1.0 mL/L). Under anaerobic conditions, sodium acetate served as the carbon source (1.0 g/L). RDX was added to the aqueous media at an initial concentration of 16-22 mg/L, and served as the sole nitrogen source. The aerobic batch experiments were conducted in eight replicates for oxygen, and eight replicates for nitrogen isotope analysis. VOL. 42, NO. 21, 2008 / ENVIRONMENTAL SCIENCE & TECHNOLOGY

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The anaerobic batch experiments were conducted in six replicates for oxygen and six replicates for nitrogen isotope analysis. For the RDX-biodegradation experiments under aerobic conditions, Rhodococcus strain YH1 isolated from RDXcontaminated soils at an industrial site (28) was used. Inoculation was carried out by adding to each 2 L sterile mineral medium 1 mL of a stationery starter culture of Rhodococcus strain YH1. For RDX degradation under anaerobic conditions, sediments excavated from the saturated zone of the same industrial site were used as a source for RDXdegrading bacteria. Initially, 3-5 g of sediment was used for inoculating a starter mineral medium (2 L), which was kept under anaerobic conditions for 1 month. The bacterial consortium was then harvested by centrifugation (Labofuge 400, Heraeus Inst., Germany) at 3500 RCF, and the pellet was suspended in 100 mL of sterile water, which was then equally divided between the 12 replicates. Aerobic cultures were constantly stirred on a rotary shaker at 175 rpm, 30 °C. Anaerobic cultures were incubated in an anaerobic chamber (Coy Laboratory, Grass Lake, MI) with a gas mixture of 94% N2 and 6% H2 at room temperature. To produce anaerobic conditions, four cycles of purging with the gas mixture, alternated with the application of vacuum, were applied to the bottles before they were introduced into the glovebox. Bottles were then sealed with a cup and kept static in the glovebox for the entire incubation period. This particular way of handling the anaerobic cultures enabled easy collection of high-volume samples, without disturbing the anaerobic conditions. Samples for isotope analysis were collected into Erlenmeyer flasks during the incubation in increasing volumes; this assured a minimal mass of 600 µg RDX in each sample. RDX concentration in the samples was monitored by highperformance liquid chromatography (HPLC; Agilent 1100 series, Palo Alto CA) according to EPA method 8330 (29). The RDX in the samples was liquid-liquid extracted into dichloromethane (DCM). The DCM extracts were reduced to a final volume of 0.5-1.0 mL under nitrogen flow at 30 °C (TurboVap Zymark, Hopkinton, MA). RDX Purification by Thin Layer Chromatography (TLC). RDX in the DCM extracts was purified from its degradation products by TLC method, using silica gel on glass TLC plates (10 × 20 cm) with an internal fluorescent indicator (Fluka, Buch, Switzerland). The mobile phase in the TLC method consisted of double-distilled water, methanol, and acetone (HPLC grade) in a volumetric ratio of 1:1:0.1. Plates were placed vertically in covered glass tanks, and the mobile phase was allowed to rise up the plate as a prewash. When the wetting front reached the top, the plate was taken out of the tank and air-dried for 30 min. After drying, RDX samples, dissolved in DCM, were applied in a line 1.5 cm above the bottom of the plate, using a disposable glass Pasteur pipet. When the solvent evaporated, plates were put back into the tanks until the mobile phase again reached the top of the plate. Plates were then removed and air-dried for 30 min. For greater separation between RDX and its degradation products, a second cycle of wetting and drying was subsequently carried out. In this second cycle, plates were put back into the tanks until the mobile phase again reached the top of the plate. They were then removed from the tank, and air-dried for 30 min. RDX spots were detected by UV light and scraped off the plate into a glass vial. Sample Preparation for Isotope Analysis. Purified RDX was eluted from the scraped silica gel by adding 3-4 mL of DCM and shaking on a rotary shaker for 1 h. Up to 2 mL DCM solution from each sample was collected in a 2 mL glass vial using a glass syringe. The collected DCM solution was allowed to evaporate at room temperature to a final volume of approximately 1 mL. To ensure the absence of 7774

