NO3-/NO2-对渤海湾油藏中硫酸盐还原菌SO42-还原活性的抑制效应

长期注水开发促进了渤海湾海域油藏中硫酸盐还原菌(SRP)的生长繁殖,产生了大量H₂S,引起油藏酸化(souring)等问题. 本文首先以改进的API RP 38培养基富集了渤海湾海域某油藏采出井井口采出液中的SRP,再通过批次试验研究了不同浓度NO₃^-和NO₂^-对SRP富集培养物SO₄^2-还原活性的抑制效应. 结果表明： 渤海湾海域油藏中的SRP富集培养物SO₄^2-还原活性较强,SO₄^2-还原速率为10.4 mmol SO₄^2-·d^-1·g^-1 dry cell;加入浓度为0.4、0.8、1.8、4.2 mmol·L^-1NO₃^-时,SRP富集培养物的SO₄^2-还原活性均可被抑制,维持时间分别为5、9、20和大于35 d;加入浓度为0.6、0.9、1.4、2.6或4.6 mmol·L^-1的NO₂^-时,SO₄^2-还原活性也被抑制,维持时间分别为3、12、22和大于39 d. SRP富集培养物具有异化NO₃^-还原成NH₄⁺的代谢途径.当环境中同时存在SO₄^2-、NO₃^-、NO₂^-时,SRP富集培养物优先利用NO₃^-和NO₂^-. SRP富集培养物对电子受体的优先利用及NO₂^-的毒性效应是NO₃^-/NO₂^-抑制渤海湾海域油藏中SO₄^2-还原活性的主要原因.     

Microdistribution of sulfate-reducing bacteria in sediments of a hypertrophic lake and their response to the addition of organic matter

To clarify the ecological significance of the association of sulfate-reducing bacteria (SRB) with sediment particle size, SRB utilizing lactate (l-SRB), propionate (p-SRB) and acetate (a-SRB) were examined with different sizes of sediment particles in a hypertrophic freshwater lake using the anaerobic plate count method. The numbers ofl-SRB anda-SRB were 10⁴–10⁵ colony forming units (CFU) per ml in the 0–3 cm layer and 10²–10³ CFU ml⁻¹ in the 10–13 cm layer while the numbers ofp-SRB were one or two orders lower than those ofl-SRB anda-SRB. A sediment suspension was fractionated into four fractions (<1, 1–10, 10–94 and >94 μm). The highest proportions ofl-SRB anda-SRB were found in the 10–94 μm fraction: 66–97% forl-SRB and 53–98% fora-SRB. The highest proportion ofp-SRB was found in the >94 μm fraction (70–74%). These results indicate that most SRB were associated with sediment particles. One isolate from an acetate-utilizing enrichment culture was similar toDesulfotomaculum acetoxidans, a spore-forming sulfate-reducing bacterium. When lactate and sulfate were added to sediment samples,l-SRB anda-SRB in the <10 μm-fraction grew more rapidly than those in whole sediment for the first 2 days. This result suggests that nutrients uptake by free-living and small particle-associated (<10 μm) SRB is higher than that by SRB associated with larger particles.     

