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Journal of Hazardous Materials 203–204 (2012) 333–340
Contents lists available at SciVerse ScienceDirect
Journal of Hazardous Materials
journal homepage: www.elsevier.com/locate/jhazmat
Biodegradation of explosives mixture in soil under different water-content
conditions
S. Sagi-Ben Moshe a , O. Dahan b , N. Weisbrod b , A. Bernstein b , E. Adar b,c , Z. Ronen b,∗
a
Dept. of Soil & Water Sciences, The Hebrew University of Jerusalem, P.O. Box 12, Rehovot 76100, Israel
Dept. of Environmental Hydrology & Microbiology, Zuckerberg Institute for Water Research, Ben-Gurion University of the Negev, Sede Boqer 84990, Israel
c
Dept. of Geological and Environmental Sciences, Ben-Gurion University of the Negev, Beer Sheva 84105, Israel
b
a r t i c l e
i n f o
Article history:
Received 27 September 2011
Received in revised form 7 December 2011
Accepted 11 December 2011
Available online 19 December 2011
This paper is dedicated to the memory of
Prof. Ronit Nativ who passed away on 31
October 2006.
Keywords:
RDX
TNT
HMX
Biodegradation
Redox potential
Soil water content
a b s t r a c t
Soil redox potential plays a key role in the rates and pathways of explosives degradation, and is highly
influenced by water content and microbial activity. Soil redox potential can vary significantly both temporally and spatially in micro-sites. In this study, when soil water content increased, the redox potential
decreased, and there was significant enhancement in the biodegradation of a mixture of three explosives.
Whereas TNT degradation occurred under both aerobic and anaerobic conditions, RDX and HMX degradation occurred only when water content conditions resulted in a prolonged period of negative redox
potential. Moreover, under unsaturated conditions, which are more representative of real environmental
conditions, the low redox potential, even when measured for temporary periods, was sufficient to facilitate anaerobic degradation. Our results clearly indicate a negative influence of TNT on the biodegradation
of RDX and HMX, but this effect was less pronounced than that found in previous slurry batch experiments: this can be explained by a masking effect of the soil in the canisters. Fully or partially saturated
soils can promote the existence of micro-niches that differ considerably in their explosives concentration,
microbial community and redox conditions.
© 2011 Elsevier B.V. All rights reserved.
1. Introduction
In many explosive-contaminated sites, the soil is contaminated
with mixtures of explosives, most commonly 2,4,6-trinitrotoluene
hexahydro-1,3,5-trinitro-1,3,5-triazine
(RDX)
and
(TNT),
octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine
(HMX)
[1,2]
(Fig. 1). Biodegradation of these compounds appears to be an effective means of remediating contaminated soil and water. Redox
conditions highly influence the efficiency of explosives biodegradation in the sub-surface, as well as dictate the degradation
pathway and the accumulated degradation products.
TNT can be biodegraded both aerobically and anaerobically.
In both cases, the initial products formed are the reduced amino
derivatives 4-amino-2,6-dinitrotoluene (4-Am-2,6-DNT) and 2amino-4,6-dinitrotoluene (2-Am-4,6-DNT) [1]. Further degradation to the most reduced product, triaminotoluene (TAT), requires
highly negative redox potential values—below −200 mV—and
therefore TAT is found only in reduced environments [3]. Condensation of the partly reduced amino intermediates may occur, leading
to the formation of azoxy intermediates [3,4].
∗ Corresponding author. Tel.: +972 8 6596895; fax: +972 8 6596909.
E-mail address: zeevrone@bgu.ac.il (Z. Ronen).
0304-3894/$ – see front matter © 2011 Elsevier B.V. All rights reserved.
doi:10.1016/j.jhazmat.2011.12.029
The biodegradation of RDX occurs under both aerobic and anaerobic conditions but the anaerobic process is significantly faster [5].
Aerobically, it has been found that microbial cleavage of one of the
N NO2 bonds produces unstable intermediates, and is followed
by rapid cleavage of the triazine ring [1]. Anaerobically, sequential
reduction of the nitro groups to produce mono-, di- and trinitroso
derivatives (MNX, DNX and TNX, respectively) is most frequently
observed. The nitroso derivatives may be further transformed to
produce the unstable hydroxylamine derivatives, leading to ring
cleavage [6]. This pathway was described for RDX incubation with
municipal sludge under measured Eh values of −250 to −300 mV
[7].
