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在厌氧含水层注入水生物膜中模拟重度硝酸盐腐蚀:流动装置中的案例研究。

Modeling of heavy nitrate corrosion in anaerobe aquifer injection water biofilm: a case study in a flow rig.

机构信息

Uni Research CIPR , Allégaten 41, 5007 Bergen, Norway.

出版信息

Environ Sci Technol. 2014;48(15):8627-35. doi: 10.1021/es500839u. Epub 2014 Jul 14.

DOI:10.1021/es500839u
PMID:25020005
Abstract

Heavy carbon steel corrosion developed during nitrate mitigation of a flow rig connected to a water injection pipeline flowing anaerobe saline aquifer water. Genera-specific QPCR primers quantified 74% of the microbial biofilm community, and further 87% of the community of the nonamended parallel rig. The nonamended biofilm hosted 6.3 × 10(6) SRB cells/cm(2) and the S(35)-sulfate-reduction rate was 1.1 μmol SO4(2-)/cm(2)/day, being congruent with the estimated SRB biomass formation and the sulfate areal flux. Nitrate amendment caused an 18-fold smaller SRB population, but up to 44 times higher sulfate reduction rates. This H2S formation was insufficient to form the observed Fe3S4 layer. Additional H2S was provided by microbial disproportionation of sulfur, also explaining the increased accessibility of sulfate. The reduced nitrate specie nitrite inhibited the dominating H2-scavenging Desulfovibrio population, and sustained the formation of polysulfide and Fe3S4, herby also dissolved sulfur. This terminated the availability of acetate in the inner biofilm and caused cell starvation that initiated growth upon metallic electrons, probably by the sulfur-reducing Desulfuromonas population. On the basis of these observations we propose a model of heavy nitrate corrosion where three microbiological processes of nitrate reduction, disproportionation of sulfur, and metallic electron growth are nicely woven into each other.

摘要

在与注水井相连的流动装置中,为减轻硝酸盐的影响,发生了严重的碳钢腐蚀,该装置中的水为厌氧咸水含水层水。种特异性 QPCR 引物定量了 74%的微生物生物膜群落,进一步定量了未修正的平行装置中 87%的群落。未修正的生物膜中含有 6.3×10(6)个硫酸盐还原菌(SRB)细胞/cm(2),硫酸盐还原速率为 1.1 μmol SO4(2-)/cm(2)/天,与估计的硫酸盐还原菌生物量形成和硫酸盐面积通量一致。硝酸盐的添加导致 SRB 种群减少了 18 倍,但硫酸盐还原率高达 44 倍。这种 H2S 的形成不足以形成观察到的 Fe3S4 层。微生物硫的歧化作用提供了额外的 H2S,这也解释了硫酸盐的可及性增加。还原态的硝酸盐物种亚硝酸盐抑制了占主导地位的 H2 清除脱硫弧菌种群,并维持了多硫化物和 Fe3S4 的形成,从而溶解了硫。这终止了内层生物膜中乙酸盐的可用性,并导致细胞饥饿,从而引发了对金属电子的生长,可能是由硫还原脱硫单胞菌种群引起的。基于这些观察结果,我们提出了一个严重硝酸盐腐蚀的模型,其中硝酸盐还原、硫歧化和金属电子生长这三个微生物过程很好地交织在一起。

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