Indicators of Microbial Sulfate Reduction in Acidic Sulfide-Rich Mine Tailings

Sulfate-reducing bacteria (SRB) are thought to be actively involved in the cycling of sulfur in acidic mine tailings. However, most studies have used circumstantial evidence to assess microbial sulfate activity in such environments. In order to fully ascertain the role of sulfate-reducing bacteria (SRB) in sulfur cycling in acidic mine tailings, we measured sulfate reduction rates, sulfur isotopic composition of reduced sulfide fractions, porewaters and solid-phase geochemistry and SRB populations in four different Cu-Zn tailings located in Timmins, Ontario, Canada. The tailings were sampled in the summer and in the spring, shortly after snowmelt. The results first indicate that all four sites showed very high sulfate reduction rates in the summer (～100–1000 nmol cm^{? 3}d^?1), which corresponded to the presence of sulfide in the porewaters and to high SRB populations. In some of the sites, zones of microbial sulfate reduction also corresponded to a decline of organic carbon and to an apparent pyrite (with slightly negative δ³⁴S values) enrichment around the same depth. Microbial sulfate reduction was also important in permanently acidic (pH 2–3) mine tailings sites, suggesting that SRB can be active under very acidic conditions. Secondly, the results showed that microbial sulfate reduction was greatly reduced in the spring, suggesting that temperature might be a key factor in the activity of SRB. However, a closer look at the results indicated that temperature was not the sole factor and that acidic conditions and limited substrate availability in the spring appeared to be important as well in limiting microbial sulfate par reduction in sulfidic mine tailings. Finally, the results indicate that sulfur undergoes rapid cycling throughout the year and that microbial sulfate reduction and metal sulfide precipitation do not appear to be a permanent sink for metals.     

Ecology of some Species of Thiobacillus and Sulfate-reducing Bacteria in the Middle Course of the River Guadalquivir (Spain)

During 1985, a study was made of the physical, chemical and biological characteristics of the River Guadalquivir. At the same time, the density of certain microorganisms involved in the transformation of sulfur compounds in the water was studied. The results obtained give the following numerical order of density: T. thioparus >sulfate reducers > T. denitrificans > T. thiooxidans. Urban waste was found to increase density levels of these microorganisms. Their relationship with certain environmental parameters is discussed in this study. Regression equations have been obtained of bacteria numbers for three of the four groups studied, using water temperature and permanganate oxidability as dependent variables.     

Inhibiting sulfate-reducing bacteria in biofilms by expressing the antimicrobial peptides indolicidin and bactenecin

To identify novel, less-toxic compounds capable of inhibiting sulfate-reducing bacteria (SRB), Desulfovibrio vulgaris and Desulfovibrio gigas in suspension cultures were exposed to several antimicrobial peptides. The bacterial peptide antimicrobials gramicidin S, gramicidin D, and polymyxin B as well as the cationic peptides indolicidin and bactenecin from bovine neutrophils decreased the viability of both SRB by 90% after a 1-h exposure at concentrations of 25–100 μg ml⁻¹. To reduce corrosion by inhibiting SRB in biofilms, the genes for indolicidin and bactenecin were expressed in Bacillus subtilisBE1500 and B. subtilis WB600 under the control of the constitutive alkaline protease (apr) promoter, and the antimicrobials were secreted into the culture medium using the apr signal sequence. Bactenecin was also synthesized and expressed as a fusion to the pro-region of barnase from Bacillus amyloliquefaciens. Concentrated culture supernatants of B. subtilis BE1500 expressing bactenecin at 3 μg ml⁻¹ decreased the viability of Escherichia coli BK6 by 90% and the reference SRB D. vulgaris by 83% in suspension cultures. B. subtilis BE1500 and B. subtilis WB600 expressing bactenecin in biofilms also inhibited the SRB-induced corrosion of 304 stainless steel six to 12-fold in continuous reactors as evidenced by the lack of change in the impedance spectra (resistance polarization) upon addition of SRB and by the reduction in hydrogen sulfide and iron sulfide in batch fermentations with mild steel. A 36-fold decrease in the population of D. vulgaris in a B. subtilis BE1500 biofilm expressing bactenecin was also observed. This is the first report of an antimicrobial produced in a biofilm for in vivo applications and represents the first application of a beneficial, genetically-engineered biofilm for combating corrosion. Received 27 October 1998/ Accepted in revised form 21 February 1999     

Anaerobic oxidation of dimethylsulfide and methanethiol in mangrove sediments is dominated by sulfate-reducing bacteria