HMX mostly undergoes anaerobic biodegradation through the
reduction of nitro groups to form the corresponding nitroso derivatives, or alternatively via direct ring cleavage [8].
The soil’s redox potential plays a key role in the degradation pathway of explosives, as well as in the rate of degradation
[1,5,8–10]. Thus, to predict the fate of explosives in the environment, knowledge of the redox conditions is required. Explosives
degradation experiments in which redox potential was measured
have involved experiments in soil slurries that do not represent
natural conditions [9,11].
Soil redox potential is known to be highly influenced by both
water content and microbial respiration. Molecular oxygen acts as
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O2 N
NO2
NO2
N
N
O2 N
NO2
CH 3
2,4,6-trinitrotoluene
(TNT)
N
N
O 2N
N
O 2N
N
NO2
Hexahydro-1,3,5-trinitro-1,3,5-triazine
(RDX)
NO2
N
NO2
Octahydro-1,3,5,7-tetranitro-1,3,5,7-tetrazocine
(HMX)
Fig. 1. The molecular structures of TNT, RDX and HMX.
the preferred electron acceptor but once it is consumed, the microbial activity switches to fermentation and anaerobic respiration
[12]. The soil water potential and pore structure determine the rate
at which oxygen is replenished in soil since the diffusion coefficient
of oxygen is lower in water than in gas [13]. It has been shown
that soil redox potential can be very dynamic, varying both temporally and spatially by several orders of magnitude, in micro-sites
[12]. Since under natural conditions soils are normally unsaturated,
the question is which of the pathways that are detected in the
laboratory can also occur in the field, and under what water contents. We hypothesized that anoxic conditions might develop in the
unsaturated zones that are sufficient for the anaerobic degradation
pathways to occur in the field. This is reinforced, for example, by the
detection of RDX’s anaerobic nitroso derivatives along unsaturated
soil profiles [14].
The degree of saturation can affect the extent at which one compound affects the degradation of another, as observed in slurry
experiments [2]. It is possible that lower saturation will decrease
the availability of inhibiting compounds.
To fill in some of these gaps in our knowledge of explosives biodegradation under unsaturated conditions we explored
whether anaerobic conditions might exist in unsaturated soils with
different water content and whether these conditions would be sufficient for anaerobic biodegradation of the explosives. We further
determined whether the inhibitory effect of TNT and its degradation products on RDX and HMX degradation occurs in unsaturated
soils, similar to the reported observation for saturated conditions
[2].
2. Experimental
2.1. Chemicals
TNT, RDX and HMX (>95% purity) provided by the Israeli Military
Industry were used for the biodegradation experiment. Analytical
standards for HPLC analysis of RDX, 2-Am-4,6-DNT and 4-Am2,6-DNT were purchased from Supelco (Bellefonte, PA). Analytical
standards for 4-nitro-2,4-diazabutanal (NDAB), MNX, DNX, and
TNX were from SRI International (Menlo Park, CA). TNT and HMX
standards for HPLC analysis were also prepared from solid powder (>95% purity). Methanol and acetone were HPLC-grade, and all
other chemicals were reagent-grade.
2.2. Biodegradation of explosives mixtures under different
water-content conditions
Batch experiments were conducted to characterize the
biodegradation of three explosives—TNT, RDX and HMX in a mixture, under different conditions of water content: dry (1%, w/w),
moderate (7%, w/w) and saturated (19%, w/w). Since intensive
fermentation and gas production occurred in the saturated soil
treatment on the first 2 days, water leaked from the canisters, and
the above water content was determined after the leakage. The soil
for all treatments (94% sand, 1% silt and 5% clay on a dry weight
basis) was excavated 10 cm below the soil surface of an infiltration pond which has been used for over 20 years to dispose of
untreated wastewater from explosives-manufacturing plants [14].
