Flagella and pili of iron-oxidizing thiobacilli isolated from a uranium mine in northern ontario, Canada

Five strains of Thiobacillus ferrooxidans, which included three recent isolates from a uranium mine, possessed flagella. Three of the strains had several pili per cell. The dimensions, fine structure, and orientation of the flagella were different. Both polar and peritrichous flagella were observed, indicating strain-dependent ultrastructural variation in acidophilic thiobacilli. Neither flagella nor pili were detected in eight other strains of T. ferrooxidans and two strains of Thiobacillus acidophilus by electron microscopy, although all of the cultures contained motile cells.

Oxidative dissolution of arsenopyrite by mesophilic and moderately thermophilic acidophiles

The purpose of this work was to determine solution- and solid-phase changes associated with the oxidative leaching of arsenopyrite (FeAsS) by Thiobacillus ferrooxidans and a moderately thermoacidophilic mixed culture. Jarosite [KFe(3)(SO(4))(2)(OH)(6)], elemental sulfur (S), and amorphous ferric arsenate were detected by X-ray diffraction as solid-phase products. The oxidation was not a strongly acid-producing reaction and was accompanied by a relatively low redox level. The X-ray diffraction lines of jarosite increased considerably when ferrous sulfate was used as an additional substrate for T. ferroxidans. A moderately thermoacidophilic mixed culture oxidized arsenopyrite faster at 45 degrees C than did T. ferroxidans at 22 degrees C, and the oxidation was accompanied by a nearly stoichiometric release of Fe and As. The redox potential was initially low but subsequently increased during arsenopyrite oxidation by the thermoacidophiles. Jarosite, S, and amorphous ferric arsenate were also formed under these conditions.

Microbiological oxidation of ferrous iron at low temperatures

Acidophilic iron-oxidizing bacteria were enriched from mine water samples with ferrous sulfate as the substrate at incubation temperatures in the range of 4 to 46 degrees C. After several subcultures at each test temperature except 46 degrees C, which was prohibitive to growth, the rates of iron oxidation were determined in batch cultures. The results yielded linear rates in a semilogarithmic scale. The rate constants of iron oxidation by growing cultures were fitted into the Arrhenius equation, which displayed linearity in the 4 to 28 degrees C range and yielded an activation energy value of 83 +/- 3 kJ/mol.

Kinetics of sulfur oxidation at suboptimal temperatures

Chemolithoautotrophic bacteria were enriched from mine water at incubation temperatures ranging from 4 to 46 degrees C, using elemental sulfur as a substrate in acid mineral salts media. Thiobacillus-type bacteria were successfully enriched for at all test temperatures except 46 degrees C. Changes in pH (-dpH/dt) were used to estimate the rate constants for the enrichment cultures. The rate constants yielded a linear Arrhenius plot, an activation energy of 65 kJ/mol, and a temperature coefficient (Q(10)) of 2.1 for the 4 to 37 degrees C temperature interval.

Screening of human enteric microorganisms for potential biotransformation of polycyclic aromatic hydrocarbons

This study examined the potential for metabolism of select polycyclic aromatic hydrocarbons (PAH) by human enteric microorganisms. Experiments were performed under anaerobic conditions with various combinations of enteric microbial suspensions, PAH concentrations, nutrient mixtures, and time courses. No PAH metabolites were detected upon GC-TOF-MS analysis of samples digested by tetramethylammonium hydroxide thermochemolysis. No mineralization of (14)C-labeled phenanthrene was observed. These results suggest the lack of partial or complete metabolism of PAHs by enteric microorganisms and therefore the absence of major bioactivation pathways that would expose intestinal lining to potentially carcinogenic PAH metabolites.

Growth of sulfate-reducing bacteria with solid-phase electron acceptors

Hannebachite (CaSO3 x 0.5H2O), gypsum (CaSO4 x 2H2O), anglesite (PbSO4), and barite (BaSO4) were tested as electron acceptors for sulfate-reducing bacteria with lactate as the electron donor. Hannebachite and gypsum are commonly associated with flue gas desulfurization products, and anglesite is a weathering product found in lead mines. Barite was included as the most insoluble sulfate. Growth of sulfate-reducing bacteria was monitored by protein and sulfide (dissolved H2S and HS-) measurements. Biogenic sulfide formation occurred with all four solid phases, and protein data confirmed that bacteria grew under these electron acceptor conditions. Sulfide formation from gypsum was almost comparable in rate and quantity to that produced from soluble sulfate salt (Na2SO4); hannebachite reduction to sulfide was not as fast. Anglesite as the electron acceptor was also reduced to sulfide in the solution phase and galena (PbS) was detected in solids retrieved from spent cultures. Barite as the electron acceptor supported the least amount of growth and H2S formation. The results demonstrate that low-solubility crystalline phases can be biologically reactive under reducing conditions. Furthermore, the results demonstrate that galena precipitation through sulfide production by sulfate-reducing bacteria serves as a lead enrichment mechanism, thereby also alleviating the potential toxicity of lead. In view of the role of acidophilic thiobacilli in the oxidation of sulfides, the present work accentuates the role of anaerobic and aerobic microbes in the biogeochemical cycling of solid-phase sulfates and sulfides.