The oxidation of dimethylsulfide and methanethiol by sulfate-reducing bacteria (SRB) was investigated in Tanzanian mangrove sediments. The rate of dimethylsulfide and methanethiol accumulation in nonamended sediment slurry (control) incubations was very low while in the presence of the inhibitors tungstate and bromoethanesulfonic acid (BES), the accumulation rates ranged from 0.02–0.34 to 0.2–0.4 nmol g FW sediment⁻¹ h⁻¹, respectively. Degradation rates of methanethiol and dimethylsulfide added were 2–10-fold higher. These results point to a balance of production and degradation. Degradation was inhibited much stronger by tungstate than by BES, which implied that SRB were more important. In addition, a new species of SRB, designated strain SD1, was isolated. The isolate was a short rod able to utilize a narrow range of substrates including dimethylsulfide, methanethiol, pyruvate and butyrate. Strain SD1 oxidized dimethylsulfide and methanethiol to carbon dioxide and hydrogen sulfide with sulfate as the electron acceptor and exhibited a low specific growth rate of 0.010 ± 0.002 h⁻¹, but a high affinity for its substrates. The isolated microorganism could be placed in the genus Desulfosarcina (the most closely related cultured species was Desulfosarcina variabilis , 97% identity). Strain SD1 represents a member of the dimethylsulfide/methanethiol-consuming SRB population in mangrove sediments.     

Enrichment of anaerobic benzene-degrading microorganisms by in situ microcosms

Microcosms filled with different solids (sand, lava, Amberlite XAD-7) were exposed for 67 days in the sulfidic part of a groundwater monitoring well downstream of the source zone of a benzene-contaminated aquifer and subsequently incubated in the laboratory. Benzene was repeatedly degraded in several microcosms accompanied by production of sulfide, leading to stable benzene-degrading enrichment cultures. In control microcosms without filling material, benzene was initially degraded, but the benzene-degrading capacity could not be sustained. The results indicate that long-term physiologically active benzene-degrading microorganisms were attached to surfaces of the solids. The biodiversity and attachment behavior of microorganisms in the in situ microcosms was assessed by confocal laser scanning microscopy and single-strand conformation polymorphism (SSCP) analysis, followed by sequencing of dominant SSCP bands. The microbial community was composed of several different Bacteria, representing members of Clostridia, Bacteroidales, all subgroups of the Proteobacteria, Verrucomicrobia, Nitrospira, Chloroflexi and Chlorobi. Only a few archaeal sequences could be retrieved from the communities. The majority of phylotypes were affiliated to bacterial groups with a possible functional relationship to the bacterial sulfur cycle, thus indicating that the microbial community in the investigated aquifer zone depends mainly on inorganic sulfur compounds as electron donors or acceptors, a finding that corresponds to the geochemical data.     

Effects of legacy nuclear waste on the compositional diversity and distributions of sulfate-reducing bacteria in a terrestrial subsurface aquifer

The impact of legacy nuclear waste on the compositional diversity and distribution of sulfate-reducing bacteria in a heavily contaminated subsurface aquifer was examined. dsrAB clone libraries were constructed and restriction fragment length polymorphism (RFLP) analysis used to evaluate genetic variation between sampling wells. Principal component analysis identified nickel, nitrate, technetium, and organic carbon as the primary variables contributing to well-to-well geochemical variability, although comparative sequence analysis showed the sulfate-reducing bacteria community structure to be consistent throughout contaminated and uncontaminated regions of the aquifer. Only 3% of recovered dsrAB gene sequences showed apparent membership to the Deltaproteobacteria. The remainder of recovered sequences may represent novel, deep-branching lineages that, to our knowledge, do not presently contain any cultivated members; although corresponding phylotypes have recently been reported from several different marine ecosystems. These findings imply resiliency and adaptability of sulfate-reducing bacteria to extremes in environmental conditions, although the possibility for horizontal transfer of dsrAB is also discussed.     

