Biological sulphate reduction using food industry wastes as carbon sources

Biological treatment with dissimilatory sulphate-reducing bacteria has been considered the most promising alternative for decontamination of sulphate rich effluents. These wastewaters are usually deficient in electron donors and require their external addition to achieve complete sulphate reduction. The aim of the present study was to investigate the possibility of using food industry wastes (a waste from the wine industry and cheese whey) as carbon sources for dissimilatory sulphate-reducing bacteria. The results show that these wastes can be efficiently used by these bacteria provided that calcite tailing is present as a neutralizing and buffer material. A 95 and 50 % sulphate reduction was achieved within 20 days of experiment by a consortium of dissimilatory sulphate-reducing bacteria grown on media containing waste from the wine industry or cheese whey respectively. Identification of the dissimilatory sulphate-reducing bacteria community using the dsr gene revealed the presence of the species Desulfovibrio fructosovorans, Desulfovibrio aminophilus and Desulfovibrio desulfuricans. The findings of the present study emphasise the potential of using wastes from the wine industry as carbon source for dissimilatory sulphate-reducing bacteria, combined with calcite tailing, in the development of cost effective and environmentally friendly bioremediation processes.     

Enhancement of Sulphide Production in Anaerobic Packed Bed Bench-scale Biofilm Reactors by Sulphate Reducing Bacteria

Two biofilm reactors, using pumice stone and Poraver as biofilm supports, were run, based on the optimization of sulphide production using a factorial design. The maximum H₂S concentrations reached were 10 and 15 mm, respectively, both being appropriate for metal precipitation in effluents. The set-up of the pumice stone biofilm reactor is suitable for application in the mining area in the Bolivian Andean region, where this material is widely available. The use of specific primers for sulphate-reducing bacteria groups permits the identification of the sulphide-producing bacteria present in biofilms.     

Bacterial bio-mediated calcite precipitation for monumental stones conservation: methods of evaluation.

The weathering of monumental stones is a complex process inserted in the more general 'matter transformation cycle' operated by physical, chemical and biological factors. The consequence of these combined actions is a loss of cohesion with dwindling and scaling of stone material and the induction of a progressive mineral matrix dissolution. In the case of calcareous stones, calcite leaching increases the material porosity and decreases its mechanical features with a general weakening of the superficial structural strength. Attempts to stop, or at least to slow down, deterioration of monumental stones has been made by conservative treatments with both inorganic or organic products. More recent studies show a new approach to hinder these phenomena by inducing a bio-mediated precipitation of calcite directly inside the stone porosity. This can be achieved either through the application of organic matrix macromolecules extracted from sea shells or of living bacteria. The effectiveness of the treatment using calcinogenic bacteria has been evaluated with laboratory tests specifically developed to evaluate the parameters such as : porosity, superficial strength and chromatic changes, influenced by the treatment itself. The results obtained seem to indicate that this type of treatment might not be suitable for monumental stone conservation.     

Utilization of the osmotolerance of sulphate-reducing bacteria in study of the genesis of subterranean waters

Cultures of sulphate-reducing bacteria from subterranean waters were divided into three groups, on the basis of their sensitivity to the sodium chloride concentration. The optimal sodium chloride concentration for group D1 cultures was 1% and under and the maximum tolerated concentration was 3.7%; in group D 4 cultures the optimal and maximum NaCl concentration were about 2% and 5.6% respectively and in group D 7 cultures about 3.5% and over 7% respectively. On using nutrient media containing 4% and 7% NaCl, these groups could be separated from a mixture and the bacterial count for each individual group could be determined. Study of the adaptation of these cultures to high sodium chloride concentrations showed that the group characteristics of the culture remained constant for at least ten passages. Comparative study of typical natural waters showed an incidence of D 1 bacteria in fresh water, but not in brackish water and sea water. The two latter types contained group D 4 and D 7 bacteria, the proportion of the latter group increasing with the degree of mineralization of the water. Study of the incidence of groups of sulphate-reducing bacteria was combined with other microbiological and hydrochemical indicators for resolving questions of the genesis of subterranean waters in Carpathian flysch. The results showed that the presence of variously mineralized hydrogen sulphide waters of different origin as regards their connection with the surface could be determined on the basis of the given criteria. The resultant picture corresponds to the recent state of the water and thus does not permit determination of the sedimentation system of the given water-bearing horizons.     

