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Applied and Environmental Microbiology, May 2009, p. 2899-2907, Vol. 75, No. 9
0099-2240/09/$08.00+0 doi:10.1128/AEM.01530-08
Copyright © 2009, American Society for Microbiology. All Rights Reserved.

UCD School of Chemical and Bioprocess Engineering,1 UCD School of Biomolecular Science, Centre for Synthesis and Chemical Biology, University College Dublin, Belfield, Dublin 4, Ireland2
Received 7 July 2008/ Accepted 4 March 2009
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Halogenated compounds are extensively used in many applications (refrigeration, lubricants, pharmaceuticals, insecticides, and herbicides) and can be considered significant environmental contaminants. The biodegradation of many chlorinated compounds has been widely reported (5, 26, 28). However, in spite of the increased use of organofluorine compounds in the past 60 years, there is limited information on their degradation (17). Currently, a large fraction of wastewater streams containing fluorinated compounds are incinerated (12). Improved biological waste treatment processes require a deeper understanding of microbial degradation of fluorinated compounds.
Some previous studies have focused on the biodegradation of fluorinated aromatic compounds using biofilm reactors (3, 10); however, there have been no studies on the degradation of fluorinated aliphatic compounds in biofilm reactors. Thus, sodium fluoroacetate was chosen as the model xenobiotic to study the efficiency of aliphatic organofluorine degradation in biofilms. It was the first naturally occurring fluorinated compound to be isolated, obtained from the South African shrub Dichapetalum cymosum (23). Fluoroacetate is highly toxic to mammals and has found extensive use as a vertebrate pesticide, particularly in Australia and New Zealand. A number of studies have focused on the isolation and identification of microbial soil isolates with the ability to degrade fluoroacetate (14, 33, 35), and other studies have focused on the mechanism of defluorination (13, 15, 21). However, there has been no research on the degradation of fluoroacetate by biofilm cultures. Biofilm systems appear ideal for the degradation of xenobiotics because of the many reported advantages they have over planktonic cultures. Most microorganisms that have the ability to degrade xenobiotic compounds have comparatively slow growth rates, and biofilm reactors allow the enrichment of these microorganisms independent of hydraulic retention times (36). It has been shown in numerous studies that biofilms are less susceptible than suspended bacteria to changes in environmental conditions such as temperature and pH and the presence of metabolic products and toxic substances (8, 25, 27, 36). The high cell concentrations that can be achieved in biofilm systems in combination with high volumetric flow rates could potentially result in high volumetric productivities without the risk of cell washout.
The species Pseudomonas fluorescens has been extensively studied; it commonly exists as a biofilm in natural environments and is ubiquitous in industrial environments (6, 29, 30). The specific strain used here, P. fluorescens DSM 8341, was previously isolated from a soil sample in Western Australia, and in a study with 23 other microbial soil isolates, it was shown to be the most efficient degrader of fluoroacetate when fluoroacetate was the sole carbon source (37). The effect of the environmental factors, pH and temperature, on the biodefluorination of fluoroacetate by P. fluorescens was also determined (38); however, at present there are no reported planktonic growth kinetics established for this strain, nor has it previously been grown as a biofilm. In this context a TBR was employed to investigate the degradation of fluoroacetate by a P. fluorescens biofilm, in conjunction with chemostat studies that were conducted to determine the efficiency of planktonic degradation of the substrate. Specific utilization rates, flow cytometry, and fluorescent microscopy were employed to compare the performance and physiological status of biofilm and planktonic cells grown with fluoroacetate as the sole organic substrate.
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Biofilm reactor.