Periplasmic superoxide dismutase from Desulfovibrio desulfuricans 1388 is an iron protein

It is shown that the genome of the sulfate-reducing bacterium Desulfovibrio desulfuricans 1388 contains a superoxide dismutase (SOD) gene (sod). The gene encodes an export signal peptide characteristic for periplasmic redox proteins. The amino acid sequence showed high homology with iron-containing SODs from other bacteria. Electrophoretically pure SOD was isolated from the periplasmic fraction of bacterial cells by FPLC chromatography. Like other Fe-SODs, D. desulfuricans 1388 superoxide dismutase is inhibited by H2O2 and azide, but not by cyanide.     

Phylogenetic Diversity and Distribution of Dissimilatory Sulfite Reductase Genes from Deep-Sea Sediment Cores

The diversity and distribution of sulfate-reducing prokaryotes (SRP) was investigated in the Nankai Trough sediments of off-central Japan by exploring the diversity of a functional gene, dissimilatory sulfite reductase (dsrAB). Bulk DNAs were extracted from five piston-cored samples (up to 4.5 m long) with 41 vertical sections, and full-length dsrABgene sequences (ca. 1.9 kb) were PCR amplified and cloned. A total of 382 dsrAB clones yielded eight phylogenetic groups with an indigenous group forming a unique dsrAB lineage. The deltaproteobacterial dsrAB genes were found in almost all sediment samples, especially in the surface layer. One unique dsrAB clone group was also widespread in the dsrAB profiles of the studied sediments, and the percentage of its clones was generally shown gradual increase with sediment depth.     

山西阳泉老窑水硫酸盐还原菌的分离鉴定及其还原功能驯化

【背景】含硫煤矿开采后,地表水/地下水回流至采空区形成酸性老窑水,含有高浓度重金属离子和硫酸盐,严重危害生态系统健康。利用微生物自身生长处理老窑水具有成本低、环境友好等特点,具有良好的应用前景。目前利用的硫酸盐还原菌大多只在适宜温度和中性pH条件下具有较高活性,在北方低温和酸性条件下难以发挥作用。【目的】本研究旨在从山西阳泉山底河流域的老窑水环境中分离硫酸盐还原菌,并调节温度和pH进行驯化,从而得到高效耐低温耐酸菌株,为北方老窑水微生物治理提供可用菌种资源。【方法】对山底河流域典型老窑水样品中的微生物进行富集培养,并筛选硫酸盐还原菌。通过革兰氏染色、扫描电镜对菌株形貌特性进行表征,利用16SrRNA基因序列比对进行菌种鉴定,探究其生长特性和硫酸盐还原性能。在此基础上降低温度和pH,对高效还原硫酸盐菌株进行驯化,探讨其在北方老窑水污染治理中的应用潜力。【结果】本研究筛选得到2株硫酸盐还原菌,命名为YQ-1和YQ-2,分别属于革兰氏阴性瘤胃解蛋白质菌属(Proteiniclasticum)和脱硫弧菌属(Desulfovibrio)。在30°C、pH 7.5条件下,YQ-1和YQ-2对1 1...     

Upgrading the efficiency of dissimilatory sulfate reduction by Desulfovibrio desulfuricans via adjustment of the COD/SO4 ratio

The potential for upgrading the microbiological reduction of sulfates and for decreasing the organic pollution levels in industrial waste-water by the adjustment of the COD/SO4 ratio was investigated. The experiments involved waste-water samples coming from industrial pig farming, baker's yeast production and organic dye manufacture. The results show that in the presence of Desulfovibrio desulfuricans both the objectives can be achieved by abating the disproportion between the content of sulfates and that of organic substances.     