Soil (200 kg) was sieved to exclude coarse materials and mixed
with 25 L of nitrogen-free sterile mineral solution [15] containing
molasses (5 g/L as carbon), which served as the external carbon
source. The soil was then air-dried for 4 days, and then sieved again
and mixed with explosives powder. The soil was then mixed with
distilled water to obtain the desired water content and packed to
completely fill 1-L stainless-steel canisters. The canisters with moderate water content were rotated twice a day (180◦ each time) to
avoid water drainage and to maintain homogeneous water-content
conditions. Three replicates of each water-content treatment were
taken at every sampling point (once a week), and the concentrations of the explosives and water content in the samples were
monitored for the three treatments (in triplicate, 3–5 subsamples
from each canister) every week. The replicate canisters from the
final sampling point (i.e. the three replicates of each water content
that were sampled at the end of the experiment) contained Ag/AgCl
electrodes (Cole-Parmer® ORP electrode, in-line, double-junction,
Vernon Hills, IL) which enabled continuous monitoring of the redox
potential throughout the entire experiment (a period of 20 weeks).
Note that the Ag/AgCl electrode readings represent only the immediate environment of the electrode and that the redox potential
may vary, as mentioned above, both temporally and spatially in
micro-sites [12].
In the first experiment, the different treatments were sampled
once a week, for a total period of 20 weeks. This first experiment
focused on the degradation of the three explosives, i.e. in the presence of TNT. Then, a second experiment was carried out, this time
focusing solely on RDX and HMX degradation. The second experiment was performed under moderate and saturated water contents
only (7% and 16% (w/w), respectively), in the absence of TNT. The
treatments in the second experiment were sampled every 1–2
weeks, for a total period of 20–24 weeks. In the second experiment, the influence of TNT on the biodegradation of RDX and HMX
was also examined. Therefore, although the soil for this experiment was contaminated only with RDX and HMX, each treatment
had additional control canisters which included TNT as well. The
TNT-containing canisters were sampled every 2–4 weeks.
The initial concentration was calculated from concentrations
determined in five replicate soil extracts (Table 1), and the
Table 1
Initial concentrations of explosives.
Explosive
compound
First experiment
(mg/kg of dry soil)
TNT
RDX
HMX
440 ± 63
343 ± 20
352 ± 32
Second experiment
(mg/kg of dry soil)
Without TNT
With TNT
317 ± 84
268 ± 24
406 ± 94
274 ± 22
222 ± 27
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2.4. Effect of TNT on soil toxicity
Soil toxicity was examined in several soil samples obtained
from different samples of the wet and moderate water-content
treatments of the second experiment (Section 2.2). Toxicity assay
was conducted using biosensor (CheckLight Qiryat-Tivo’n, Israel),
a microbial sensor that is engineered to produce light in response
to environmental toxic effects [17].
Soil (1.5 g) from several replicates of the wet treatment of the
second experiment was suspended in 3 mL double-distilled water
and shaken on a rotary shaker (150 rpm) for 1 h. The suspended sediment was allowed to settle and the supernatant was centrifuged
to further reduce suspended solids. The toxicity of this solution was
tested using PCB-TOX (ToxScreen3) that contains the luminescent
bacterium Photobacterium leiognathi according the manufacturer’s
instructions for microliter plate assay (CheckLight Ltd.). The plates
were incubated and read by Tecan Infinite M200 micro-plate reader
(Männedorf, Switzerland). The toxicity was expressed as IC50 (IC50
representing the percentage sample dilution causing a twofold
decrease in luminescence, while lower IC50 values signify higher
toxicity), where IC50 values of the different samples were calculated
using an Excel spread sheet provided by the toxicity kit manufacturer.
2.5. Analytical methods
To determine explosives concentrations, soil samples from the
different experiments were extracted in methanol using Accelerated Solvent Extraction (ASE-200, Dionex Corporation, Sunnyvale,
CA) according to the method of Ronen et al. [20]. Concentrations
of the compounds TNT, 2-Am-4,6-DNT, 4-Am-2,6-DNT, RDX, MNX,
DNX, TNX and HMX were analyzed by HPLC (Agilent 1100 series,
Agilent Technologies, Inc., Santa Clara, CA) according to EPA method
8330 [18]. The detection limit for the above compounds in the soil
extracts was 0.05 mg/L.