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reduced degradation products in the samples, a fraction from the DCM solution was analyzed by HPLC following EPA method 8330 (29). RDX standard for HPLC was prepared from solid powder obtained from the Israeli Military Industry (Ramat Hasharon). MNX, DNX, and TNX were purchased from SRI International (Menlo Park, CA). In samples in which the presence of the degradation products MNX, DNX, and TNX was found to be greater than 5% of the RDX mass, the solution was subjected to an additional separation procedure on TLC plates, as described above. For δ15N analysis, the DCM solution was injected into two duplicate tin capsules for liquids, and for δ18O analysis the DCM solution was injected into two duplicate silver capsules for liquids (Hekatech, Wegberg, Germany). Before closing the capsules, DCM was allowed to evaporate, leaving an expected minimal mass of 120 µg purified RDX. Isotope Analysis Technique. Isotope analysis was carried out by an elemental analyzer (EA) (Euro Vector SPA, Milan, Italy) coupled with a combustion unit (Hekatech, Wegberg, Germany) followed by IRMS (Thermo Fisher Scientific, Bremen, Germany). The temperature of the oxidation tube in the EA was 1000 °C and the temperature of the reduction tube was 600 °C. The temperature of the combustion tube was 1480 °C. For calibration, before and after the analysis of each 46sample batch, three different standards were analyzed in triplicate. Standards used for δ15N calibration were caffeine (IAEA-600), and L-glutamic acid (USGS-40 and USGS-41). Standards used for δ18O calibration were benzoic acid (IAEA601 and IAEA-602) and sucrose (IAEA-CH6). In addition, a standard was analyzed after every seventh sample for calibrating shifts in the measurements. Caffeine standard was used for this purpose in the δ15N measurements and benzoic acid was used for this purpose in the δ18O measurements. Calculations. The natural abundance of 18O and 15N is 0.205% and 0.368%, respectively. IRMS yields the isotopic composition of the investigated compound x relative to the isotopic composition of a standard. This isotope ratio, δ, is given in per mil units (‰) and is defined as δx )

(

)

Rx - Rstd × 1000 Rstd

(1)

where δx is the isotope ratio of the investigated compound, and Rx and Rstd are the ratios between the heavy and light isotopes in the investigated compound, and in the standard, respectively. The mathematical description of the relation between the extent of degradation and isotopic composition of the investigated compound can be performed by a Rayleigh distillation equation (30) ln

( )

RX,t ) (R - 1)ln f RX,0

(2)

Ct C0

(3)

with f)

where C0 and Ct are the compound concentrations at times 0 and t, respectively. The stable isotope fractionation factor R can be obtained by plotting the natural logarithm of the isotopic enrichment, (Rx,t/Rx,0), against the natural logarithm of the extent of degradation, f. The linear slope of the obtained curve is thus (R - 1). Enrichment factors () were determined for the different degradation experiments, expressed as ε ) (R - 1) × 1000

(4)

TABLE 1. Isotopic Composition of RDX Standards with and without the TLC Purification RDX following TLC procedure average

Pure RDX without TLC procedure

std. deviation

average

std. deviation

0.13‰ 1.18‰

-9.61‰ (n ) 7) 23.06‰ (n ) 34)

0.04‰ 1.30‰

δ15N -9.66‰ (n ) 7) δ18O 24.07‰ (n ) 13)

When several atoms of the same element are present in a compound, those not taking part in the reaction will decrease the observable isotope fractionation (31). Thus, intrinsic isotope enrichment, i, can be defined as εi ) ε · n

(5)

where n is the number of atoms in the element.