The effects of in situ drying on sediment–phosphate interactions in sediments from an old wetland

We examined the effects of drying on sediment–P interactions for sediments from a shallow wetland ca. 6000 years old. Sediments from this wetland would have been subjected to numerous drying and wetting episodes during the life of the wetland. The factors affecting potential orthophosphate release were compared in surface sediments that had previously been desiccated for 3 months, surface sediments that had remained inundated and wet sediment 25–30 cm below the surface. All sediments released small amounts of orthophosphate once subjected to anaerobic conditions. Sulfate alone stimulated phosphate release from the surface sediment, irrespective of the previous hydrological status, whereas orthophosphate release from deep sediments was co-limited by carbon and sulfate. Decreases in soluble Fe (II) were measured concurrently with sulfate-stimulated P release, which is consistent with formation of iron sulfides. Similar numbers of culturable sulfate-reducing bacteria were obtained from the wet and dry sediments, their tolerance to desiccation explaining why release could occur after extensive drying of the sediment. Phosphate adsorption isotherms of the sediments showed that sediments from all sites had a relatively low affinity for ortho-phosphate. The adsorption data showed reasonable fit to the Freundlich adsorption isotherm. No difference in the maximum amount of ortho-phosphate uptake was observed if the sediment isotherm experiments were done under an inert atmosphere or, following exposure to air, suggesting that even anoxic sediments were not highly reduced. However, significant variations in the value of the Freundlich constants were observed. The results presented in this study are consistent with the hypothesis that repeated wetting/drying cycles select for bacteria that are tolerant to periods of desiccation and/or oxidation. Furthermore, repeated wetting and drying cycles may result in changes to sediment mineralogy.     

Role of Organic Carbon Sources and Sulfate in Controlling Net Methylmercury Production in Riverbank Sediments of the South River,VA (USA)

Mercury (Hg) transport and methylmercury (MeHg) production in riverbank sediments are complex processes influenced by site-specific physical and biogeochemical conditions. The South River watershed in VA, USA, contains elevated concentrations of Hg in riverbank and floodplain sediments, which has the potential to methylate. The role of specific organic carbon sources in promoting methylation reactions in natural sediments under dynamic flow conditions is not well understood. Four saturated column experiments were conducted, including a control column, which received South River water as an influent solution, and three columns that received South River water amended with: acetate (5.8 mM); lactate (5.7 mM); and lactate (5.7 mM) with SO₄^2? (10.1 mM). The amendments were selected to promote growth of different microorganisms to gain an understanding of the microbial processes, controlling rates of methylation. The column receiving lactate and SO₄^2? had the highest MeHg concentrations in the effluent and in the pore water near the effluent at 1.8 and 4.9 μg L^?1, respectively. At the cessation of the column experiments, the lactate–sulfate column sediments contained the highest populations of enumerable sulfur-reducing bacteria and the highest solid-phase MeHg at 530 ± 100 ng g^?1 dry wt. from the interval closest to the influent. The results suggest that the form and availability of electron donors and acceptors are primary factors controlling rates of methylation in the South River sediment.     

Diversity of Culturable Bacteria,from the Anaerobic Zone of the Meromictic Lake Pavin,Able to Perform Dissimilatory-Iron Reduction in Different in Vitro Conditions

A culture-dependent study was performed with the aim of assessing the carbon, electron and Fe(III) sources used for the dissimilatory Fe(III) reduction pathway and the diversity of culturable Fe(III)-reducers in the anoxic zone of the meromictic Lake Pavin. This metabolic pathway was investigated in enrichment cultures inoculated with water samples collected at 70 m depth in the anoxic zone of Lake Pavin. Combinations of different media, organic acids, and incubation gas phases were performed. The potential for Fe(III) reduction in the different growth conditions was assessed by measuring the accumulation of Fe(II) overtime. Bacterial community structure was determined in each growth conditions by Temporal Temperature gradient Gel Electrophoresis (TTGE) profiles of 16S rDNA genes and bands of interest in positive enrichments were sequenced. Comparisons of bacterial community structure between growth conditions revealed that the electron donor, the basal media as well as the Fe(III) source yielded to the selection of different bacterial populations, suggesting that Fe(III) reducers occupy different ecological niches in the anoxic zone of Lake Pavin. Facultative Fe(III) reducers, such as fermentative (e.g., Pseudomonas, Clostridium) and sulphate-reducing (e.g., Desulfovibrio sp.) bacteria, were retrieved in enrichments but well-known obligatory Fe(III) reducers (e.g., Geobacter) were not detected. A greater Fe(III) reduction was noted under H₂:CO₂ gas phase, suggesting that H₂ is used as an electron donor for Fe(III) reduction. Acetate was not used as a precursor for this terminal electron-accepting process, and a high Fe(III) reduction was observed with fumarate provided as the electron donor and carbon sources suggesting that this metabolite may be energetically more beneficial for Fe(III)-reducers.     