Water content in the soil samples was determined gravimetrically in three to five replicate soil samples from each canister by
comparing a sample weight relative to its weight after drying for
24 h at 105 ◦ C.
3. Results
3.1. Biodegradation of explosives mixture under different
water-content conditions
In both experiments, the increase in water content resulted in
an increase in degradation extent. In the first experiment, under
gravimetric water content (GWC) of 1%, we observed some disappearance of TNT but no disappearance of RDX or HMX (Fig. 2a).
Relative concentrations (C/C0)
In order to follow shifts in microbial populations, DNA was
extracted from 0.65 g of soil from several samples of the three
treatments of the first biodegradation experiment (Section 2.2)
with Power Soil DNA Kit (Mo Bio, Carlsbad, CA). Polymerase chain
reaction (PCR) followed by denaturing gradient gel electrophoresis
(DGGE) was preformed as describe previously [2,16]. Major bands
from the gel were carefully excised, DNA was extracted from gel
slices and cloned in the plasmid pTZ57R/T using the InsTAcloneTM
PCR Cloning Kit (Fermentas, Hanover, MD). DNA sequencing was
performed by Macrogen Inc. (Seoul City, Korea).
(a)
TNT
RDX
HMX
2-Am-4,6-DNT
4-Am-2,6-DNT
1.2
1.0
.8
.6
.4
.2
0.0
1.4
0
5
10
15
20
(b)
Relative concentrations (C/C0)
2.3. Effect of explosives concentrations and soil water content on
the microbial population
1.4
TNT
RDX
HMX
2-Am-4,6-DNT
4-Am-2,6-DNT
1.2
1.0
.8
.6
.4
.2
0.0
1.4
0
5
10
15
20
(c)
Relative concentrations (C/C0)
uncertainties (±values) represent one standard deviation of the
replicate measurements.
335
1.2
1.0
.8
TNT
RDX
HMX
2-Am-4,6-DNT
4-Am-2,6-DNT
MNX
TNX
.6
.4
.2
0.0
0
5
10
15
20
Time (weeks)
Fig. 2. Biodegradation of TNT, RDX and HMX under: (a) dry conditions (1% GWC);
(b) moderate water-content conditions (7% GWC) and (c) high water-content conditions (19% GWC). Data points of representative experiments are the means of
triplicates ± SD.
Under 7% GWC, although TNT was degraded, no degradation of
RDX or HMX was observed (Fig. 2b). In the saturated treatment of
the first experiment, almost full disappearance (>98%) of TNT was
observed after 11 weeks (Fig. 2c). RDX degradation was delayed
and started only after 20 weeks, as indicated by the slight accumulation of the anaerobic nitroso products. An average of ca. 7% of the
initial RDX amount has recovered as nitroso derivates at this sampling point (a total of 107 mol/kg). These degradation products
appeared when TNT had almost completely disappeared from the
soil and the concentration of the TNT amino intermediates was ca.
10 ± 7% of the initial TNT concentration. At the end of the incubation period, the HMX concentration did not differ from its initial
concentration indicating that biodegradation of HMX did not occur
in any of the treatments.
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300
(a)
(a)
RDX
RDX (+TNT)
HMX
HMX (+TNT)
1.5
200
Redox potential (mV)
Relative concentrations (C/C0 )
2.0
1.0
.5
100
0
-100
-200
-300
0.0
0
5
10
15
0
20
5
10
15
20
5
10
15
20
10
15
20
300
(b)
200
1.0
Redox potential (mV)
Relative concentrations (C/C0 )
(b)
.8
.6
.4
100
0
-100
-200
.2
-300
0
0.0
0
5
10
15
300
20
(c)
Time (weeks)
In the second experiment in the absence of TNT, degradation of
RDX and HMX was not expected to be retarded and it was therefore
possible to study their behavior under different water contents. The
biodegradation rates of RDX and HMX (Fig. 3a and b) were found
to be faster with increasing water content. Although retardation in
RDX and HMX degradation was observed in the TNT-containing
canisters, complete degradation inhibition was not observed, in
contrast to the stronger inhibitory effect detected in the presence
of TNT in the first experiment.
