Evaluation of a microbial method to reduce hydrogen sulfide levels in a porous rock biofilm

Summary The efficacy of nitrate addition, with and without inoculation with a sulfide-resistant strain ofThiobacillus denitrificans (strain F), in reducing sulfide levels in an experimental system using cores and subsurface formation water from a gas storage facility was examined. The addition of nitrate (40 mM) alone to the formation water injected into core systems operated at hydraulic retention times of 3.2 and 16.7 h resulted in lower effluent sulfide concentrations, from an influent concentration of about 170–190 M to an effluent concentration of 110 and 3 M, respectively. A reduction in effluent nitrate concentrations in both core systems indicated the presence of indigenous nitrate-using populations. After strain F was inoculated into the core system operated at the shorter retention time, the effluent sulfide concentration decreased from 110 to 16–25 M. The effluent sulfate concentration increased, and the effluent nitrate concentration decreased concomitant with the presence of high concentrations of denitrifying thiobacilli in the inoculated core system. The denitrifying thiobacilli detected after inoculation were presumed to be strain F since these organisms were not detected in this core system before inoculation, or in any of the samples from the uninoculated core system. These data suggest that the efficacy of the nitrate treatment may depend on the residence times of the liquids in the core system, and that inoculation with strain F was required to reduce sulfide levels to <20 M in the core system operated at a short hydraulic retention time.     

Transformation of iron sulfide to greigite by nitrite produced by oil field bacteria

Nitrate, injected into oil fields, can oxidize sulfide formed by sulfate-reducing bacteria (SRB) through the action of nitrate-reducing sulfide-oxidizing bacteria (NR-SOB). When reservoir rock contains siderite (FeCO₃), the sulfide formed is immobilized as iron sulfide minerals, e.g. mackinawite (FeS). The aim of our study was to determine the extent to which oil field NR-SOB can oxidize or transform FeS. Because no NR-SOB capable of growth with FeS were isolated, the well-characterized oil field isolate Sulfurimonas sp. strain CVO was used. When strain CVO was presented with a mixture of chemically formed FeS and dissolved sulfide (HS⁻), it only oxidized the HS⁻. The FeS remained acid soluble and non-magnetic indicating that it was not transformed. In contrast, when the FeS was formed by adding FeCl₂ to a culture of SRB which gradually produced sulfide, precipitating FeS, and to which strain CVO and nitrate were subsequently added, transformation of the FeS to a magnetic, less acid-soluble form was observed. X-ray diffraction and energy-dispersive spectrometry indicated the transformed mineral to be greigite (Fe₃S₄). Addition of nitrite to cultures of SRB, containing microbially formed FeS, was similarly effective. Nitrite reacts chemically with HS⁻ to form polysulfide and sulfur (S⁰), which then transforms SRB-formed FeS to greigite, possibly via a sulfur addition pathway (3FeS + S⁰ → Fe₃S₄). Further chemical transformation to pyrite (FeS₂) is expected at higher temperatures (>60°C). Hence, nitrate injection into oil fields may lead to NR-SOB-mediated and chemical mineral transformations, increasing the sulfide-binding capacity of reservoir rock. Because of mineral volume decreases, these transformations may also increase reservoir injectivity. Electronic supplementary material  The online version of this article (doi:) contains supplementary material, which is available to authorized users.     

Effect of nitrate and nitrite on sulfide production by two thermophilic,sulfate-reducing enrichments from an oil field in the North Sea

Thermophilic sulfate-reducing bacteria (tSRB) can be major contributors to the production of H₂S (souring) in oil reservoirs. Two tSRB enrichments from a North Sea oil field, NS-tSRB1 and NS-tSRB2, were obtained at 58°C with acetate-propionate-butyrate and with lactate as the electron donor, respectively. Analysis by rDNA sequencing indicated the presence of Thermodesulforhabdus norvegicus in NS-tSRB1 and of Archaeoglobus fulgidus in NS-tSRB2. Nitrate (10 mM) had no effect on H₂S production by mid-log phase cultures of NS-tSRB1 and NS-tSRB2, whereas nitrite (0.25 mM or higher) inhibited sulfate reduction. NS-tSRB1 did not recover from inhibition, whereas sulfate reduction activity of NS-tSRB2 recovered after 500 h. Nitrite was also effective in souring inhibition and H₂S removal in upflow bioreactors, whereas nitrate was similarly ineffective. Hence, nitrite may be preferable for souring prevention in some high-temperature oil fields because it reacts directly with sulfide and provides long-lasting inhibition of sulfate reduction.     

