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Assessing Marine Microbial Induced Corrosion at Santa Catalina Island California

机译:在加利福尼亚州圣卡塔琳娜岛评估海洋微生物引起的腐蚀

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摘要

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.
机译:据报道,高铁和富营养条件是导致加速低水腐蚀的一种环境因素,低水腐蚀是近岸微生物诱发腐蚀的一种增强形式。为了探究这一假设,我们在来自美国加利福尼亚州圣卡塔琳娜岛的地表海水连续不断流动的情况下,在基于实验室的水族箱中部署了流通殖民化系统,持续了两个月和六个月。基材由低碳钢(海洋基础设施的主要组成部分)和天然存在的硫化铁矿物黄铁矿组成。测试了四个条件:自由排气的“高通量”条件; “停滞”状态; “主动”流通状态,海水缓慢泵送到基材上;在“浓缩”条件下,缓慢抽入海水补充营养丰富的培养基。对两个月高通量孵育的电子显微镜分析表明,基材上涂有“扭曲的茎”,类似于海洋嗜中性铁氧化细菌(FeOB)制成的羟基氧化铁生物沉淀物。相对于停滞条件,六个月的培养在活性水流和营养丰富的条件下表现出增加的生物膜和基质腐蚀。与高通量条件相比,在所有六个月的慢流量条件下均观察到扭曲的茎的稀缺性,这可能归因于慢通量条件下的氧浓度对于产生茎的细菌的持续生长而言是极低的。基于16S rRNA基因测序,所有底物均形成了反映原始海水输入的微生物群落。 Deltaproteobacteria序列在活动流量和营养富集条件下相对丰富,而在停滞条件下,gammaproteobacteria序列相对更丰富。这些结果表明(i)具有较高氧气利用率的高通量孵育有利于发展具有类似于海洋嗜中性FeOB的茎秆的生​​物膜,以及(ii)长期的营养刺激导致基质腐蚀和具有不同细菌群落组成的生物膜。相对于停滞和非营养性培养的结构。在附近的洛杉矶港可能发生类似的微生物演替情景,其中涉及营养投入的增加,导致厌氧铁和硫循环行会的扩散,并可能对海上港口基础设施造成破坏。

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