In the last sample of the 7% water-content treatment, extremely
high variation in degradation extents was observed between the
different canisters: whereas 75% and 43% degradation of RDX and
HMX, respectively, were found in one of the canisters, no degradation of RDX and HMX was observed in the other two replicates
(Fig. 3a and b).
3.2. Redox potential during biodegradation of explosives under
different water-content conditions
All treatments presented a general trend of decreasing redox
potential with increasing water content. Nevertheless, the temporal trends of the different replicates and treatments were very
different. For example, in the 7% GWC treatment of the first experiment, three different patterns of redox potential were observed for
each of the replicates (Fig. 4b). This pattern was also observed in
7% GWC treatment of the second experiment (Fig. 5a).
Redox potential (mV)
200
Fig. 3. Biodegradation of RDX and HMX in the presence and absence of TNT under:
(a) moderate water-content conditions (7%, w/w) and (b) high water-content conditions (16%, w/w). Data points of representative experiments are the means of
triplicates ± SD.
100
0
-100
-200
-300
0
5
Time (weeks)
Fig. 4. Redox potential (first experiment) under: (a) dry conditions (1% GWC); (b)
moderate water-content conditions (7% GWC) and (c) high water-content conditions (19% GWC).
In the high water-content treatment (19% GWC) of the
first experiment, significantly lower redox-potential values were
observed (Fig. 4c): a significant decrease (∼170 mV) in redox potential was observed on the first 4 days (Fig. 4c). This rapid decrease
was followed by an increase in redox potential to a range between
−240 and −80 mV. Finally, anaerobic redox potential was measured
in this treatment, with final values of −195, −215 and −277 mV. In
the high water-content treatment of the second experiment (16%
GWC), patterns similar to the first experiment were observed, with
final values below −360 mV (Fig. 5b).
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Redox potential (mV)
Table 2
Soil toxicity during the incubation period under the different treatments (means of
duplicates ± SD).
(a)
400
200
0
-200
-400
0
Redox potential (mV)
5
10
15
20
Treatment
Week
IC50 (%)
Wet
Wet
Wet
Wet + TNT
Wet + TNT
Wet + TNT
Moderate
Moderate
Moderate
Moderate + TNT
Moderate + TNT
Moderate + TNT
1
10
20
1
10
20
1
10
20
1
10
17
35.4 ± 9.76
27.8 ± 1.27
24.25 ± 0.35
6.64 ± 1.98
29.6 ± 1.84
7.65 ± 0.78
32.4 ± 1.7
34.1 ± 1.56
29.6 ± 0.14
8.1 ± 0.85
23.5 ± 0.71
7.95 ± 1.63
25
sample was also included in this group and generally, the groups
in this cluster were not much affected by the water content or the
incubation time. The second group of M20, M6 and W11 appeared
to indeed be influenced by both water content and time. The last
group consisted of the three replicates of the W20 samples, with
the D1 (dry) sample distantly clustering with this group.
(b)
400
337
200
3.4. Effect of TNT on soil toxicity
0
-200
-400
0
5
10
15
20
25
Time (weeks)
Fig. 5. Redox potential (second experiment) under: (a) moderate water-content
conditions (7% GWC) and (b) high water-content conditions (16% GWC).
3.3. Effect of explosives concentrations and soil water content on
the microbial population
PCR-DGGE analysis of samples from the first experiments was
performed to examine the effect of soil water content and explosives concentration on the natural microbial population. In the first
experiment, two bands showed up in all except the dry treatment,
where they became very weak after the first week, probably due to
lack of activity under these conditions (Fig. 6). These bands exhibited low sequence similarity to the 16S rRNA gene of uncultured
Bacteroidetes and uncultured Sphingobacteria, respectively (marked
with arrows 1 and 2 in Fig. 6). Another strong band, which exhibited
96% sequence similarity with the 16S rRNA gene of Sporolactobacillus kofuensis, appeared after 11 weeks in the wet treatment (marked
with a circle in Fig. 6). This was the last sample before RDX degradation began (9 weeks later). Overall, none of these sequences was
associated with a known explosives degrader.