Results and Discussion Previous studies suggested that aerobic biodegradation of RDX by Rhodococcus strain YH1, which was isolated from contaminated soils at the RDX production site (28), is initiated by denitration (10). Thus, under aerobic conditions, biodegradation was expected to be accompanied by accumulation of NDAB and by a primary isotopic effect of δ15N enrichment, whereas no, or only very slight δ18O enrichment would be observed. It was also hypothesized that under anaerobic conditions, with a mixed culture of contaminated soil originating from the same RDX production site, RDX biodegradation would follow the transformation pathway described by McCormick et al. (5), accompanied by accumulation of the nitroso derivates MNX, DNX, and TNX and by a primary isotope effect for both δ15N and δ18O. The present work was aimed at establishing a methodology for stable isotope analysis of RDX, and testing whether stable isotope fractionation analysis of several elements (N and O) can distinguish between anaerobic and aerobic degradation, or even support one or the other proposed reactions. As already noted, the use of GC-C-IRMS for CSIA analyses of RDX is difficult due to decomposition of the compound within the injector and the column, and the accompanying isotopic effect. Consequently, there was a clear need to establish a new technique for CSIA of RDX. TLC Separation. The separation procedure using the silica-gel TLC plates and methanol-water-acetone mixture was sufficient to observe clear separation of RDX from its degradation products. The Rf values using this method were 0.53, 0.63, 0.73, and 0.80 for RDX, MNX, DNX, and TNX, respectively. When the mass of RDX and its degradation products was high, the spots were smeared, and the separation procedure was therefore repeated. The additional separation cycle was found to be sufficient to decrease the concentration of the reduced degradation products in the RDX samples to less than 5%, as verified by HPLC. To determine the method’s accuracy and precision, replicates of pure RDX from a stock solution (1.0 mg/mL RDX in HPLC-grade DCM) were subjected to the TLC preparation procedure and subsequently analyzed for δ18O and for δ15N. The results were compared to the δ18O and δ15N composition of an RDX stock solution that was not separated by TLC (Table 1) to ensure that the TLC procedure itself does not cause stable isotope fractionation. The δ18O and δ15N isotope compositions of the TLC-treated RDX were found to be within the error range of the pure, non-TLCtreated RDX (Table 1). This suggests that the TLC procedure does not cause significant isotope fractionation, and that the procedure does not suffer from external contamination

with respect to δ15N or δ18O composition. The TLC-treated samples gave less precise results in the δ18O vs δ15N analysis. Nevertheless, the average isotopic composition found for the TLC-treated RDX was similar to that of the pure RDX. Thus, it is suggested that the purification procedure is suitable for routine use of CSIA for RDX with respect to δ15N and δ18O compositions. Stable Isotope Fractionation in Aerobic and Anaerobic Cultures. The analysis of δ15N and δ18O stable isotope fractionation during the biodegradation of RDX in batch experiments produced distinct fractionation trends and enrichment factors under aerobic and anaerobic conditions (Figure 2, Table 2). Under aerobic conditions, clear δ15N enrichment of RDX was detected. Although early reports indicated that both NsN and CsH bond cleavage result in an unstable intermediate leading to rapid ring cleavage (2, 32), the clear δ15N enrichment observed in this study was in accordance with later reports that NsN bond cleavage, rather than CsH bond cleavage, is the first step in the aerobic biodegradation pathway of RDX by Rhodococcus strain YH1. Studies on the biochemical pathway of RDX biodegradation under aerobic conditions have revealed denitration (with the involvement of cytochrome P450) to be an initial step in various Rhodococcus strains. This was demonstrated by Fournier et al. (3) and Bhushan et al. (4) who studied the RDX-biodegradation pathway of Rhodococcus strain DN22, and by Seth-Smith et al. (12), who presented similar results withRhodococcus strain 11Y. Later works identified the role of the gene xplA which encodes cytochrome P450 (7, 11, 12). The work of Nejidat et al. (10), who studied the aerobic biodegradation of RDX by Rhodococcus strain YH1, revealed the formation of a polypeptide which is identical to polypeptides encoded by xplA. Thus, it has been well established that denitration is the initial step in RDX biodegradation under aerobic conditions by this strain. To further confirm the occurrence of this degradation pathway, we carried out biodegradation experiments under aerobic conditions using this strain. During these experiments, HPLC analyses for the detection of RDX, nitroso derivates and NDAB were carried out (see the Supporting Information for the methods and complete results). In these experiments, accumulation of NDAB was observed following RDX degradation, whereas nitroso derivates (among them MNX) were not detected. Mass-balance calculations revealed that the RDX was completely converted to NDAB within 100 h of incubation. From these results, it could be concluded that RDX biodegradation indeed followed the denitration pathway. Nevertheless, in contrast to our expectation of a primary isotopic effect of δ15N enrichment during denitration under aerobic conditions with no, or only very slight δ18O enrichment, clear δ18O enrichment was detected in RDX that was biodegraded under aerobic conditions. This raised the assumption that, in contrast to the knowledge gained on the aerobic degradation pathway used by strain YH1, NsO bond cleavage is the initial step in this pathway rather than NsN bond cleavage, as suggested above. However, if RDX biodegradation under aerobic conditions was initiated by an NsO bond cleavage, inevitably, MNX would have formed. Theoretically, MNX degradation could have resulted in the formation of NDAB as well, which was detected with complete recovery as the product of RDX biodegradation in this work. However, this theoretical possibility seems unlikely, as MNX was not detected in HPLC analyses performed during the incubation period (detection limit 0.25 µM). This leads to the possibility that the pronounced δ18O enrichment is the consequence of intramolecular hydrogen bonds between the NO2 oxygens and the CH2 hydrogens (33). Thus, denitration not only involves the cleavage of an NsN bond but also of an intramolecular HsO hydrogen bond which may be accompanied by a δ18O enrichment. Alternatively, it is VOL. 42, NO. 21, 2008 / ENVIRONMENTAL SCIENCE & TECHNOLOGY