Bacterial colonization of pellet softening reactors used during drinking water treatment

Pellet softening reactors are used in centralized and decentralized drinking water treatment plants for the removal of calcium (hardness) through chemically induced precipitation of calcite. This is accomplished in fluidized pellet reactors, where a strong base is added to the influent to increase the pH and facilitate the process of precipitation on an added seeding material. Here we describe for the first time the opportunistic bacterial colonization of the calcite pellets in a full-scale pellet softening reactor and the functional contribution of these colonizing bacteria to the overall drinking water treatment process. ATP analysis, advanced microscopy, and community fingerprinting with denaturing gradient gel electrophoretic (DGGE) analysis were used to characterize the biomass on the pellets, while assimilable organic carbon (AOC), dissolved organic carbon, and flow cytometric analysis were used to characterize the impact of the biological processes on drinking water quality. The data revealed pellet colonization at concentrations in excess of 500 ng of ATP/g of pellet and reactor biomass concentrations as high as 220 mg of ATP/m(3) of reactor, comprising a wide variety of different microorganisms. These organisms removed as much as 60% of AOC from the water during treatment, thus contributing toward the biological stabilization of the drinking water. Notably, only a small fraction (about 60,000 cells/ml) of the bacteria in the reactors was released into the effluent under normal conditions, while the majority of the bacteria colonizing the pellets were captured in the calcite structures of the pellets and were removed as a reusable product.     

Distribution of sulphur-cycle bacteria in the Ems-Dollard estuary

Summary A quantitative study of the sulphur cycle in the tidal flat-sediments of the Eems-Dollard estuary was started by determining the distribution of two physiologically different groups of bacteria: sulphate-reducing and sulphide-oxidizing bacteria. Viable counts of these bacterial groups were determined by most probable number techniques.The highest numbers of aerobic sulphide-oxidizing bacteria were found in the upper 2 cm of the sediment. A rapid decrease was observed with increasing depth.The anaerobic sulphate-reducing bacteria showed different distribution-patterns with depth. Frequently high numbers of these bacteria were found above the redox-discontinuity-layer. This may be attributed to the presence of anaerobic micro-pockets in this largely aerobic top-layer of the sediment.The horizontal distribution of the sulphide-oxidizing bacteria appeared to be highly correlated with sediment parameters such as organic carbon and clay content of the sediment. The sulphate-reducing bacteria showed only a small linear correlation with these parameters.By means of polyfactor-analysis mathematical models were made with bacterial numbers as the dependent variables and with some environmental parameters as independent variables. The parameters used in this models could explain the variance of the viable counts for approximately 70%. The clay content of the sediment and the number of sulphate reducing bacteria appeared to determine to a large extent the variance in numbers of sulphide-oxidizing bacteria. There are indications that a great deal of the sulphide-oxidizing bacteria might be mixotrophic.For the explanation of the variance in numbers of sulphate-reducing bacteria the most important parameters were the clay content of the sediment, the number of aerobic heterotrophic bacteria and temperature (or season). Therefore the numbers of these organisms were varying throughout the year. It is assumed that the heterotrophic bacteria supply the sulphate-reducing bacteria with organic substrates.     

Isolation of new types of sulphate-reducing bacteria from estuarine and marine sediments using chemostat enrichments

Anaerobic chemostat enrichments have been successfully employed to isolate acetate-utilizing, sulphate-reducing bacteria from sediments in the Tay estuary. Several different morphologically and nutritionally versatile types of sulphate-reducing bacteria have been isolated by this means which has proved especially useful when they are present in low numbers. The principal advantage of this method is that strict anaerobes such as sulphate-reducing bacteria can be isolated in a controlled and reproducible enrichment system at low growth rates.     