Dynamics of corrosion rates associated with nitrite or nitrate mediated control of souring under biological conditions simulating an oil reservoir

Representative microbial cultures from an oil reservoir and electrochemical techniques including potentiodynamic scan and linear polarization were used to investigate the time dependent corrosion rate associated with control of biogenic sulphide production through addition of nitrite, nitrate and a combination of nitrate-reducing, sulphide-oxidizing bacteria (NR-SOB) and nitrate. The addition of nitrate alone did not prevent the biogenic production of sulphide but the produced sulphide was eventually oxidized and removed from the system. The addition of nitrate and NR-SOB had a similar effect on oxidation and removal of sulphide present in the system. However, as the addition of nitrate and NR-SOB was performed towards the end of sulphide production phase, the assessment of immediate impact was not possible. The addition of nitrite inhibited the biogenic production of sulphide immediately and led to removal of sulphide through nitrite mediated chemical oxidation of sulphide. The real time corrosion rate measurement revealed that in all three cases an acceleration in the corrosion rate occurred during the oxidation and removal of sulphide. Amendments of nitrate and NR-SOB or nitrate alone both gave rise to localized corrosion in the form of pits, with the maximum observed corrosion rates of 0.72 and 1.4 mm year⁻¹, respectively. The addition of nitrite also accelerated the corrosion rate but the maximum corrosion rate observed following nitrite addition was 0.3 mm year⁻¹. Furthermore, in the presence of nitrite the extent of pitting was not as high as those observed with other control methods.     

Biological souring of crude oil under anaerobic conditions

Seawater injection into oil reservoirs for purposes of secondary oil recovery is frequently accompanied by souring (increased sulfide concentrations). Production of hydrogen sulfide causes various problems, such as microbiologically influenced corrosion (MIC) and deterioration of crude oil. Sulfate-reducing bacteria (SRB) are considered to be major players in souring. Volatile fatty acids (VFAs) in oil-field water are believed to be produced by microbial degradation of crude oil. The objective of this research was to investigate mechanisms of souring, focusing specifically on VFA production via crude oil biodegradation. To this end, a microbial consortium collected from an oil–water separator was suspended in seawater; crude oil or liquid n-alkane mixture was added to the culture medium as the sole carbon source, and the culture was incubated under anaerobic conditions for 190 days. Physicochemical analysis showed that preferential toluene degradation and sulfate reduction occurred concomitantly in the culture containing crude oil. Sulfide concentrations were much lower in the alkane-supplemented culture than in the crude oil-supplemented culture. These observations suggest that SRB are related to the toluene activation and VFA consumption steps of crude oil degradation. Therefore, the electron donors for SRB are not only VFA, but many components of crude oil, especially toluene. Alkanes were also degraded by microorganisms, but did not contribute to reservoir souring.     

(Per)chlorate reduction at high temperature: Physiological study of Archaeoglobus fulgidus and potential implications for novel souring mitigation strategies

The recent finding that Archaeoglobus fulgidus is able to couple (per)chlorate reduction to growth expanded this trait to the hyperthermophilic range of life. This sulfate-reducing archaeon is considered to be one of the major contributors to souring in hot oil reservoirs. Therefore, it is important to study its physiology in depth, particularly in view of novel souring mitigation strategies. A. fulgidus does not possess the classical (per)chlorate reduction pathway, as it lacks the key enzyme chlorite dismutase. Rather, the microorganism seems to couple (per)chlorate reduction to sulfur metabolism. Growth experiments show the strict necessity of sulfur compounds to sustain perchlorate reduction. Furthermore, the chemical formation of elemental sulfur was observed during perchlorate reduction, a compound that is biologically reduced again. Additional experiments showed that tetrathionate, but not elemental sulfur and polysulfide, serves as an electron acceptor for growth by A. fulgidus. Taken together these results provide further evidence for the importance of chemical and biological redox reactions involving sulfur compounds during (per)chlorate reduction. In non-reduced media also, nitrate could be reduced by A. fulgidus, though not coupled to growth. This observation and the fact that A. fulgidus had prolonged adaptation phases on sulfate after long-lasting growth on perchlorate are of interest in the development of new souring mitigation strategies using nitrate and/or (per)chlorate.