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Microbial community structures and in situ sulfate-reducing and sulfur-oxidizing activities in biofilms developed on mortar specimens in a corroded sewer system

机译:腐蚀的下水道系统中砂浆标本上形成的生物膜中的微生物群落结构和原位硫酸盐还原和硫氧化活性

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Microbially induced concrete corrosion (MICC) caused by sulfuric acid attack in sewer systems has been a serious problem for a long time. A better understanding of microbial community structures of sulfate-reducing bacteria (SRB) and sulfur-oxidizing bacteria (SOB) and their in situ activities is essential for the efficient control of MICC. In this study, the microbial community structures and the in situ hydrogen sulfide production and consumption rates within biofilms and corroded materials developed on mortar specimens placed in a corroded manhole was investigated by culture-independent 16S rRNA gene-based molecular techniques and microsensors for hydrogen sulfide, oxygen, pH and the oxidation-reduction potential. The dark-gray gel-like biofilm was developed in the bottom (from the bottom to 4 cm) and the middle (4-20 cm from the bottom of the manhole) parts of the mortar specimens. White filamentous biofilms covered the gel-like biofilm in the middle part. The mortar specimens placed in the upper part (30 cm above the bottom of the manhole) were corroded. The 16S rRNA gene-cloning analysis revealed that one clone retrieved from the bottom biofilm sample was related to an SRB, 12 clones and 6 clones retrieved from the middle biofilm and the corroded material samples, respectively, were related to SOB. In situ hybridization results showed that the SRB were detected throughout the bottom biofilm and filamentous SOB cells were mainly detected in the upper oxic layer of the middle biofilm. Microsensor measurements demonstrated that hydrogen sulfide was produced in and diffused out of the bottom biofilms. In contrast, in the middle biofilm the hydrogen sulfide produced in the deeper parts of the biofilm was oxidized in the upper filamentous biofilm. pH was around 3 in the corroded materials developed in the upper part of the mortar specimens. Therefore, it can be concluded that hydrogen sulfide provided from the bottom biofilms and the sludge settling tank was emitted to the sewer atmosphere, then oxidized to corrosive compounds in the upper and middle parts of the manhole, and only the upper part of the mortar specimens were corroded, because in the middle part of the manhole the generated corrosive compounds (e.g., sulfuric acid) was reduced in the deeper parts of the biofilm.
机译:长期以来,由硫酸侵蚀下水道系统引起的微生物引起的混凝土腐蚀(MICC)一直是一个严重的问题。更好地了解硫酸盐还原细菌(SRB)和硫氧化细菌(SOB)的微生物群落结构及其原位活性对于有效控制MICC是至关重要的。在这项研究中,通过与培养无关的基于16S rRNA基因的分子技术和硫化氢微传感器,研究了置于腐蚀的人孔的砂浆标本上形成的生物膜和腐蚀材料中的生物膜和腐蚀材料中的微生物群落结构以及原位硫化氢的产生和消耗速率。 ,氧气,pH和氧化还原电位。在灰浆样本的底部(从底部到4厘米)和中间(从人孔的底部到4-20厘米)部分形成了深灰色凝胶状生物膜。白色丝状生物膜覆盖了中间的凝胶状生物膜。放置在上部(沙井底部上方30 cm)的灰浆样本被腐蚀。 16S rRNA基因克隆分析表明,从底部生物膜样品中检索到的一个克隆与SRB相关,从中间生物膜样品和被腐蚀的材料样品中检索到的12个克隆和6个克隆分别与SOB相关。原位杂交结果表明,在整个底部生物膜中都检测到了SRB,主要在中间生物膜的上层有氧层中检测到丝状SOB细胞。微传感器测量表明,硫化氢在底部生物膜中产生并扩散出底部生物膜。相反,在中间生物膜中,在生物膜较深部分产生的硫化氢在上部丝状生物膜中被氧化。在砂浆样品上部形成的腐蚀材料中,pH值约为3。因此,可以得出结论,从底部生物膜和污泥沉淀池提供的硫化氢被排放到下水道大气中,然后在人孔的上部和中部被氧化成腐蚀性化合物,仅在砂浆标本的上部被氧化。之所以被腐蚀,是因为在人孔的中部,生物膜的较深部分减少了所产生的腐蚀性化合物(例如硫酸)。

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