Characterization of chemotactic responses and flagella of Hyphomicrobium strain W1-1B

Motile swarmer cells of Hyphomicrobium strain W1-1B displayed positive chemotactic responses toward methylamine, dimethylamine, and trimethylamine but did not display significant chemotactic responses towards methanol and arginine. Electron micrographs of negatively stained intact flagellar filaments indicated a novel striated surface pattern. The flagella were composed of two proteins of 39 and 41 kDa. Neither protein was a glycoprotein as determined by Schiff's staining and by enzyme immunoassay. Protein fingerprints visualized from silver-stained polyacrylamide gels and Western blots of protease-digested samples indicated that the two proteins were similar but not identical. Monoclonal antibodies prepared to the complex flagella of Rhizobium meliloti cross-reacted with the striated flagella of Hyphomicrobium strain W1-1B; however, these antibodies did not cross-react with smooth-surface flagella. These results suggest that complex and striated flagella possess homologous epitope regions.

Biodegradation of the acetanilide herbicides alachlor, metolachlor, and propachlor

Alachlor, metolachlor, and propachlor are detoxified in biological systems by the formation of glutathione-acetanilide conjugates. This conjugation is mediated by glutathione-S-transferase, which is present in microorganisms, plants, and mammals. Other organic sulfides and inorganic sulfide also react through a nucleophilic attack on the 2-chloro group of acetanilide herbicides, but the products are only partially characterized. Sorption in soils and sediments is an important factor controlling the migration and bioavailability of these herbicides, while microbial degradation is the most important factor in determining their overall fate in the environment. The biodegradation of alachlor and metolachlor is proposed to be only partial and primarily cometabolic, and the ring cleavage seems to be slow or insignificant. Propachlor biodegradation has been reported to proceed to substantial (> 50%) mineralization of the ring structure. Reductive dechlorination may be one of the initial breakdown mechanisms under anaerobic conditions. Aerobic and anaerobic transformation products vary in their polarity and therefore in soil binding coefficient. A catabolic pathway for chloroacetanilide herbicides has not been presented in the literature because of the lack of mineralization data under defined cultural conditions.

Phylogenetic and narG analysis of a Hyphomicrobium isolate

An obligately methylotrophic organism was isolated from a water well that manifested symptoms of biofouling. The isolate was appendaged and utilized methylamine, dimethylamine, trimethylamine, or methanol as the sole carbon and energy source. The isolate exhibited hydroxypyruvate reductase activity, suggesting C1-assimilation via the serine pathway. Fatty acid profiling indicated the predominance of 18:1 cis-fatty acids. The isolate did not grow anaerobically with nitrate as the final electron acceptor. Genomic DNA from the isolate did not hybridize against the narG gene, which encodes the alpha subunit of dissimilatory nitrate reductase in Escherichia coli. The phenotypic data suggested the assignment of the isolate to the genus Hyphomicrobium. The identification was supported by phylogenetic characterization based on 16S rRNA sequence comparisons of the isolate.

Insertion sequence IST3091 of Thiobacillus ferrooxidans

An insertion sequence, designated as IST3091, was located adjacent to the putative origin of replication region of plasmid pTFI91 of Thiobacillus ferrooxidans TFI-91. The DNA sequence of the transposase gene of IST3091 revealed similarity with that of IS30, IS1086, IS4351, and the integrase gene of SpV1-R8A2 B (a bacteriophage of Spiroplasma citri). The sequence of IST3091 is 1063 bp long with partially matched 30-bp terminal inverted repeats. Several restriction fragments of plasmid pTFI91 of T. ferrooxidans containing the IST3091 element were cloned into the vector pHSG398. The hybrid plasmids (pBTL) were transformed into Escherichia coli NK7379 containing a miniF plasmid, which was devoid of transposable elements. The transposition function of the IST3091 element was confirmed by mobilizing hybrid plasmids via conjugation from transformed E. coli NK7379 (donor) to E. coli M8820 (recipient). The presence of the transposed element in transconjugants was detected by polymerase chain reaction amplification.