The biofilm was grown in the lumen of a silicone tube (Alteil, United Kingdom), referred to as a TBR, which is schematically presented in Fig. 1. The nominal inner dimension of the silicone tubing was 3 mm, and the wall thickness was 1 mm. The system consisted of a medium reservoir, peristaltic pump, a glass flow break, four 40-cm sections of silicone tubing separated by 5 sample ports, a glass flow break, and a spent medium reservoir. This reactor configuration allowed the determination of local metabolite concentrations and biofilm characteristics, and thus each section can be considered an independent reactor. Four separate TBR experiments were performed, with concentrations of 10, 20, and 50 mM fluoroacetate in the medium feed; the 20-mM experiment was repeated. Thus, 16 different specific fluoroacetate loading rates were examined (four reactors with four sections each). Cells were grown for 24 h at 30°C in batch culture prior to reactor inoculation to ensure that the cells were in the exponential phase of growth. The 24-h culture was adjusted to a turbidity of approximately 0.1 at 660 nm in phosphate-buffered saline (PBS), mixed with 10 ml of medium, and inoculated into the reactor. Following inoculation the system was operated in static mode for approximately 48 h at 30°C, after which time the flow of medium was initiated at a flow rate of 6 ml/h (velocity, 0.023 cm/s) and maintained throughout the experiments. The dilution rate was approximately 2.5 times greater than the maximum planktonic growth rate; this was chosen to ensure the washout of planktonic cells and encourage biofilm formation. Samples were taken from the reactor daily from sample port 5 and from all five ports 24 h prior to biofilm harvesting. The following parameters were analyzed: optical density, fluoroacetate, free fluoride ion, glycolate, DNA content of cells, and CFU count. The biofilm was allowed to develop for approximately 300 h, at which time the bioreactor was disassembled, and the biofilm was harvested for analysis.
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FIG. 1. Schematic of TBR. Each section consists of 40 cm of silicone tubing, with a total reactor length of 160 m.
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Chemostat trials.
Chemostat studies were performed in duplicate in a 3-liter bioreactor (Applikon, The Netherlands) with a working volume of 1.5 liters, and the performance of planktonic cells was assessed at four fluoroacetate loading rates representing growth rates between 45 and 80% of the maximum growth rate. The reactor was equipped with controls for agitation, pH, temperature, and dissolved oxygen. For pH adjustment 1 M NaOH was used. The inlet gas flow rate was maintained at a constant rate of 1.5 liters/min by use of a mass flow controller. Dissolved oxygen was controlled by agitation and maintained at or above 40% air saturation throughout the experiments. Temperature was maintained at 30°C throughout the experiments. The reactor was inoculated with 15 ml of 24-h-old culture adjusted to an optical density of 0.1 at 660 nm. Samples were taken from the reactor periodically, and the following parameters were analyzed: optical density, fluoroacetate, free fluoride ion, glycolate, DNA content of cells, dry weight, and number of CFU. The reactor was operated under batch conditions during the exponential phase of growth; at the onset of the stationary phase of growth, the reactor was switched to continuous operation. The feed flow rate was measured by recording the mass of liquid effluent over a specified period of time using a balance (Mettler Toledo). The initial fluoroacetate concentration during the batch phases of growth was 20 mM.
Batch growth trials.
Planktonic growth rates were determined for initial fluoroacetate concentrations of 10, 20, and 50 mM in 250-ml conical flasks incubated at 30°C with shaking at 150 rpm. The flasks were operated with a working volume of 50 ml and inoculated with 0.5 ml of a 24-h-old culture adjusted to an optical density of 0.1 at 660 nm with PBS. The flasks were sampled periodically and analyzed for optical density and free fluoride ion.
Anaerobic batch culture experiments.
Anaerobic batch culture experiments were performed in triplicate with 20 mM fluoroacetate or 20 mM glycolate as the sole carbon source in 100-ml Schott Duran bottles with a working volume of 30 ml. An anaerobic environment was maintained by continuous subsurface sparging of nitrogen gas at a flow rate of 0.5 ml/min. This flow rate was found to be sufficient to ensure an anaerobic environment while also avoiding liquid losses due to evaporation over the 8-h duration of the experiment. The Duran bottles were inoculated by harvesting 30 ml of a 24-h-old culture grown on fluoroacetate; the harvested cells were then resuspended in 1 ml of fresh medium prior to inoculation. The bottles were incubated at 30°C with shaking at 150 rpm for 8 h, at which time they were sampled and analyzed for optical density, dissolved oxygen, and metabolite concentrations. There was no dissolved oxygen detected in any of the anaerobic experiments while the dissolved oxygen concentrations in the aerobic control bottles were found to be above 40% air saturation after the 8-h incubation period.
Epifluorescence microscopy.