Organic Carbon Degradation in Anoxic Organic-Rich Shelf Sediments: Biogeochemical Rates and Microbial Abundance

Identifying and explaining bottlenecks in organic carbon mineralization and the persistence of organic matter in marine sediments remain challenging. This study aims to illuminate the process of carbon flow between microorganisms involved in the sedimentary microbial food chain in anoxic, organic-rich sediments of the central Namibian upwelling system, using biogeochemical rate measurements and abundances of Bacteroidetes, Gammaproteobacteria, and sulfate-reducing bacteria at two sampling stations. Sulfate reduction rates decreased by three orders of magnitude in the top 20 cm at one sampling station (280 nmol cm^?3 d^?1 – 0.1 nmol cm^?3 d^?1) and by a factor of 7 at the second station (65 nmol cm^?3 d^?1 – 9.6 nmol cm^?3 d^?1). However, rates of enzymatic hydrolysis decreased by less than a factor of three at both sampling stations for the polysaccharides laminarin (23 nmol cm^?3 d^?1– 8 nmol cm^?3 d^?1 and 22 nmol cm^?3 d^?1– 10 nmol cm^?3 d^?1) and pullulan (11 nmol cm^?3 d^?1– 4 nmol cm^?3 d^?1 and 8 nmol cm^?3 d^?1– 6 nmol cm^?3 d^?1). Increasing imbalance between carbon turnover by hydrolysis and terminal oxidation with depth, the steep decrease in cell specific activity of sulfate reducing bacteria with depth, low concentrations of volatile fatty acids (less than 15 μM), and persistence of dissolved organic carbon, suggest decreasing bioavailability and substrate limitation with depth.     

Abundance and diversity of mucosa-associated hydrogenotrophic microbes in the healthy human colon

Hydrogenotrophic microbiota have a significant impact on colonic health; however, little is known about their diversity and ecology in situ. Here, molecular-based methods and multivariate analyses were used to examine the abundance and diversity of mucosa-associated hydrogenotrophic microbes in 90 biopsies collected from right colon, left colon and rectum of 25 healthy subjects. Functional genes of all three hydrogenotrophic groups were detected in at least one colonic region of all subjects. Methanogenic archaea (MA) constituted approximately one half of the hydrogenotrophic microbiota in each colonic region. Sulfate-reducing bacteria (SRB) were more abundant than acetogens in right colon, while acetogens were more abundant than SRB in left colon and rectum. MA genotypes exhibited low diversity, whereas SRB genotypes were diverse and generally similar across the three regions within subject but significantly variable among subjects. Multivariate cluster analysis defined subject-specific patterns for the diversity of SRB genotypes; however, neither subject- nor region-specific clusters were observed for the abundance of hydrogenotrophic functional genes. Sequence analyses of functional gene clones revealed that mucosa-associated SRB were phylogenetically related to Desulfovibrio piger, Desulfovibrio desulfuricans and Bilophila wadsworthia; whereas MA were related to Methanobrevibacter spp., Mb. smithii and the order Methanomicrobiales. Together these data demonstrate for the first time that the human colonic mucosa is persistently colonized by all three groups of hydrogenotrophic microbes, which exhibit segmental and interindividual variation in abundance and diversity.     