Biodegradation of atrazine in surface soils and subsurface sediments collected from an agricultural research farm

The purpose of the present study was to assess atrazine (2-chloro-4-ethylamino-6-isopropylamino-s-triazine) mineralization by indigenous microbial communities and to investigate constraints associated with atrazine biodegradation in environmental samples collected from surface soil and subsurface zones at an agricultural site in Ohio. Atrazine mineralization in soil and sediment samples was monitored as 14CO2 evolution in biometers which were amended with 14C-labeled atrazine. Variables of interest were the position of the label ([U-14C-ring]-atrazine and [2-14C-ethyl]-atrazine), incubation temperature (25 degrees C and 10 degrees C), inoculation with a previously characterized atrazine-mineralizing bacterial isolate (M91-3), and the effect of sterilization prior to inoculation. In uninoculated biometers, mineralization rate constants declined with increasing sample depth. First-order mineralization rate constants were somewhat lower for [2-14C-ethyl]-atrazine when compared to those of [U-14C-ring]-atrazine. Moreover, the total amount of 14CO2 released was less with [2-14C-ethyl]-atrazine. Mineralization at 10 degrees C was slow and linear. In inoculated biometers, less 14CO2 was released in [2-14C-ethyl]-atrazine experiments as compared with [U-14C-ring]-atrazine probably as a result of assimilatory incorporation of 14C into biomass. The mineralization rate constants (k) and overall extents of mineralization (Pmax) were higher in biometers that were not sterilized prior to inoculation, suggesting that the native microbial populations in the sediments were contributing to the overall release of 14CO2 from [U-14C-ring]-atrazine and [2-14C-ethyl]-atrazine. A positive correlation between k and aqueous phase atrazine concentrations (Ceq) in the biometers was observed at 25 degrees C, suggesting that sorption of atrazine influenced mineralization rates. The sorption effect on atrazine mineralization was greatly diminished at 10 degrees C. It was concluded that sorption can limit biodegradation rates of weakly-sorbing solutes at high solid-to-solution ratios and at ambient surface temperatures if an active degrading population is present. Under vadose zone and subsurface aquifer conditions, however, low temperatures and the lack of degrading organisms are likely to be primary factors limiting the biodegradation of atrazine.

Microbiological degradation of the herbicide dicamba

Pseudomonas paucimobilis was isolated from a consortium which was capable of degrading dicamba (3,6-dichloro-2-methoxybenzoic acid) as the sole source of carbon. The degradation of dicamba by P. paucimobilis and the consortium was examined over a range of substrate concentration, temperature, and pH. In the concentration range of 100-2000 mg dicamba L-1 (0.5-9.0 mM), the degradation was accompanied by a stoichiometric release of 2 mol of Cl- per mol of dicamba degraded. The cultures had an optimum pH 6.5-7.0 for dicamba degradation. Growth studies at 10 degrees C, 20 degrees C, and 30 degrees C yielded activation energy values in the range of 19-36 kcal mol-1 and an average of Q10 value of 4.0. Compared with the pure culture P. paucimobilis, the consortium was more active at the lower temperature.

Characterization of the pTFI91-family replicon of Thiobacillus ferrooxidans plasmids

Plasmids found in six strains of Thiobacillus ferrooxidans were mapped and compared in an effort to detect the origin of replication. Four strains yielded an identical 9.8-kb plasmid, pTFI91. Restriction mapping and Southern blot hybridization analysis were used to confirm this finding. Dissimilar plasmids found in two other strains contained a conserved 2.2-kb SacI region common to pTFI91. DNA sequence analysis of this region showed structural features common to bacterial plasmid replicons. A comparison of the pTFI91 origin with those of T. ferrooxidans pTF-FC2 and other broad host range vectors did not show significant homologous DNA sequences. To verify the replication function, a chloramphenicol acetyl transferase marker gene was ligated at the unique sites of pTFI91, and the plasmid was transformed into Escherichia coli DH5 alpha cells but no transformants were identified. To test the replication of pTFI91 independent of DNA polymerase I in E. coli, different restriction fragments of pTFI91 were cloned into pHSG398 (Cmr, ColEI origin) and transformed into the polA1 mutant SF800, but chloramphenicol-resistant transformants were not detected. Electrotransformation of T. ferrooxidans TFI-70 and Pseudomonas putida ATCC 19151 also failed to yield transformants. The results suggested that the pTFI91 plasmid replicon does not function either in E. coli or in P. putida. Since pTFI91 contains the same origin of replication as other plasmids in several other T. ferrooxidans strains, this replicon may be commonly distributed in T. ferrooxidans.

