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评估加利福尼亚州圣卡塔利娜岛的海洋微生物诱导腐蚀。

Assessing Marine Microbial Induced Corrosion at Santa Catalina Island, California.

作者信息

Ramírez Gustavo A, Hoffman Colleen L, Lee Michael D, Lesniewski Ryan A, Barco Roman A, Garber Arkadiy, Toner Brandy M, Wheat Charles G, Edwards Katrina J, Orcutt Beth N

机构信息

Department of Biological Sciences, University of Southern California, Los Angeles CA, USA.

Department of Earth Science, University of Minnesota-Twin Cities, Minneapolis MN, USA.

出版信息

Front Microbiol. 2016 Oct 25;7:1679. doi: 10.3389/fmicb.2016.01679. eCollection 2016.

DOI:10.3389/fmicb.2016.01679
PMID:27826293
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC5078718/
Abstract

High iron and eutrophic conditions are reported as environmental factors leading to accelerated low-water corrosion, an enhanced form of near-shore microbial induced corrosion. To explore this hypothesis, we deployed flow-through colonization systems in laboratory-based aquarium tanks under a continuous flow of surface seawater from Santa Catalina Island, CA, USA, for periods of 2 and 6 months. Substrates consisted of mild steel - a major constituent of maritime infrastructure - and the naturally occurring iron sulfide mineral pyrite. Four conditions were tested: free-venting "high-flux" conditions; a "stagnant" condition; an "active" flow-through condition with seawater slowly pumped over the substrates; and an "enrichment" condition where the slow pumping of seawater was supplemented with nutrient rich medium. Electron microscopy analyses of the 2-month high flux incubations document coating of substrates with "twisted stalks," resembling iron oxyhydroxide bioprecipitates made by marine neutrophilic Fe-oxidizing bacteria (FeOB). Six-month incubations exhibit increased biofilm and substrate corrosion in the active flow and nutrient enriched conditions relative to the stagnant condition. A scarcity of twisted stalks was observed for all 6 month slow-flow conditions compared to the high-flux condition, which may be attributable to oxygen concentrations in the slow-flux conditions being prohibitively low for sustained growth of stalk-producing bacteria. All substrates developed microbial communities reflective of the original seawater input, as based on 16S rRNA gene sequencing. Deltaproteobacteria sequences increased in relative abundance in the active flow and nutrient enrichment conditions, whereas Gammaproteobacteria sequences were relatively more abundant in the stagnant condition. These results indicate that (i) high-flux incubations with higher oxygen availability favor the development of biofilms with twisted stalks resembling those of marine neutrophilic FeOB and (ii) long-term nutrient stimulation results in substrate corrosion and biofilms with different bacterial community composition and structure relative to stagnant and non-nutritionally enhanced incubations. Similar microbial succession scenarios, involving increases in nutritional input leading to the proliferation of anaerobic iron and sulfur-cycling guilds, may occur at the nearby Port of Los Angeles and cause potential damage to maritime port infrastructure.

摘要

高铁和富营养化条件被报道为导致加速低水腐蚀的环境因素,这是近岸微生物诱导腐蚀的一种增强形式。为了探究这一假设,我们在美国加利福尼亚州圣卡塔利娜岛的表层海水连续流动的情况下,在实验室水族箱中部署了流通式定殖系统,为期2个月和6个月。底物由低碳钢(海洋基础设施的主要成分)和天然存在的硫化铁矿物黄铁矿组成。测试了四种条件:自由通风的“高通量”条件;“停滞”条件;海水缓慢泵过底物的“活跃”流通条件;以及通过富含营养的培养基补充海水缓慢泵送的“富集”条件。对2个月高通量培养物的电子显微镜分析记录了底物被“扭曲茎”覆盖,类似于海洋嗜中性铁氧化细菌(FeOB)产生的氢氧化铁生物沉淀。与停滞条件相比,6个月的培养显示在活跃流动和营养富集条件下生物膜和底物腐蚀增加。与高通量条件相比,在所有6个月的慢流条件下观察到扭曲茎较少,这可能是由于慢流条件下的氧气浓度对于产生茎的细菌的持续生长过低。基于16S rRNA基因测序,所有底物都形成了反映原始海水输入的微生物群落。在活跃流动和营养富集条件下,δ-变形菌序列的相对丰度增加,而在停滞条件下γ-变形菌序列相对更丰富。这些结果表明:(i)具有较高氧气可用性的高通量培养有利于形成具有类似于海洋嗜中性FeOB的扭曲茎的生物膜;(ii)长期营养刺激导致底物腐蚀以及相对于停滞和非营养增强培养具有不同细菌群落组成和结构的生物膜。类似的微生物演替情况,包括营养输入增加导致厌氧铁和硫循环群落的增殖,可能发生在附近的洛杉矶港,并对海港基础设施造成潜在损害。

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