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FIGURE 2. Enrichment in δ15N (left) and δ18O (right) composition of RDX during biodegradation. Open symbols represent anaerobic biodegradation by anoxic sediments, and full symbols represent aerobic biodegradation by Rhodococcus strain YH1.

TABLE 2. Enrichment Factors, E (‰), of δ15N and δ18O during Aerobic and Anaerobic Biodegradation of RDX (in Brackets Are the Intrinsic Isotopic Enrichment Factors, Ei) δ15N (‰)

δ18O (‰)

aerobic -2.1 ( 0.1 (-12.6 ( 0.6) -1.7 ( 0.1 (-10.2 ( 0.6) anaerobic -5.0 ( 0.3 (-30.0 ( 1.8) -5.3 ( 0.5 (-31.8 ( 3.0)

possible that a strong secondary isotopic effect occurs in this system as a consequence of the biochemical mechanism of the rate-determining step. Hengge and Cleland (34) and more recently, Hengge (35) studied secondary isotopic effects in phosphoryl-transfer reactions and later in sulfuryl-transfer reactions. Using labeled compounds, they observed, in certain reactions, secondary isotopic effects in the nonbridge oxygen atoms of the phosphate esters that were in the same range as the bridge oxygen atoms being cleaved. Certainly, RDX denitration has no similarity to phosphoryl or sulfuryl reactions; however, it was shown that strong secondary isotopic effects can indeed occur in certain reactions which are related to their mechanism. Similar to isotopic enrichment during aerobic biodegradation, enrichment of both δ15N and δ18O was evident under anaerobic conditions (Figure 2). These results were expected, as NsO bond cleavage was identified as the first step in the reduction pathway under anaerobic conditions by the enriched culture. Ring cleavage as an initial step in RDX biodegradation under anaerobic conditions, as reported by Hawari et al. (6), was excluded as a possible pathway in this study following the observed sequential formation of MNX, DNX, and TNX during the degradation process (for massbalance calculations, see the Supporting Information). Reports in the literature on δ15N or δ18O enrichment following biodegradation are scarce. Three studies exhibiting some similarities with RDX biodegradation were performed by Hartenbach et al. (36), Tobler et al. (37), and Hofstetter et al. (38) who measured isotope enrichment during the abiotic reduction of different nitro-aromatic compounds. In this process, an NsO bond is cleaved in a nitro group that is external to the aromatic ring; this is somewhat similar to the anaerobic reduction pathway of RDX in which an NsO bond is cleaved in a nitro group that is external to the triazinic ring. In the three aforementioned studies, the intrinsic δ15N enrichment factors, i, varied between -28.0 ( 0.8‰ and -41.9 ( 1.1‰. The intrinsic enrichment factors of δ15N found in this work for anaerobic biodegradation of RDX (-30.0 ( 1.8) are within the same range. However, neither of the aforementioned studies looked at δ18O enrichment. Studies on fractionation involving NsN bond cleavage in similar organic compounds have not been reported in the literature. Because the bacteria used in this study originated from an RDX-contaminated site, the results of the study point to 7776