A 5-cm section of tubing containing biofilm was washed with PBS (1 ml) and stained with 5-cyano-2,3-ditoyl tetrazolium chloride (CTC; 400 µg/ml) for 2 h at 30°C. The tubing was drained, washed with PBS (1 ml), and stained with 4',6'-diamidino-2-phenylindole (DAPI; 100 µg/ml) for 30 min at ambient temperature. The tubing was washed with PBS and embedded with 5 ml of 22-oxyacalcitriol (OCT) histological cryoembedding medium (Tissue TEK OCT compound), which was gently injected into the tubing. The tubing was then placed in an embedding chamber for 10 min to solidify the OCT, and samples were stored at –80°C until sectioning. The embedded biofilm was sectioned (10-µm cross-sections) after the biofilm was removed from the silicone tubing, using a Microm HM 550 cryostat (Microm, Walldorf, Germany). The sections were placed on glass slides and examined with an Olympus BX51 epifluorescence microscope using a 4x objective. Photographs were obtained with an Olympus DP70 digital camera. The exposure time was 500 ms to acquire CTC images and 50 ms to acquire DAPI images.
Thickness measurements and image analysis.
Biofilm thickness was analyzed by Able Image Analyser software (Mu Labs, Slovenia). Thickness was measured as the distance from the membrane to the biofilm liquid interface. From each section of the reactor, six phase-contrast images were analyzed for thickness, and 25 measurements were taken from each image. These measurements were then averaged to give a final thickness. Depth profiles of respiratory activity (CTC) and biomass (DAPI) were measured perpendicular to the membrane in overlapped CTC and DAPI images acquired at the same point. The interface between the biofilm and the membrane was set at zero. Fifteen individual profiles were performed in six different images from each section. Three representative profiles were then averaged to produce a final radial profile of respiratory activity and biomass for each section.
Dry weight.
Biofilm dry weight was determined by drying a 5-cm section of tubing at 60°C for 48 h, at which point a constant weight was achieved. The tubing was immersed in warm water to hydrate the biofilm, and the biofilm was removed by pinching the silicone tubing, which was then washed vigorously with water to remove any residual biofilm. The silicone tubing was dried for a further 48 h and reweighed. The weight of the biofilm was calculated by subtracting the dry weight of the empty tubing from the weight of the tubing plus biofilm.
Specific utilization rate.
The specific utilization rate (q) is defined as the concentration of substrate degraded per unit time per CFU. The utilization of a carbon/energy substrate is separated into two fluxes (Fig. 2) corresponding to consumption of the substrate for incorporation into biomass (qan) and utilization of substrate for energy, which can be further subdivided into the energy required for growth (qen) and energy required for maintenance (qm). In some cases it is possible that there is a rate-limiting step in the overall catabolic pathways, which leads to the accumulation of an intermediate metabolite and is described here as overflow metabolism. Fluoroacetate was the sole organic substrate available to the cells. It is initially degraded by the enzyme fluoroacetate dehalogenase (Fig. 3), yielding free fluoride ion and glycolate; glycolate is then utilized as the carbon/energy source. Figure 3 shows that carbon is conserved in the fluoroacetate dehalogenase reaction; thus, there are two specific utilization rates: qf is the specific utilization rate of fluoroacetate, which is a single enzymatic reaction that results in the production of glycolate, and qg is the specific utilization rate of glycolate consumed for the production of cell material (qan) and ATP generation (qen and qm). Unconsumed glycolate (overflow metabolism) is transported across the cell membrane into the bulk liquid. In order to compare qf and qg directly, specific utilization rates were calculated as the concentration (in mM) of carbon.
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FIG. 2. The utilization of fluoroacetate involves the enzymatic cleavage of the carbon-fluorine bond with the production of glycolate. The specific utilization rate of glycolate, qg, is a combination of qan where carbon is incorporated into cell (anabolism), qen, where carbon is used to provide energy for growth, and qm, where carbon is used to provide energy for the maintenance of cellular function not associated with growth (maintenance of intracellular osmotic potential) but excludes any glycolate that is produced but not utilized (overflow metabolism [Om]) and represents the total carbon utilized. The specific fluoroacetate utilization rate includes qan, qe, qm, and Om and represents the total fluoroacetate degraded.
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FIG. 3. Fluoroacetate defluorination via haloacetate dehalogenase.
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FIG. 4. Typical histogram of fluorescent intensity for planktonic cells. Multicycle software was used to determine the B, C, and D phases of the cell cycle. B-phase cells have a single copy of DNA, C-phase cells are synthesizing DNA, and D-phase cells have a double copy of DNA and are predivision.