The composition of the microbial population after 20 weeks of
the wet treatment was significantly different from that of the initial population, with several new bands. Since in the soil samples
taken after 20 weeks, RDX-degradation products (i.e. MNX, DNX
and TNX) appeared for the first time, these bands might represent
the microbial population capable of RDX degradation. Similarity
analysis of the different lanes using Equity 1 1D software (BioRad)
provided some interesting results (Fig. 7). Three main groups were
clustered: M1, W1, M6 and M11 from the first period of the experiment (where M represents the moderate and W the wet treatments,
and the integer is the elapsed time in weeks). The “week 0”
Toxicity was tested using the luminescent bacterium P. leiognathi (CheckLight Ltd.). In the absence of TNT and presence of RDX
and HMX, soil toxicity increased slightly with time in the wet treatment (IC50 decreased systematically from 35.4 to 24.25%), while no
significant difference in toxicity was observed during the experimental period in the moderate water treatment (IC50 remained
between 29.6 and 34.1%) (Table 2).
In the presence of TNT, soil toxicity was significantly higher after
1 week in comparison to its toxicity in the absence of TNT (IC50 of
6.64% in comparison to 35.4% in the wet treatment and IC50 of 8.1%
in comparison to 32.4% in the moderate water-content treatment).
In the soils containing TNT, toxicity decreased in the samples taken
after 10 weeks and increased again after 10 additional weeks.
The toxicity effect was observed for each compound separately (data not shown) and therefore we could not separate the
toxicity effect of each compound in the explosives mixture and
consequently could not calculate the IC50 concentrations for each
explosive compound.
4. Discussion
We assessed the effect of water content and redox potential
on the biodegradation of a mixture of explosives in soil samples
from the unsaturated zone. Results revealed a link between water
content, redox potential and the rate and extent of explosives
biodegradation. As expected, when soil water content increased,
the redox potential decreased, and significant enhancement in the
biodegradation of all three explosives was observed (Figs. 2 and 3).
This implies that although TNT and RDX can be degraded aerobically, this degradation pathway is not as rapid as anaerobic
degradation. It was also observed that the low redox potential, even
when measured for temporary periods, was sufficient to facilitate
anaerobic degradation throughout the 20 weeks of incubation.
The interplay between water content, redox potential and
biodegradation rate can be demonstrated by comparing the different treatments: under dry conditions, only slight degradation of
TNT and no biodegradation of RDX and HMX were observed during the 20 weeks of the experiment due to the low water content.
Although aerobic biodegradation (positive redox potential) of both
TNT and RDX is known [19,20], it require higher soil water content [20]. Moreover, a recent study has shown that the enzyme
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Fig. 6. PCR-DGGE analysis of the microbial population under different explosives concentrations and soil water-content conditions.
xenobiotic reductase, involved in the biotransformation of different explosives by Pseudomonas fluorescens I-C, is sensitive to high
oxygen tension [21].
The redox trends in all replicates of 7% GWC presented transient formation of anaerobic conditions, reaching low negative
redox potentials, albeit for differing durations (Fig. 4). In the first
experiment, in which a mixture of all three explosives was tested,
we observed partial degradation of TNT and no degradation of
RDX or HMX, and the redox potential remained positive during
most of the experimental period. In the second experiment, in
Fig. 7. Dendogram describing the similarity between the different microbial populations at different time points during the experiment as calculated from the DGGE
analysis (Fig. 6). D, M, and W represent the dry, moderate and wet treatments,
respectively, and the integer represents the elapsed time in weeks.