Degradation and mineralization of atrazine by a soil bacterial isolate

An atrazine-degrading bacterial culture was isolated from an agricultural soil previously impacted by herbicide spills. The organism was capable of using atrazine under aerobic conditions as the sole source of C and N. Cyanuric acid could replace atrazine as the sole source of N, indicating that the organism was capable of ring cleavage. Ring cleavage was confirmed in 14CO2 evolution experiments with [U-14C-ring]atrazine. Between 40 and 50% of ring-14C was mineralized to 14CO2. [14C]biuret and [14C]urea were detected in spent culture media. Cellular assimilation of 14C was negligible, in keeping with the fully oxidized valence of the ring carbon. Chloride release was stoichiometric. The formation of ammonium during atrazine degradation was below the stoichiometric amount, suggesting a deficit due to cellular assimilation and metabolite-N accumulation. With excess glucose and with atrazine as the sole N source, free ammonium was not detected, suggesting assimilation into biomass. The organism degraded atrazine anaerobically in media which contained (i) atrazine only, (ii) atrazine and glucose, and (iii) atrazine, glucose, and nitrate. To date, this is the first report of a pure bacterial isolate with the ability to cleave the s-triazine ring structure of atrazine. It was also concluded that this bacterium was capable of dealkylation, dechlorination, and deamination in addition to ring cleavage.

Maximum Temperature Limits for Acidophilic, Mesophilic Bacteria in Biological Leaching Systems

The maximum temperature for growth ( T max ) was determined for pure and mixed cultures of acidophilic thiobacilli. The experimental system was based on incubating the cultures in liquid media exposed to a linear temperature gradient. The T max values varied within the range of 36.1 to 43.6°C.

Nutrient Effect on the Biological Leaching of a Black-Schist Ore

The purpose of the study was to examine the influence of inorganic N (NH 4 + , NO 3 - ) and phosphate on the biological oxidation of a sulfidic black-schist ore which contained pyrrhotite as the main iron sulfide. Iron was initially solubilized as Fe 2+ from the ore and subsequently oxidized to Fe 3+ in shake flask experiments. Under these experimental conditions, iron dissolution from pyrrhotite was mainly a chemical reaction, with some enhancement by bacteria, whereas the subsequent Fe 2+ oxidation was bacterially mediated, with negligible contribution from chemical oxidation. Phosphate amendment did not enhance Fe 2+ oxidation. Chemical analysis of leach solutions with no exogenous phosphate revealed that phosphate was solubilized from the black-schist ore. Ammonium amendment (6 mM) enhanced Fe 2+ oxidation, whereas the addition of nitrate (6 and 12 mM) had a negative effect. An increase in the temperature from 30 to 35°C slightly enhanced Fe 2+ oxidation, but the effect was statistically not significant. The precipitation of potassium jarosite was indicative of Fe 2+ oxidation and was absent in nitrate-inhibited cultures because of the lack of Fe 2+ oxidation. The black-schist ore also contained phlogopite, which was altered to vermiculite in iron-oxidizing cultures.

Mineral Products of Pyrrhotite Oxidation by Thiobacillus ferrooxidans

The biological leaching of pyrrhotite (Fe 1- x S) by Thiobacillus ferrooxidans was studied to characterize the oxidation process and to identify the mineral weathering products. The process was biphasic in that an initial phase of acid consumption and decrease in redox potential was followed by an acid-producing phase and an increase in redox potential. Elemental S was one of the first products of pyrrhotite degradation detected by X-ray diffraction. Pyrrhotite oxidation also yielded K-jarosite [KFe 3 (SO 4 ) 2 (OH) 6 ], goethite (α-FeOOH), and schwertmannite [Fe 8 O 8 (OH) 6 SO 4 ] as solid-phase products. Pyrrhotite was mostly depleted after 14 days, whereas impurities in the form of pyrite (cubic FeS 2 ) and marcasite (orthorhombic FeS 2 ) accumulated in the leach residue.

Role of divalent cations in the subunit associations of complex flagella from Rhizobium meliloti

Rhizobium meliloti, a symbiotic, nitrogen-fixing soil bacterium with complex flagella, as well as other members of the family Rhizobiaceae, rapidly lost motility when suspended in buffers lacking divalent cations but retained good motility in buffers containing calcium, magnesium, barium, or strontium. Loss of motility was associated with loss of flagella from the cells. Analysis of flagella by sedimentation, gel electrophoresis, and electron microscopy revealed that removal of divalent cations from the complex flagella of R. meliloti resulted in extensive dissociation of the flagellar filaments into low-molecular-weight subunits. Accordingly, divalent cations such as calcium and magnesium that are normally present at high concentrations in the soil solution may be crucial to the assembly and rigidity of complex flagella.