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Visual observations of the biofilm formation provides some qualitative information as to when initial biofilm formation occurs, and measured metabolite concentrations throughout the time course of the experiments indicate when steady-state conditions have been reached, but these data do not provide any quantitative measurement of biofilm structure or performance. Thus, biofilm characteristics of thickness, dry weight, cell number, and density were calculated at different sections of the reactor (Fig. 1) for different carbon loading rates after biofilm harvesting (Table 1). Cross-sectional biofilm thickness was calculated from phase-contrast images. These thickness measurements show little variation in the average biofilm thickness for all sections where the carbon loading rates were above 0.017 mM/h; the average thickness was 116.8 µm, with a standard deviation around the mean of ± 22.9 µm. An exception to this trend was the section with a carbon loading rate of 0.107 mM/h, where the average thickness was 130 µm thicker than that recorded in any other section. The same trends observed for average thickness were observed for dry weight, CFU count, and density measurements, with a few exceptions, most notably for the section with a carbon loading rate of 0.107 mM/h. Images taken from the section with this carbon loading rate suggest that the biofilm may have been in the process of sloughing, and this could explain the greater thickness and lower density values recorded in this section. The reactor experiment using 20 mM fluoroacetate was performed in duplicate, and single-factor analysis of variance showed that there was no significant difference between biofilm thickness, dry weight, cell number, and density values recorded in these two reactors (F = 0.15, F critical = 4.7, and P = 0.69). Biofilm was present in three individual sections of the reactors where the carbon loading rate was 0 mM/h as a result of carbon source depletion, and in these sections the presence of biofilm was probably caused by the presence of carbon during the early stages of the reactor operation.
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TABLE 1. Biofilm thickness, dry weight, CFU count, and density data after approximately 300 h of growth at various carbon loading ratesa
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FIG. 5. Specific fluoroacetate () and glycolate ( ; shown with the symbol for fluoroacetate superimposed) utilization rates for planktonic cells and specific fluoroacetate ( ) and glycolate ( ) utilization rates for biofilm cells at various specific fluoroacetate loading rates. Regression analysis shows the superior performance of planktonic cells (slope = 0.87; R2 = 0.90) in comparison to biofilm cells (slope = 0.57; R2 = 0.91) at specific fluoroacetate loading rates between 2 x 10–12 and 14 x 10–12 mM/CFU/h. Dashed lines, 95% confidence intervals.
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FIG. 6. Fluorescent images of biofilm stained with the respiratory indicator CTC (red) and the DNA binding dye DAPI (A) and the corresponding depth profiles of the location of respiratory activity (solid line) and biomass (dotted line) within the biofilm (B) show that respiratory activity decreases toward the biofilm-bulk liquid interface.
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FIG. 7. Cell cycle distributions for planktonic (A) and biofilm (B) cells at a number of specific glycolate utilization rates. Open bar, B phase; dark gray bar, C phase; and light gray bar, D phase. Standard deviations were determined from a minimum of three independent biological samples. Planktonic specific glycolate utilization rates between 4 to 8 and 8 to 12 mM/CFU/h correspond to growth rates of between 0.07 to 0.08 and 0.09 to 0.12 h–1, respectively.
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Here, two methods have been used to determine the physiological status and activity of planktonic and biofilm cells. First, the metabolic activities of biofilm and planktonic cells were assessed in terms of specific utilization rates. It was found that the performance of planktonic cells was superior to that of biofilm cells, with planktonic cells mineralizing more fluoroacetate per CFU per hour than the biofilm cells. When the cells were grown under planktonic conditions, there was no difference between specific fluoroacetate and specific glycolate utilization rates at any of the specific fluoroacetate loading rates examined (Fig. 5). This was not the case for the biofilm cells, and specific glycolate utilization rates were lower than their corresponding specific fluoroacetate utilization rates at a number of specific fluoroacetate loading rates. Thus, the major differences between biofilm and planktonic cells were the performance of the biofilm cells in terms of fluoroacetate and glycolate utilization and the overflow metabolism of glycolate.