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FIGURE 3. δ15N versus δ18O for aerobic and anaerobic biodegradation of RDX. two different potential RDX-biodegradation pathways at this site: an aerobic pathway which is initiated by a denitration step, followed by ring cleavage (pathway A in Figure 1), and an anaerobic pathway, which is characterized by sequential transformation of RDX to its nitroso derivates (pathway B in Figure 1). There is no evidence in this work for the existence of the other proposed pathways (6):initial ring cleavage under anaerobic conditions (pathway C in Figure 1) or initial CsH bond cleavage under aerobic conditions. Anaerobic and aerobic degradation of RDX produce different isotope fractionation patterns (Figure 3), which optimally might constitute a valuable tool to distinguish between the two possible pathways in contaminated field sites (19). Theoretically, if RDX isotope values from the field were to lie on one of the curves in a two-dimensional isotope plot of δ15N versus δ18O, the type of degradation pathway and the extent of biodegradation could be evaluated, providing that the parent values (R0) of the original released compound were known. However, as the difference between the two patterns in the case of RDX biodegradation is not very pronounced, it might be difficult to perform such an evaluation. Thus, the δ15N and δ18O enrichment factors obtained in this study for RDX biodegradation under aerobic and anaerobic conditions, although valuable for quantifying the extent of biodegradation at RDX-contaminated field sites, may not be useful for distinguishing the relative importance of the biodegradation pathways involved at the site.

Acknowledgments We thank Dietmar Jurrat for laboratory assistance. This work was supported by the Israel Water Authority, the Eshkol Fellowship and the BMBF young scientist exchange program.

Supporting Information Available Experiments were carried out to determine the RDX degradation products under aerobic and under anaerobic

conditions. This material is available free of charge via the Internet at http://pubs.acs.org.