Solid-Phase Products of Bacterial Oxidation of Arsenical Pyrite

Bacterial leaching of an As-containing pyrite concentrate produced acidic (pH < 1) leachates. During the leaching, the bacteria solubilized both As and Fe, and these two elements were distributed in solution-phase and solid-phase products. Jarosite and scorodite were the exclusive crystalline products in precipitate samples from the bacterial leaching of the sulfide concentrate.

Bacterial Oxidation of Sulfide Minerals in Column Leaching Experiments at Suboptimal Temperatures

The purpose of the work was to quantitatively characterize temperature effects on the bacterial leaching of sulfide ore material containing several sulfide minerals. The leaching was tested at eight different temperatures in the range of 4 to 37°C. The experimental technique was based on column leaching of a coarsely ground (particle diameter, 0.59 to 5 mm) ore sample. The experimental data were used for kinetic analysis of chalcopyrite, sphalerite, and pyrrhotite oxidation. Chalcopyrite yielded the highest (73 kJ/mol) and pyrrhotite yielded the lowest (25 kJ/mol) activation energies. Especially with pyrrhotite, diffusion contributed to rate limitation. Arrhenius plots were also linear for the reciprocals of lag periods and for increases of redox potentials ( d mV/ dt ). Mass balance analysis based on total S in leach residue was in agreement with the highest rate of leaching at 37 and 28°C. The presence of elemental S in leach residues was attributed to pyrrhotite oxidation.

Chemical inactivation of microorganisms on rigid gas permeable contact lenses

The efficiency of four contact lens disinfectant formulations was tested against three types of bacteria (Pseudomonas aeruginosa, Staphylococcus aureus, and Serratia marcescens) and one fungus (Aspergillus niger). The bacteria were tested both as free suspensions and after attachment on surfaces of rigid gas permeable contact lenses (RGPCL). The disinfection data were used to calculate the death rates and decimal reduction times for the test organisms. P. aeruginosa was the most sensitive and A. niger was the most resistant organism to the disinfectants. Scanning electron micrographs showed that P. aeruginosa occurred mostly as single cells, with little extracellular material, on the lens surface. In contrast, S. marcescens produced copious amounts of capsular material layered on the lens surface, promoting cell aggregation. Transmission electron micrographs revealed that bacterial cells were physically separated from the lens surface by a space barricaded with capsular material.

Microbiological degradation of pesticides in yard waste composting

Changes in public opinion and legislation have led to the general recognition that solid waste treatment practices must be changed. Solid-waste disposal by landfill is becoming increasingly expensive and regulated and no longer represents a long-term option in view of limited land space and environmental problems. Yard waste, a significant component of municipal solid waste, has previously not been separated from the municipal solid-waste stream. The treatment of municipal solid waste including yard waste must urgently be addressed because disposal via landfill will be prohibited by legislation. Separation of yard waste from municipal solid waste will be mandated in many localities, thus stressing the importance of scrutinizing current composting practices in treating grass clippings, leaves, and other yard residues. Yard waste poses a potential environmental health problem as a result of the widespread use of pesticides in lawn and tree care and the persistence of the residues of these chemicals in plant tissue. Yard waste containing pesticides may present a problem due to the recalcitrant and toxic nature of the pesticide molecules. Current composting processes are based on various modifications of either window systems or in-vessel systems. Both types of processes are ultimately dependent on microbial bioconversions of organic material to innocuous end products. The critical stage of the composting process is the thermophilic phase. The fate and mechanism of removal of pesticides in composting processes is largely unknown and in need of comprehensive analysis.

Detection and identification of substituted phenols as intermediates of concurrent bacterial degradation of the phenoxy herbicides MCPP and 2,4-D

The concurrent bacterial degradation of 2-(2-methyl-4-chlorophenoxy)propionic acid and 2,4-dichlorophenoxyacetic acid was studied using a stirred tank reactor and a bacterial culture which had been originally derived by enrichment with MCPP. High pressure liquid chromatographic methodology was used to measure both herbicides and it also resolved the corresponding phenols as intermediates, i.e., 2-methyl-4-chlorophenol and 2,4-dichlorophenol. Gas chromatography-mass spectrometry was used to verify the intermediates. UV scans of spent cultures showed that the wave-length of maximum absorption shifted from 282 nm to 280 nm toward the end of incubation, but the characteristic peaks of maximum absorption of these compounds could not be used resolved because of the overlap.