海岸盐沼湿地土壤硫循环中的微生物及其作用

硫及硫化合物的动态循环是海岸盐沼湿地的重要组成部分,硫酸盐还原菌(SRB)和硫氧化菌(SOB)是推动硫循环的重要微生物。硫酸盐还原菌把硫酸盐还原为硫化物,同时消耗土壤中的有机物质;硫氧化菌把还原性硫化合物氧化为硫酸盐,缓解土壤中硫化物的积累,它们共同维持硫循环的动态平衡。本文综述了海岸盐沼湿地土壤中硫的存在形式、硫的地球化学循环以及在硫循环过程中扮演重要角色的硫酸盐还原菌和硫氧化菌的生物多样性、活性测定方法及其生态学意义等的最新研究进展,并提出了存在的问题及研究展望。     

油田硫酸盐还原菌酸化腐蚀机制及防治研究进展

硫酸盐还原菌(Sulfate reducing bacteria,SRB)是一些厌氧产硫化氢的细菌的统称,是以有机物为养料的厌氧菌。它们广泛分布于pH值6-9的土壤、海水、河水、淤泥、地下管道、油气井、港湾及锈层中,它们生存于好气性硫细菌产生的沉积物下,其最适宜的生长温度是20-30℃,可以在高达50-60℃的温度下生存,与腐蚀相关的最主要的是脱硫脱硫弧菌(Desulfovibrio desulfuricans)。 它们是许多腐蚀问题的主因,例如油田系统金属管路的腐蚀等。在海上油田生产中,海水常被注入油井用于进行2次采油。富含硫酸盐的海水能加速油藏中SRB的生长,随之H₂S大量产生,引起油田水的酸化,H₂S具有毒性和腐蚀性,增加石油和天然气中的硫含量,并可能引起油田堵塞。SRB引起的腐蚀问题是拭待解决的最主要问题。国内外治理该问题的途径主要有物理杀灭、添加化学杀菌剂等方法,但是这些方法成本高,持续效果不显著。近几年来国外学者开始重点关注利用生物竞争排斥技术(Bio-competitive inhibition technology,BCX)控制硫酸盐还原菌的生长代谢的方法,该方法的原理为通过加入特定的药剂,激活油藏中的本源微生物或加入外源微生物,使其与SRB竞争营养源或产生代谢物抑制SRB的生长代谢,进而抑制H₂S的产生。GMT-LATA的科学家对在厌氧油气储层和开采系统中硝酸盐还原菌的作用进行了最早的研究,认为该细菌可以抑制硫酸盐还原菌的代谢活动。随后BCX技术已经在国外部分油田得到了应用,国内还没有在海油生产中应用的报道,但是也有学者对该方法进行了研究。     

象山港海域硫酸盐还原菌的时空分布及其影响因素

分别于2007年7月(夏季)、11月(秋季)与2008年1月(冬季)、4月(春季),调查了象山港海域的水样(表层海水和上覆水)及沉积物中的硫酸盐还原菌丰度的时空分布特征及主要影响因素.结果表明,水样及沉积物中硫酸盐还原菌实测值的变化范围为30～2300 cells·ml-1,沉积物中的硫酸盐还原菌数量高于上覆水及表层海水;硫酸盐还原菌丰度的平面分布均呈现不均匀状态,人类开发活动较多的地区明显高于其他站点.根据硫酸盐还原菌数量,对底质进行腐蚀性评价结果表明,象山港大部分范围底质具有中等强度腐蚀性.有机质污染、水温、pH是表层海水中硫酸盐还原菌分布的重要影响因素(P＜0.01);上覆水中的硫酸盐还原菌含量与上覆水的营养盐(NO2--N、NH4+-N)呈显著正相关;沉积物中的硫酸盐还原菌含量与沉积物中的石油类呈显著正相关(P＜0.05).