Literature Cited (1) Spain, J. C. Biodegradation of nitroaromatic compounds. Annu. Rev. Microbiol. 1995, 523–555. (2) Hawari, J.; Beaudet, S.; Halasz, A.; Thiboutot, S.; Ampleman, G. Microbial degradation of explosives: biotransformation versus mineralization. Appl. Microbiol. Biotechnol. 2000, 54, 605–618. (3) Fournier, D.; Halasz, A.; Spain, J.; Fiurasek, P.; Hawari1, J. Determination of key metabolites during biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine with Rhodococcus sp., strain DN22. Appl. Environ. Microbiol. 2002, 68, 166–172. (4) Bhushan, B.; Trott, S.; Spain, J. C.; Halasz, A.; Paquet, L.; Hawari, J. Biotransformation of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) by a rabbit liver cytochrome P450: Insight into the mechanism of (RDX) biodegradation by Rhodococcus sp., strain DN22. Appl. Environ. Microbiol. 2003, 69, 1347–1351. (5) McCormick, N. G.; Cornell, J. H.; Kaplan, A. M. biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine. Appl. Environ. Microbiol. 1981, 42, 817–823. (6) Hawari, J.; Halasz, A.; Sheremata, T.; Beaudet, S.; Groom, C.; Paquet, L.; Rhofir, C.; Ampleman, G.; Thiboutot, S. Characterization of metabolites during biodegradation of hexahydro1,3,5-trinitro-1,3,5-triazine (RDX) with municipal sludge. Appl. Environ. Microbiol. 2000, 66, 2652–2657. (7) Jackson, R. J.; Rylott, E. L.; Fournier, D.; Hawari, J.; Bruce, N. C. Exploring the biochemical properties and remediation applications of the unusual explosive-degrading P450 system XplA/B. Proc. Natl. Acad. Sci. U. S. A. 2007, 104, 16822–16827. (8) Binks, P. R.; Nicklin, S.; Bruce, N. C. Degradation of hexahydro1,3,5-trinitro-1,3,5-triazine (RDX) by Stenotrophomonas maltophilia PB1. Appl. Environ. Microbiol. 1995, 61, 1318–1322. (9) Coleman, N. V.; Nelson, D. R.; Duxbury, T. Aerobic degradation of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX). as a nitrogen source by a Rhodococcus sp., strain DN22. Soil Biol. Biochem. 1998, 30, 1159–1167. (10) Nejidat, A.; Kafka, L.; Tekoah, Y.; Ronen, Z. Effect of organic and inorganic nitrogenous compounds on RDX degradation and cytochrome P-450 expression in Rhodococcus strain YH1. Biodegradation 2008, 19, 313–320. (11) Indest, K. J.; Crocker, F. H.; Athow, R. A TaqMan polymerase chain reaction method for monitoring RDX-degrading bacteria based on the xplA functional gene. J. Microbiol. Methods 2007, 68, 267–274. (12) Seth-Smith, H. M. B.; Rosser, S. J.; Basran, A.; Travis, E. R.; Dabbs, E. R.; Nicklin, S.; Bruce, N. C. Cloning, sequencing, and characterization of the Hexahydro-1,3,5-trinitro-1,3,5-triazine degradation gene cluster from Rhodococcus rhodochrous. Appl. Environ. Microbiol. 2002, 68, 4764–4771. (13) Sheremata, T. W.; Hawari, J. Mineralization of RDX by the white rot fungus Phanerochaete chrysosporium to carbon dioxide and nitrous oxide. Environ. Sci. Technol. 2000, 34, 3384–3388. (14) Bhatt, M.; Zhao, J. S.; Monteil-Rivera, F.; Hawari, J. Biodegradation of cyclic nitramines by tropical marine sediment bacteria. J. Ind. Microbiol. Biotechnol. 2005, 32, 261–267. (15) Van Aken, B.; Yoon, J. M.; Schnoor, J. L. Biodegradation of nitrosubstituted explosives 2,4,6-trinitrotoluene, hexahydro-1,3,5trinitro-1,3,5-triazine, and octahydro-1,3,5,7-tetranitro-1,3,5tetrazocine by a phytosymbiotic Methylobacterium sp. associated with poplar tissues (Populus deltoides × nigra DN34). Appl. Environ. Microbiol. 2004, 70, 508–517. (16) Pennington, J. C.; Brannon, J. M.; Gunnison, D.; Harrelson, D. W.; Zakikhani, M.; Miyares, P.; Jenkins, T. F.; Clarke, J.; Hayes, C.; Ringleberg, D.; Perkins, E.; Fredrickson, H. Monitored natural attenuation of explosives. Soil Sed. Contam. 2001, 10, 45–70. (17) Griebler, C.; Safinowski, M.; Vieth, A.; Richnow, H. H.; Meckenstock, R. U. Combined application of stable carbon isotope analysis and specific metabolites determination for assessing in situ degradation of aromatic hydrocarbons in a tar oilcontaminated aquifer. Environ. Sci. Technol. 2004, 38, 617–631. (18) Meckenstock, R. U.; Morasch, B.; Griebler, C.; Richnow, H. H. Stable isotope fractionation analysis as a tool to monitor biodegradation in contaminated aquifers. J. Contam. Hydrol. 2004, 75, 215–255.