Sulphur and sulphate reduction with acetate and propionate in an aerobic process for sulphide removal

Summary Sulphide production rates of sulphur-and sulphate-reducing bacteria up to 50 mg per biomass support particle per day were observed in an aerated sulphide-removal reactor with polyurethane (PUR) foam as carrier material. The optimal pH and temperature for the sulphide-producing bacteria were 8.0 and 30°C respectively. Raschig rings and four types of cube-shaped PUR particles were tested as carrier materials. When using PUR particles, the sulphide production rate was always between 3% and 4% of the sulphide removal rate, dependent on the dimensions and pore size of the polyurethane support particles. With the Raschig rings this ratio was only 2% and for reactors in which no carrier materials were present it was even lower (0.6%). Media containing different mixtures of acetate, propionate, sulphur and sulphate inoculated under anoxic conditions with sludge from the aerated reactor showed the presence of acetate-degrading sulphur-reducing, but not of acetate-degrading sulphate-reducing, bacteria. With propionate as sole electron donor no degradation occurred in the presence of sulphur within 2 weeks, whereas sulphate-dependent propionate oxidation started after 5–6 days incubation. Bacteria were isolated and resembled Desulfuromonas acetoxidans and Desulfobulbus propionicus morphologically and physiologically.     

Immunofluorescence of sulphate-reducing bacteria

An indirect fluorescent antibody technique was used as a method of rapidly assessing and identifying sulphate-reducing bacteria. Five specific antisera and one polyvalent serum were raised and tested against 44 strains of the genera Desulfovibrio and Desulfotomaculum along with 4 control organisms. Immunofluorescence was found to be mainly strain specific with the sulphate-reducing bacteria although weak fluorescence was seen both within and between recognised groups. A polyvalent antiserum was successfully used to detect sulphate-reducing bacteria. No interference from 4 control organisms was found.     

Selective inhibitors for continuous non-axenic hydrogen production by Rhodobacter capsulatus

To produce H₂ continuously by photosynthetically grown Rhodobacter capsulatus in non-axenic anaerobic reactors, the interaction between the phototroph and possible contaminants was studied and the ecological competitiveness of the Rhodobacter spp. in nitrogen-limited conditions was determined. Experimental test runs showed that blue-green and green algae, sulphate-reducing, acetogenic and methanogenic bacteria significantly interfere with the net amounts of H₂ produced by photobacteria. Therefore, inhibitors to control the growth of those contaminants selectively were screened. By applying a combination of chloroxuron (10mg/l) and cycloheximide (10mg/l) against algae, isohumulones (30 bitterunits/l) and molyb-date (0.5g/l) against sulphate-reducing bacteria and isohumulones and chloroform (10 mg/l) against acetogens and methanogens, photoreactors could be operated in a non-axenic way and continued to produce hydrogen gas at rates depending on the feed quality varying from 333 to 676 ml H₂l reactor/d, for a period of 116d without apparent interference from other microbial contaminants. These findings have a considerable potential for facilitating the isolation of organo-phototrophs and the production of H₂ by these bacteria.     

The bacteria of the sulphur cycle

This paper concentrates on the bacteria involved in the reductions and oxidations of inorganic sulphur compounds under anaerobic conditions. The genera of the dissimilatory sulphate-reducing bacteria known today are discussed with respect to their different capacities to decompose and oxidize various products of fermentative degradations of organic matter. The utilization of molecular hydrogen and formate by sulphate reducers shifts fermentations towards the energetically more favourable formation of acetate. Since acetate amounts to about two-thirds of the degradation products of organic matter, the complete anaerobic oxidation of acetate by several genera of the sulphate-reducing bacteria is an important function for terminal oxidation in sulphate-sufficient environments. The results of pure culture studies agree well with ecological investigations of several authors who showed the significance of sulphate reduction for the complete oxidation of organic matter in anaerobic marine habitats. In the dissimilatory sulphur-reducing bacteria of the genus Desulfuromonas the oxidation of acetate is linked to the reduction of elemental sulphur. Major characteristics of the anaerobic, sulphide-oxidizing phototrophic green and purple sulphur bacteria as well as of some facultative anoxygenic cyanobacteria, are given. By the formation of elemental sulphur and sulphate, these bacteria establish sulphur cycles with the sulphide-forming bacteria. In view of the morphological diversity of the sulphate-reducing bacteria and question of possible evolutionary relations to phototrophic sulphur bacteria is raised.     