Quantitative enumeration of acanthamoeba for evaluation of cyst inactivation in contact lens care solutions

A simple, quantitative plate assay has been developed for use in the enumeration of Acanthamoeba. The technique uses an agarose overlay and low-nutrient medium to support the growth of amoebae on a bacterial lawn. The authors found that in this assay, individual trophozoites or dormant cysts will cause plaques to form in an Enterobacter aerogenes lawn. With the assay, it is possible to quantitatively assess the effects of various disinfectant compounds on the viability of Acanthamoeba. The authors used this assay to enumerate Acanthamoeba cyst viability after chemical disinfection in contact lens care solutions. The inactivation data indicated major differences among the four test solutions evaluated.

Temperature Effects on Bacterial Leaching of Sulfide Minerals in Shake Flask Experiments

The microbiological leaching of a sulfide ore sample was investigated in shake flask experiments. The ore sample contained pyrite, pyrrhotite, pentlandite, sphalerite, and chalcopyrite as the main sulfide minerals. The tests were performed at eight different temperatures in the range of 4 to 37°C. The primary data were used for rate constant calculations, based on kinetic equations underlying two simplified models of leaching, i.e., a shrinking particle model and a shrinking core model. The rate constants thus derived were further used for the calculation of activation energy values for some of the sulfide minerals present in the ore sample. The chalcopyrite leaching rates were strongly influenced by the interaction of temperature, pH, and redox potential. Sphalerite leaching could be explained with the shrinking particle model. The data on pyrrhotite leaching displayed good fit with the shrinking core model. Pyrite leaching was found to agree with the shrinking particle model. Activation energies calculated from the rate of constants suggested that the rate-limiting steps were different for the sulfide minerals examined; they could be attributed to a chemical or biochemical reaction rather than to diffusion control.

Biological degradation of 2,4-dichlorophenoxyacetic acid: chloride mass balance in stirred tank reactors

A mass balance was developed for the degradation of 2,4-dichlorophenoxyacetic acid by a mixed culture. Batch culture experiments showed the degradation to be an acid-producing step. Inorganic chloride concentration consistently correlated with the expected value and with base consumption to maintain a constant pH.

Protein and elemental analysis of contact lenses of patients with superior limbic keratoconjunctivitis or giant papillary conjunctivitis

Soft contact lenses worn by six patients (12 eyes) diagnosed as having contact lens-induced superior limbic keratoconjunctivitis (SLK) and from four patients (5 eyes) with giant papillary conjunctivitis (GPC) were analyzed for protein concentration and for elemental content. Fifty-five percent water content, ionic lenses containing methacrylic acid had high protein concentration. Calcium was not a common element found on protein-coated lenses. Sulfur and iron were found on used and new lenses. An elevated level of mercury was detected in one gray lens that had been disinfected in thimerosal-preserved saline with a high heat disinfection unit by a patient with SLK.

Fast Kinetics of Fe 2+ Oxidation in Packed-Bed Reactors

Thiobacillus ferrooxidans was used in fixed-film bioreactors to oxidize ferrous sulfate to ferric sulfate. Glass beads, ion-exchange resin, and activated-carbon particles were tested as support matrix materials. Activated carbon was tested in both a packed-bed bioreactor and a fluidized-bed bioreactor; the other matrix materials were used in packed-bed reactors. Activated carbon displayed the most suitable characteristics for use as a support matrix of T. ferrooxidans fixed-film formation. The reactors were operated within a pH range of 1.35 to 1.5, which effectively reduced the amount of ferric iron precipitation and eliminated diffusion control of mass transfer due to precipitation. The activated-carbon packed-bed reactor displayed the most favorable biomass holdup and kinetic performance related to ferrous sulfate oxidation. The fastest kinetic performance achieved with the activated-carbon packed-bed bioreactor was 78 g of Fe 2+ oxidized per liter per h (1,400 mmol of Fe 2+ oxidized per liter per h) at a true dilution rate of 40/h, which represents a hydraulic retention time of 1.5 min.

Characterization of Jarosite Formed upon Bacterial Oxidation of Ferrous Sulfate in a Packed-Bed Reactor

A packed-bed bioreactor with activated-carbon particles as a carrier matrix material inoculated with Thiobacillus ferrooxidans was operated at a pH of 1.35 to 1.5 to convert ferrous sulfate to ferric sulfate. Despite the low operating pH, trace amounts of precipitates were produced in both the reactor and the oxidized effluent. X-ray diffraction and chemical analyses indicated that the precipitates were well-ordered potassium jarosite. The chemical analyses also revealed a relative deficiency of Fe and an excess of S in the reactor sample compared with the theoretical composition of potassium jarosite.