(19) Elsner, M.; Zwank, L.; Hunkeler, D.; Schwarzenbach, R. P. A new concept linking observable stable isotope fractionation to transformation pathways of organic pollutants. Environ. Sci. Technol. 2005, 39, 6896–6916. (20) Richnow, H. H.; Annweiler, E.; Michaelis, W.; Meckenstock, R. U. Microbial in situ degradation of aromatic hydrocarbons in a contaminated aquifer monitored by carbon isotope fractionation. J. Contam. Hydrol. 2003, 65, 101–120. (21) Schmidt, T. C.; Zwank, L.; Elsner, M.; Berg, M.; Meckenstock, R. U.; Haderlein, S. B. Compound-specific stable isotope analysis of organic contaminants in natural environments: a critical review of the state of the art, prospects, and future challenges. Anal. Bioanal. Chem. 2004, 378, 283–300. (22) Phillips, S. A.; Doyle, S.; Philp, L.; Coleman, M. Proceedings: network developing forensic applications of stable isotope ratio mass spectrometry conference 2002. Sci. Justice 2003, 43, 153– 160. (23) Lott, M. J.; Howa, J.; Ehleringer, J. R. Locating the Origins of Explosives through Stable Isotope Ratio Analysis. Poster at the Forensic Isotope Ratio Mass Spectrometry (Firms) Conference, 2002. (24) DiGnazio, F. J.; Krothe, N. C.; Baedke, S. J.; Spalding, R. F. δ15N of nitrate derived from explosive sources in karst aquifer beneath the Ammunition Burning Ground, Crane Naval Surface Warfare Center, Indiana, USA. J. Hydrol. 1998, 206, 164–175. (25) Bordeleau, G.; Savard, M. M.; Martel, R.; Ampleman, G.; Thiboutot, S. Determination of the origin of groundwater nitrate at an air weapons range using the dual isotope approach. J. Contam. Hydrol. 2008, 98, 97–105. (26) Beller, H. R.; Madrid, V.; Hudson, G. B.; McNab, W. W.; Carlsen, T. Biogeochemistry and natural attenuation of nitrate in groundwater at an explosives test facility. Appl. Geochem. 2004, 19, 1483–1494. (27) Hoffsommer, J. C.; Kubose, D. A.; Glover, D. J. Kinetic isotope effects and intermediate formation for the aqueous alkaline homogeneous hydrolysis of 1,3,5-tiaza-1,3,5-trinitrocyclohexane (RDX). J. Phys. Chem. 1977, 81, 380–385. (28) Brenner, A.; Ronen, Z.; Harel, Y.; Abeliovich, A. Use of RDX as a nitrogen source in biological treatment of munitions wastes. Water Environ. Res. 2000, 72, 469–475. (29) U.S. Environmental Protection Agency. Method 8330, SW-846 update III, Part 4: 1 (B), U.S. EPA Office of Solid Waste, U.S. Government Printing Office: Washington, DC, 1997. (30) Rayleigh, J. W. S. Theoretical considerations respecting the separation of gases by diffusion and similar processes. Philos. Mag. 1896, 42, 493–498. (31) Morasch, B.; Richnow, H. H.; Vieth, A.; Schink, B.; Meckenstock, R. U. Stable isotope fractionation caused by glycyl radical enzymes during bacterial degradation of aromatic compounds. Appl. Environ. Microbiol. 2004, 70, 2935–2940. (32) Melius, C. F., In Chemistry and Physics of Energetic Materials: Thermochemical Modeling: I Applications to Decomposition of Energetic Materials; Bulusu, S. N., Ed; Kluwer Academic Publishers: Dordrecht, Netherlands, 1990; pp 21-49. (33) Harris, N. J.; Lammertsma, K. Ab initio density functional computations of conformations and bond dissociation energies for hexahydro-1,3,5-trinitro-1,3,5-triazine. J. Am. Chem. Soc. 1997, 119, 6583–6589. (34) Hengge, A. C.; Cleland, W. W. Phosphoryl-transfer reactions of phosphodiesters: characterization of transition states by heavyatom isotope effects. J. Am. Chem. Soc. 1991, 113, 5835–5841. (35) Hengge, A. C. Isotope effects in the study of phosphoryl and sulfuryl transfer reactions. Acc. Chem. Res. 2002, 35, 105–112. (36) Hartenbach, A.; Hofstetter, T. B.; Berg, M.; Bolotin, J.; Schwarzenbach, R. P. Using nitrogen isotope fractionation to assess abiotic reduction of nitroaromatic compounds. Environ. Sci. Technol. 2006, 40, 7710–7716. (37) Tobler, N. B.; Hofstetter, T. B.; Schwarzenbach, R. P. Assessing iron-mediated oxidation of toluene and reduction of nitroaromatic contaminants in anoxic environments using compoundspecific isotope analysis. Environ. Sci. Technol. 2007, 41, 7773– 7780. (38) Hofstetter, T. B.; Neumann, A.; Arnold, W. A.; Bolotin, J.; Cramer, C. J.; Schwarzenbach, R. P. Substituent effects on nitrogen isotope fractionation during abiotic reduction of nitroaromatic compounds. Environ. Sci. Technol. 2008, 42, 1997–2003.

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