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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 46 (2003), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The kinetics of sulfate reduction and cell densities of sulfate-reducing bacteria (SRB) were determined in activated sludge at Aalborg East wastewater treatment plant, a modern 100 000 person equivalent plant, where SRB are subjected to alternating cycles of oxic and anoxic conditions. The number of SRB was relatively constant over the year, ranging from 2.1×105 to 1.1×106 cells ml−1 as determined by 35S-radiotracer most probable number (MPN) in a growth medium prepared from anaerobic, sterilized sludge. Under anoxic conditions, the sulfide production in the activated sludge followed a biphasic pattern, being linear for approximately 5 h, followed by an exponential phase with doubling times of sulfide production of 4.2–12.6 h. Sulfate reduction started immediately after the onset of the anoxic cycle. Addition of antibiotics (chloramphenicol and streptomycin) to the activated sludge prevented the exponential phase of sulfate reduction for up to 100 h and this treatment was found to yield precise estimates of potential sulfate reduction rates. The addition of sulfate, sodium dithionite or single carbon compounds (lactate, acetate and glucose) did not decrease the length of the linear phase of sulfate reduction, nor did it affect the sulfate reduction rate. Our results indicate a tight and efficient metabolic coupling between populations of SRB and fermenting bacteria in activated sludge and a high capacity for sulfate reduction in sludge stored in settling tanks. Bacterial sulfate reduction may therefore be an important process in the destabilization of the floc structure when activated sludge is stored anaerobically for several days prior to dewatering.
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  • 2
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The presence of iron-solubilising bacteria in the weathered, naturally exposed part of a large sulfide ore deposit (gossan) in the High Arctic (eastern North Greenland, 83°N) was demonstrated. Microscopic examination of ore material and enrichment cultures in minimal medium containing FeS2 or Fe2+ as sole inorganic electron donors revealed the presence of rod-shaped Thiobacillus-like bacteria. When glucose was added as a supplementary energy source to the same enrichment medium, growth of spherical or filamentous acidophilic heterotrophs was observed. Growth kinetics and iron solubilisation activity of acidophilic autotrophs and heterotrophs, respectively, in samples of gossan material were investigated in the temperature range between 0 and 32.5°C. Assimilation of 14C-labelled bicarbonate and glucose occurred at low temperatures (down to 0°C) in both types of enrichments but was optimal around 21°C. It is noteworthy that the rate of dissolved iron (DI=Fe2++Fe3+) production from ore material at 0°C constituted as much as 30% of the maximal value at 21°C. The bacteria involved thus exhibited iron-dissolving activity at the lowest temperature ever reported. An activation energy for DI production of 56 kJ mol−1 K−1 was calculated in the temperature interval from 0 to 17°C. The corresponding H14CO−3 incorporation into biomass at 0°C only amounted to about 5% of the incorporation measured at 21°C. Rates of production were reduced by approximately 25% in incubations amended with glucose as compared to incubations solely containing inorganic compounds. These results indicate that autotrophic bacteria were involved in the solubilisation of iron from the gossan samples.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    FEMS microbiology ecology 53 (2005), S. 0 
    ISSN: 1574-6941
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology
    Notes: The present study addresses the effects of oxygen exposure on the aerobic and anaerobic respiratory activity of Desulfovibrio desulfuricans strain DvO1. This strain was isolated from the highest sulfate-reduction positive most-probable-number dilution (106) of an activated sludge sample, which had been subjected to 120 h of continuous aeration. Washed cell suspensions of strain DvO1 were aerated at 50% atmospheric oxygen saturation in sulfide-free media for a period of 33 h in the presence or absence of an external electron donor (10 mM lactate). During the aeration periods, samples were removed at intervals for determination of anaerobic INT (2-(p-iodophenyl)-3-(p-nitrophenyl)-5-phenyl tetrazolium chloride]-reducing activity, anaerobic sulfate-reducing activity, and oxygen-reducing activity. The cell suspension aerated in the absence of lactate showed negligible endogenous oxygen reduction rates and therefore did not consume oxygen during the aeration period. In contrast, the cell suspension aerated in the presence of lactate sustained significant rates of oxygen reduction during the entire 33 h aeration period. Despite this, no explicit differences in the potential INT-, oxygen-, or sulfate-reducing activities were evident between the two cell suspensions during the aeration periods. Strain DvO1 remained viable throughout the 33 h aeration periods irrespective of the presence or absence of lactate, however, the oxygen exposure resulted in a dose-dependent reversible metabolic inactivation. Notably, lactate-dependent anaerobic sulfate-reducing activity recovered quickly upon anaerobiosis, and was more oxygen tolerant than lactate-dependent oxygen-reducing activity.
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Archives of microbiology 139 (1984), S. 61-66 
    ISSN: 1432-072X
    Keywords: Desulfovibrio ; Freshwater and marine species ; Dissimilatory sulfate reduction ; Sulfate kinetics ; ApparentK m andV max for sulfate uptake
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology
    Notes: Abstract Apparent half-saturation constants (K m) and maximum uptake rates (V max) for sulfate were determined in four species ofDesulfovibrio of freshwater and marine origin using a35S-sulfate tracer technique. The lowerstK m (5 μM) was found in the freshwater speciesDesulfovibrio vulgaris (Marburg) and the highestK m (77 μM) in the marine speciesDesulfovibrio salexigens. Maximum specific rates of sulfate uptake (i.e.,V max) were proportional to the growth rates observed in batch cultures. The halophilicDesulfovibrio salexigens did not change itsK m andV max between 1 and 6,000 μM SO 4 2- , and apparently did not induce a low-affinity uptake system at high sulfate concentrations. The low half-saturation constants measured for sulfate uptake explain why high rates of bacterial sulfate reduction occur in surface sediments of freshwater lakes, and why sulfate reduction can be a quantitatively important process in anaerobic carbon mineralization in low-sulfate environments. The results shows that extremely low sulfate concentrations must occur before sulfate reduction is completely outcompeted by methanogenesis.
    Type of Medium: Electronic Resource
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