Transfer of broad host-range plasmids to sulphate-reducing bacteria

Abstract The broad-host-range, IncQ, plasmid R300B (Sm, Su) has been stably transferred to two strains of sulphate-reducing bacteria ( Desulfovibrio sp. 8301 and Desulfovibrio desulfuricans 8312), using the IncP1 transfer system of the helper plasmid pRK2013 and cocultivation of sulphate-reducing bacteria with facultative anaerobes in media provided with sulphate and nitrate ions as electron acceptors. R300B was transferred at a frequency of 10⁻² to 1 per acceptor cell. The Sm^R marker was expressed in both sulphate-reducing bacteria strains while the Su^R was expressed only in strain 8301. R300B can also be transferred back to E. coli strains provided with IncP1 plasmids taking advantage of the retrotransfer ability of these plasmids. This occurs at a frequency up to 10⁻⁴ by recipient E. coli cell.     

THE ESTIMATION OF SULPHATE-REDUCING BACTERIA (D. DESULPHURICANS)

SUMMARY: Sodium sulphide or cysteine stimulated the growth of sulphate-reducing bacteria; small populations often did not grow without such supplements. Ascorbic acid, glutathione or thiolacetic acid had similar properties but thiolacetic acid was sometimes inhibitory, Dilution counts in liquid media or colony counts in agar media did not bear any regular relation to the total count unless one of these supplements was present. With suitable precautions colony counts reaching 50 to 60% of the total count were obtained in media incorporating cysteine and a ferrous salt (as an indicator of sulphide formation).
Samples of natural origin containing sulphate-reducing bacteria gave greater viable counts in cysteine-iron media than in unsupplemented media. Blackend culture tubes with natural populations were sometimes due to cysteine-decomposing organisms; further examination of positive tubes was therefore necessary.     

A convenient method for detecting sulphate-reducing bacteria

Sulphate-reducing bacterial cells, after addition of sodium hydroxide, showed a pink colour under a visible light microscope. This phenomenon is suggested as a test for sulphate-reducing bacteria.     

Biological sulphate reduction using gas-lift reactors fed with hydrogen and carbon dioxide as energy and carbon source

Feasibility and engineering aspects of biological sulphate reduction in gas-lift reactors were studied. Hydrogen and carbon dioxide were used as energy and carbon source. Attention was paid to biofilm formation, sulphide toxicity, sulphate conversion rate optimization, and gasliquid mass transfer limitations. Sulphate-reducing bacteria formed stable biofilms on pumice particles. Biofilm formation was not observed when basalt particles were used. However, use of basalt particles led to the formation of granules of sulphate-reducing biomass. The sulphate-reducing bacteria, grown on pumice, easily adapted to free H(2)S concentrations up to 450 mg/L. Biofilm growth rate then equilibrated biomass loss rate. These high free H(2)S concentrations caused reversible inhibition rather than acute toxicity. When free H(2)S concentrations were kept below 450 mg/L, a maximum sulphate conversion rate of 30 g SO(4) (2-)/L . d could be achieved after only 10 days of operation. Gas-to-liquid hydrogen mass transfer capacity of the reactor determined the maximum sulphate conversion rate. (c) 1994 John Wiley & Sons, Inc.     

The effect of pressure and temperature on sulphate-reducing bacteria and the action of biocides in oilfield water injection systems

The effects of elevated pressures and temperatures on the growth, morphology and metabolic activity of sulphate-reducing bacteria, isolated from the North Sea, are described. Pressure/temperature profiles, growth curves and sulphate reduction rates are presented for several isolates. The maximum pressure and temperature that supported growth were 65 000 KPa and 45°C respectively. The results are discussed in connection with water injection into oil-bearing reservoirs where there is a concern that generation of hydrogen sulphide by sulphate-reducing bacteria may lead to increased hydrogen sulphide levels (souring) in oil and gas, and to corrosion problems in production facilities. The bacteriostatic effects of a number of commercial biocides were enhanced at elevated hydrostatic pressures and temperatures.     