Evaluation of contact lenses by microbial enumeration and protein determination

Contact lenses worn for varying periods of time (from 1 to 48 months) were subjected to microbiological examination by plate counts and protein determination. Seventy percent of the lenses displayed bacterial colony counts below 120 colony-forming units (CFU)/lens, 28 percent were in the range of 140 to 9060 CFU/lens, and one lens was contaminated with greater than 6 x 10(4) CFU/lens. Fungal contaminants were detected in three lens specimens in the range of 220 to 760 CFU/lens. Protein accumulation showed wide variation of up to 1.2 mg of protein per lens. Statistical analysis indicated highly significant associations (p less than 0.001) between the bacterial colony counts obtained with three different media. Some significant associations were found between the protein concentration and bacterial counts. The data did not indicate statistically significant relations between the above variables and either the water content or the length of wear of the contact lenses.

Effects of refrigeration on daily microbial bioburden of hydrogel lenses

Microbial bioburden of contact lenses was evaluated in connection with lens care by refrigeration. Subjects wore new hydrogel contact lenses for approximately 8 hours. The microbial bioburden initially and after an overnight refrigeration of the lens was evaluated with the use of viable counts on three different media. No major changes in viable counts were observed resulting from this method of storage. Scanning electron microscopy indicated the presence of foreign material on both new and worn lenses, presumed to be debris from lens manufacture and mucoid deposits from daily wear. Microbial colonization was not apparent and single bacterial cells could not be discerned on the micrographs.

Inhibitor Evaluation with Immobilized Nitrobacter agilis Cells

Nitrobacter agilis was entrapped in calcium alginate beads and used as a floating bed supplied with a continuous flow of nitrite medium. Complete nitrite oxidation was achieved within 30 h, and the system could be maintained for at least 210 h. The immobilized Nitrobacter system was subjected to sulfur oxyanions, acidity, and metal ions. Thiosulfate and tetrathionate (up to 20 mM each) did not inhibit the nitrite oxidation activity. A low pH of 4.2 resulted in the complete cessation of nitrite oxidation, and the activity was not restored upon increasing the pH to 7. Nitrite oxidation by N. agilis was sensitive to 10 mM each Ni 2+ and Al 3+ but insensitive to 10 mM MoO 4 2− .

Aerobic and anaerobic microorganisms in tubercles of the Columbus, Ohio, water distribution system

Aerobic and anaerobic microorganisms were enumerated in tubercles collected from sections of the water distribution pipeline in the Columbus, Ohio, metropolitan area. Coliform bacteria were not detected in the tubercles examined. Sulfate-reducing bacteria were detected in 80% of the samples. Nitrate-reducing heterotrophs were present in all samples. The results, including plate counts of aerobic heterotrophs, indicated variation in bacterial densities depending on the tubercle sample and fraction examined. The associations among the viable counts obtained by the different culture methods were analyzed statistically, using three methods (Pearson, Spearman, and Kendall).

Plasmid DNA in acidophilic, chemolithotrophic thiobacilli

Plasmid patterns were determined in 15 strains of iron-oxidizing Thiobacillus ferrooxidans. In four of these strains plasmid DNA was not detected. In the other strains the molecular weights of plasmids ranged from 5 x 10(6) to 50 x 10(6) and each strain had a different plasmid composition. The change of growth substrate from ferrous iron to tetrathionate did not affect the plasmid pattern in T. ferrooxidans nor did it in T. acidophilus, which was adapted from glucose to grow on tetrathionate.

Nitrogen Requirement of Iron-Oxidizing Thiobacilli for Acidic Ferric Sulfate Regeneration

Ammonium was shown to be a limiting nutrient for iron oxidation in cultures of Thiobacillus ferrooxidans. In addition, one strain was also able to assimilate nitrate, but not nitrite, for growth and coupled iron oxidation. Some amino acids (0.5 mM) were tested as a source of nitrogen; none clearly stimulated bacterial activity and inhibition was commonly encountered. Complex nitrogenous compounds were inhibitory at high concentrations (0.1 to 0.5%, wt/vol) and, at low concentrations, some clearly stimulated the bacterial iron oxidation in ammonium-limited cultures. Enhancement of iron oxidation by these compounds was also observed in ammonium-unlimited cultures, suggesting their possible role in providing trace nutrients and possibly carbon for the bacteria.