which only RDX and HMX were included, partial degradation of
these explosive compounds indeed occurred (Fig. 3), while anaerobic conditions were developed for different periods (Fig. 5a). The
formation of temporary anaerobic conditions in unsaturated soils
presumably occurs in soil micro-sites [12]. The transient conditions
and high variability between replicates are unique to the heterogeneous moderate water content, and are not observed under dry
or saturation conditions, which are expected to be more homogeneous. Such anaerobic micro-sites are less abundant under dry
conditions, whereas under saturation the entire soil canisters are
expected to be anaerobic. Clearly the soil bulk redox potential,
which is measured by the Ag/AgCl2 electrode (with diameter of
0.5 cm), cannot represent the local conditions within a microbial
biofilm (with a thickness of only a few micrometers) that is attached
to the sediment under unsaturated conditions. It can be assumed
that biodegradation of RDX and HMX at moderate water content
occurred mostly in these anaerobic micro-sites, rather than in aerobic micro-sites, since anaerobic biodegradation was seen to be
more enhanced. The fact that anaerobic micro-sites are more active
is further supported by the observed accumulation of RDX nitroso
derivatives, which appear only during anaerobic degradation, and
the complete absence of NDAB, an aerobic RDX derivate which is
considered to be a relatively persistent product [22]. However, it
should be noted that we cannot exclude the formation of some aerobic degradation product (NDAB) and its further transformation.
The trend in the explosives degradation with time did not show
changes correlated to the fluctuations in the bulk redox potential,
which may further support the assumption that the bulk redox
potential does not represent the actual redox conditions in separate
micro-niches.
The conclusion that explosives degradation is enhanced with
decreasing redox potential is reinforced by the results of the
last samples from the moderate GWC treatment of the second
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experiment, in which the Ag/AgCl2 electrodes provided continuous
monitoring of the redox potential in the canisters throughout the
entire experimental period. The three replicates of the last sampling
point showed three different redox patterns in the three replicate
canisters, which were correlated to degradation extents: the greatest degradation of RDX and HMX (75% and 43%, respectively) was
found in the canister in which the redox potential remained below
−300 mV for over 9 weeks. In the other two replicate canisters, on
the other hand, in which the anaerobic period was much shorter
and the redox potential was higher, no degradation of RDX or HMX
was observed. Therefore, we suggest that redox potential measurements in unsaturated soil can provide only a rough indication of
the efficiency of reductive biodegradation processes. It should be
noted that although the three canisters displayed different redox
patterns while having similar water contents, it does not imply that
the water content and redox potential are actually not correlated.
The correlation between the water content and the redox potential
is reinforced by the comparison of the moderate water composition
to dry and saturated conditions. Whereas the dry and saturated
soils set a clear trend between these two extreme situations, the
observations from the moderate water content treatment is in correlation to this trend. Thus the high variability between the three
replicates of moderate water content may be the result of the high
variability between the three canisters.
At high water content in the absence of TNT, nearly full degradation of RDX and HMX (up to 98.3% and 90.5%, respectively) was
detected by the end of the second experiment. Anaerobic redox
conditions were measured in two of the three replicates of this
treatment throughout the entire experimental period, with final
redox values below −360 mV. The exceptional third replicate presented an increase in redox potential after approximately 15 weeks,
reaching a final value of 155 mV. Nevertheless, the extent of RDX
and HMX degradation in this canister was similar to that in the
other two. It is suggested that the low redox potential observed
early on in this canister was sufficient to promote anaerobic degradation, and that these conditions remained within micro-niches
in the canister but were not represented by the high, bulk redox
potential.
The general observation of more enhanced RDX degradation
under anaerobic conditions is in agreement with previous studies.
Price et al. [11] observed relative stability of RDX under oxidizing
and moderately reducing conditions, and instability of RDX under
highly reducing conditions (−150 mV), which was accompanied
by the appearance of nitroso derivatives. Those derivatives were
detected at only very low concentrations under oxidizing or moderately reducing conditions. Ringelberg et al. [9] showed that the
rate of RDX loss is significantly greater when the soil is saturated,
coinciding with a gradual increase in the anaerobicity of the system
and the formation of nitroso intermediates, followed by their disappearance from the system. In contrast, no nitroso intermediates
were detected in the unsaturated microcosms. The general observation of more enhanced RDX degradation with increasing water
content is in agreement with previous studies with soil from the
same site. Ronen et al. [20] calculated the RDX half life in carbonamended saturated soil to be 6 days, while in carbon-amended
unsaturated soil (0.1 bar metric potential) it was 21 days.