Calcium carbonate precipitation by heterotrophic bacteria isolated from biofilms formed on deteriorated ignimbrite stones: influence of calcium on EPS production and biofilm formation by these isolates

Heterotrophic CaCO₃-precipitating bacteria were isolated from biofilms on deteriorated ignimbrites, siliceous acidic rocks, from Morelia Cathedral (Mexico) and identified as Enterobacter cancerogenus (22e), Bacillus sp. (32a) and Bacillus subtilis (52g). In solid medium, 22e and 32a precipitated calcite and vaterite while 52g produced calcite. Urease activity was detected in these isolates and CaCO₃ precipitation increased in the presence of urea in the liquid medium. In the presence of calcium, EPS production decreased in 22e and 32a and increased in 52g. Under laboratory conditions, ignimbrite colonization by these isolates only occurred in the presence of calcium and no CaCO₃ was precipitated. Calcium may therefore be important for biofilm formation on stones. The importance of the type of stone, here a siliceous stone, on biological colonization is emphasized. This calcium effect has not been reported on calcareous materials. The importance of the effect of calcium on EPS production and biofilm formation is discussed in relation to other applications of CaCO₃ precipitation by bacteria.     

Microbial sulphate reduction at a low pH

It is now well established that microbial sulphate-reduction can proceed in environments with a pH<5. This review summarizes existing reports on sulphate reduction at low pH and discusses possible pH effects on sulphate-reducing bacteria. Microbial sulphate reduction has been observed in acidic lakes, wetlands, mesocosms, acidic sulphate soils and bioreactors. Possible inhibitory factors include the metabolites H(2)S and organic acids, which can be toxic depending on pH. Metal sulphide precipitation and competition with other bacteria, namely iron-reducing bacteria, can inhibit sulphate reduction. Theoretical considerations show that normal sulphate reduction rates are too low to maintain a neutral micro niche in an acidic environment. The first acidotolerant sulphate-reducing bacteria have been isolated recently.     

Characterization of sulphate-reducing bacterial populations within marine and estuarine sediments with different rates of sulphate reduction

Viable counts of sulphate-reducing bacteria, able to use a range of different growth substrates were determined in sediments from two Sea Lochs (Etive and Eil) and an estuarine site (Tay), in Scotland. The composition of the sulphate-reducing bacterial population, in terms of substrate utilization, broadly corresponded to the in situ substrates for sulphate reduction and concentration of substrates at each site. Addition of acetate, lactate, propionate, butyrate, hydrogen and glutamate/serine (20 mM) to replicate slurries from each site resulted in stimulation of the corresponding population of sulphate-reducing bacteria and the in situ rates of sulphate reduction. The metabolism of the added substrates and changes in bacterial phospholipid fatty acids (PLFA) were quantified. With the exception of acetate and hydrogen, added substrates were incompletely oxidised, producing a mixture of further substrates, which predominantly were sequentially oxidised, and resulted in the stimulation of a mixed population of sulphate-reducing bacteria. There were significant changes in the PLFA of slurries with added substrate compared to controls. Acetate was completely removed at all sites and the small increase in even chain PLFA together with the absence of stimulation of any other biomarker, indicated that acetate was oxidised by sulphate-reducing bacteria distinctly different from those using other substrates. A biomarker for Desulfobacter, 10 Methyl 16:0, was not stimulated in any of the acetate slurries or in slurries where acetate was produced. Biomarkers for the propionate utilizing Desulfobulbus sp (17:1w6, 15:1w6) were always stimulated in propionate slurries and also in lactate slurries, where partial lactate fermentation produced propionate and acetate. In lactate and glutamate / serine slurries from the Tay estuary and lactate and hydrogen slurries from Loch Etive the biomarker for Desulfovibrio sp (i17:1w7) as well as those for Desulfobulbus were stimulated. This provides direct evidence for the significance of Desulfovibrio sp. within sediment slurries and demonstrates the competitive interaction between members of this genus and Desulfobulbus sp. for lactate, hydrogen and amino acid metabolism. At the estuarine site, sulphate reduction was limited at higher sulphate concentrations (about 3.5 mM) than the Sea Loch sites (<2 mM) and this had a significant effect on propionate and butyrate metabolism, as well as on methane production. These results demonstrate that although the sulphate-reducing bacterial population at each site could metabolise identical substrates, the types of sulphate-reducing bacteria involved and their sulphate thresholds were characteristically different.