It has been shown previously (7) that the fluoroacetate dehalogenase enzyme isolated from P. fluorescens does not require the presence of oxygen to degrade fluoroacetate, and in this study it has been demonstrated that the utilization of glycolate via aerobic respiration requires oxygen as a terminal electron acceptor. Thus, oxygen limitation within the biofilm offers an explanation for the overflow metabolism of glycolate. Spatial stratification of respiratory activity, as indicated by CTC, supports the possibility of oxygen limitation within the biofilm. Respiratory activity is highest at the biofilm-membrane interface and decreases toward the biofilm-bulk liquid interface (Fig. 6). This spatial stratification of nutrients within the biofilm is a major difference between biofilm and planktonic cells. For planktonic cells grown in the chemostat system, the dissolved oxygen concentration was controlled at or above 2.8 mg/liter, providing sufficient oxygen for all cells. Oxygen was supplied to the biofilm by diffusion through the silicone membrane, which also acts as a support for the biofilm. As the biofilm grows, it increasingly acts to resist the mass transfer of nutrients to the inner regions of the biofilm. Calculations of oxygen penetration depth suggest that the biofilm was sufficiently thick to prevent the penetration of oxygen to the region of the biofilm located adjacent to the bulk liquid interface, and they support the possibility of oxygen limitation.
At similar specific fluoroacetate loading rates, the specific utilization rate of fluoroacetate was lower for biofilm cells than planktonic cells. A possible explanation for this result is that less energy is available to biofilm cells due to decreased glycolate utilization; thus, there is less energy produced for, among other requirements, the production of fluoroacetate dehalogenase and for the production of any permease necessary for the transport of fluoroacetate into the cell. Therefore, a reduced glycolate utilization rate due to oxygen limitation could ultimately affect fluoroacetate utilization. This suggestion is supported by the observation that under anaerobic conditions, resting cells degraded only 1.4 mM fluoroacetate compared with 8.5 mM in resting cells incubated aerobically.
Cell cycle distributions show that there was no statistical difference in the percentage of cells in the B phase of growth at specific glycolate utilization rates between 4 x 10–12 and 8 x 10–12 mM/CFU/h for both biofilm and planktonic cells, suggesting similar growth rates (Fig. 7). If growth rates of biofilm cells were decreased in comparison to planktonic cells at similar specific glycolate utilization rates, then an increase in the number of cells occupying the B phase of growth would be expected. This was not the case, and the cells can be considered to be in a similar physiological state. While some biofilm populations had increased percentages of cells in the B phase of the cell cycle, these increases were probably due to carbon limitation as a result of the low carbon loading rates (between 0.06 x 10–12 and 2 x 10–12 mM/CFU/h) in these sections and not as a result of any intrinsic differences between the two modes of growth. The planktonic system was not operated at these low carbon loading rates, and consequently it was not possible to make comparisons between the two modes of growth at these low carbon loading rates.
In conclusion, the TBR was found to be a versatile system for determining the performance of biofilm cells. The TBR allows the determination of local metabolite concentrations and other parameters such as dry weight, CFU count, and biofilm thickness, which can then be used to assess biofilm performance. While other commonly used biofilm reactor systems such as the rotating disk reactor, the capillary biofilm reactor, and the drip flow biofilm reactor allow the determination of some of these parameters, none allows the determination of so many parameters simultaneously. The TBR system does have its limitations; most significantly, it is labor-intensive, which makes replication time-consuming. The identification of the overflow metabolism in biofilm systems could have important implications in the treatment of wastewater streams containing fluorinated compounds. In this case the overflow product was glycolate. Glycolate subsequently acted as the carbon source and did not have any detrimental effect on performance. However, the degradation of other fluorinated compounds, such as fluoroaromatics, might result in the accumulation of toxic fluorometabolites, e.g., fluorocatechol, which could detrimentally affect the performance of biofilm cells. Planktonic cells were found to be superior to biofilm cells at degrading the xenobiotic, with higher fluoroacetate and glycolate utilization rates per CFU recorded at similar specific fluoroacetate loading rates. This difference in performance can be explained by oxygen limitation in the biofilm; however, the high free-fluoride concentrations recorded in the TBR may also have a negative impact on performance. These results show that while planktonic cells were more efficient at utilizing both fluoroacetate and the intermediate metabolite glycolate, the advantages of biofilm systems for the degradation of xenobiotics, such as the enrichment of slow-growing species, may outweigh the superior performance of planktonic cells observed here.
We thank the Science Foundation Ireland (grant 04/BRG/E0072) for financial support.
Published ahead of print on 13 March 2009. ![]()
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