Microscopic examination of bacteria in Fe(III)-oxide deposited from ground water

Ochreous sludge deposited in the course of aeration of ground water contained an assortment of bacterial forms and structures which were investigated by light microscopy, scanning electron microscopy, and transmission electron microscopy. Bacterial structures were often covered by iron deposition which could be removed by acidification of the samples. Sulfuric acid treatment was consistently better than hydrochloric acid to dissolve iron without a considerable damage to the bacterial cells. Partial dissolution of amorphous ferric iron was achieved by acidifying the samples with oxalic acid or citric acid prior to the preparation for electron microscopy.

A method for the preparation of solidified colloidal sulphur media

The chemical reaction between tetrathionate and sulphide produces colloidal sulphur and thiosulphate. This reaction can be employed to prepare agar media containing thiosulphate and finely divided colloidal sulphur particles.

Proton translocation in intack cells of Thiobacillus denitrificans

Proton translocation assessed by the quinacrine fluorescence technique was compared with oxygen uptake during thiosulphate oxidation by cells of Thiobacillus denitrificans. The addition of thiosulphate to cell suspensions resulted in an outwardly directed proton translocation as reflected by an increased quinacrine fluorescence. Compared to the O2 uptake activity, the proton translocating system was much more sensitive to proton conductors, other ionophores and inhibitors of electron transport. The results indicate that (a) the proton-translocation activity (membrane energization) is enhanced in aged cell suspensions, (b) intactness of the cytoplasmic membrane is essential for establishing a protonmotive force in cells, (c) the fluorescence increase and proton translocation are reversible processes, (d) inhibitors of electron transport may also act as proton conductors by altering the integrity of the cytoplasmic membrane.

Bacterial oxidation of polythionates: determination of tetrathionate with an ion-selective electrode

A commercially available ion-selective electrode for nitrate was used to continuously monitor tetrathionate oxidation by Thiobacillus dentrificans. The electrode was much more sensitive to tetrathionate than to nitrate. The same electrode could also be used for the determination of trithionate.

Utilization of 35S-thiosulphate and an appraisal of the role of ATP-sulphurylase in chemolithotrophic Thiobacillus ferrooxidans

Differentially labelled 35S-thiosulphate was taken up by washed cells of Thiobacillus ferrooxidans which were previously grown on thiosulphate. The uptake was proportional to the biomass over the range 0.5-4.0 mg dry wt. of bacteria and showed typical saturation kinetics with an estimated Km value of 0.5 mM for 35S-thiosulphate. Dithionate and Group VI anions inhibited the uptake, which was under pH control and had a temperature optimum of 50 degrees C. In the absence of thiosulphate, the cells bound 35S-sulphate but the binding did not increase on prolonged incubation and the label could be removed completely by washing with dilute sulphuric acid. Increasing amounts of the label were incorporated from [outer-35S]thiosulphate into cellular materials over a 60-min period, whereas little or no assimilation was observed from either the [inner-35S]thiosulphate or 35S-sulphate. The kinetic properties of the sulphate-activating enzyme ATP-sulphurylase enriched from bacteria grown with either thiosulphate or ferrous-iron were similar although this enzyme has an assimilatory function only when the bacterium is grown with ferrous-iron.

Degradation of sulphur nucleotides in cell-free extracts of Thiobacillus ferrooxidans

The cell-free extracts of Thiobacillus ferrooxidans contain hydrolytic enzymes which cleave sulphate from either adenosine 5'-sulphatophosphate or adenosine 3'-phosphate 5'-sulphatophosphate. These sulphatase activities may be retarded by including either phosphates or adenine nucleotides in the incubation mixtures. Adenosine 3'-phosphate 5'-sulphatophosphate and its immediate breakdown product adenosine 3'-phosphate 5'-phosphate were degraded at slower rates than adenosine 5'-sulphatophosphate.

The uptake and assimilation of sulphate by Thiobacillus ferrooxidans

Sulphate was rapidly bound by cell suspensions of Thiobacillus ferrooxidans. The binding was depressed by tetrathionate but was unaffected by Group VI anions, cysteine or methionine. Increasing uptake of sulphate was observed in cell suspensions incubated in the presence of ferrous iron. The bulk of 35S-sulphate was removed from the organisms by washing with dilute sulphuric acid and the remaining label was incorporated into cold trichloroacetic acid-soluble compounds. 35S-labelled adenosine 5'-sulphatophosphate was produced from ATP and 35S-sulphate by cell suspensions and in cell-free extracts. There was no evidence for the production of adenosine 3'-phosphate 5'-sulphatophosphate assayed by a very sensitive bioluminescence method.