It should be noted that the moderate water content may represent the real saturation status of soil in the environment. Saturated,
or close to saturated water-content conditions may be less abundant, but may still be observed, e.g. in the vicinity of low conductive
soil layers. In both cases, the total biodegradation of explosives
can be facilitated, and will be enhanced with the increase in water
content (where anaerobic biodegradation dominates). This is supported by field observations on a subsurface soil profile from the
same site that showed enriched ␦15 N values of RDX (indicating
greater degradation extents) in the vicinity of clayey layers, where
339
higher water contents are observed [14]. This enrichment was also
correlated to an increase in the detected nitroso derivatives of RDX,
which suggested that anaerobic RDX biodegradation in these sampling points was dominant.
Similar to previous experiments under saturated conditions,
this study shows that TNT and its metabolite inhibit the biodegradation of RDX and HMX. Our results clearly indicate a negative
influence of TNT on the biodegradation of RDX and HMX by indigenous soil microorganisms. The presence of TNT in the soil decreased
RDX and HMX degradation rate during the experimental period
(Fig. 3). Nevertheless, the inhibitory effect in this study was not as
pronounced as that observed in uniform slurries [2], which presented stronger inhibition of RDX and HMX degradation in the
presence of TNT and its intermediate tetranitroazoxytoluene. This
inhibition was explained by a probable cytotoxic effect on the RDXand HMX-degrading microbial population, as well as direct inhibition of enzymes involved in RDX and HMX degradation [21,23].
Luminescent bacterium P. leiognathi toxicity tests performed in our
current work indicated that soil toxicity significantly increases in
the presence of TNT and decreases after its degradation (after 10
weeks) (Table 2). The second increase in soil toxicity 10 weeks later
can be explained by the possible formation of the TNT intermediate tetranitroazoxytoluene, which has been found to be more toxic
than TNT itself and to cause a higher rate of mutations [3].
The fact that the effect of TNT on the degradation of RDX and
HMX in this study was less pronounced can be explained by a
masking effect of the soil in the canisters. In contrast to homogeneous slurry experiments, fully or partially saturated soils can
promote the existence of micro-niches that differ considerably in
their explosives concentration, microbial community and redox
conditions. Thus, biodegradation of RDX and HMX may proceed
in micro-niches in which TNT and its toxic degradation product do
not exist (either because they have already been fully degraded in
these niches, or because they were completely absent in the first
place).
Changes in microbial populations were evident upon analysis
of the DGGE gel. The strong bands (marked 1 and 2 in Fig. 6)
were most similar to the 16S rRNA gene of uncultured Bacteroidetes
(JN695872) and to the 16S rRNA gene (96%) of the uncultured Sphingobacteria (EF520602). These are freshwater sediment organisms
with no known relation to explosives degradation. The unique band
in the wet treatment after 11 weeks was most similar (96%) to the S.
kofuensis 16S rRNA gene (AJ634661.1), a lactic acid bacteria present
in the soil but with no known ability to degrade explosives [24].
Nevertheless, it appears from Fig. 7 that the population changes
with time. The complete divergence of samples after 20 weeks in
the wet treatment from the rest of the samples showed that overall, water content was the most important factor in the evolution
of microbial populations during the experiment. The inability to
detect 16S rRNA gene sequences belonging to known explosives
degraders prevented us from assessing the effects of explosives
concentration on the microbial population. A functional marker for
genes involved in TNT, RDX and HMX degradation would be useful
in future work.
5. Conclusions
We found that the soil’s indigenous microbial population can
degrade TNT, RDX and HMX in a mixture, under conditions that
reflect the natural conditions of the contaminated vadose zone. The
degradation was shown to be strongly affected by soil water content and consequently, redox conditions. While the degradation of
TNT occurred, in these experiments, under both aerobic and anaerobic conditions, the degradation of RDX and HMX occurred only
when water-content conditions resulted in a prolonged period of
Author's personal copy
340
S. Sagi-Ben Moshe et al. / Journal of Hazardous Materials 203–204 (2012) 333–340
negative redox potential. These conditions usually developed under
saturation, but could also develop temporarily in soil micro-sites
under moderate water content and thus promote RDX and HMX
degradation.
Acknowledgments
We would like to acknowledge the Israel Water Authority as
well as BMBF-MOST for funding this research and Ms. Natalia
Bondarenko and Dr. Regina Goldin-Tzirkin for their technical assistance.
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