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Iron-Corroding Methanogen Isolated from a Crude-Oil Storage Tank

机译:从原油储罐中分离出的铁腐蚀产甲烷菌

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摘要

Microbiologically influenced corrosion of steel in anaerobic environments has been attributed to hydrogenotrophic microorganisms. A sludge sample collected from the bottom plate of a crude-oil storage tank was used to inoculate a medium containing iron (Fe-0) granules, which was then incubated anaerobically at 37 degrees C under an N-2-CO2 atmosphere to enrich for microorganisms capable of using iron as the sole source of electrons. A methanogen, designated strain KA1, was isolated from the enrichment culture. An analysis of its 16S rRNA gene sequence revealed that strain KA1 is a Methanococcus maripaludis strain. Strain KA1 produced methane and oxidized iron much faster than did the type strain of M. maripaludis, strain JJ(T), which produced methane at a rate expected from the abiotic H-2 production rate from iron. Scanning electron micrographs of iron coupons that had been immersed in either a KA1 culture, a JJ(T) culture, or an aseptic medium showed that only coupons from the KA1 culture had corroded substantially, and these were covered with crystalline deposits that consisted mainly of FeCO3.
机译:在厌氧环境中,受微生物影响的钢腐蚀归因于氢营养微生物。从原油储罐底板收集的污泥样品用于接种含有铁(Fe-0)颗粒的培养基,然后在N-2-CO2气氛下在37°C下厌氧孵育,以富集能够使用铁作为唯一电子来源的微生物。从富集培养物中分离出一种产甲烷菌株 KA1。对其 16S rRNA 基因序列的分析显示,菌株 KA1 是一种 Methanococcus maripaludis 菌株。菌株 KA1 产生甲烷和氧化铁的速度比 M. maripaludis 菌株 JJ(T) 的产生速度快得多,后者以铁的非生物 H-2 产生速率的预期速率产生甲烷。浸入 KA1 培养物、JJ(T) 培养物或无菌培养基中的铁试样的扫描电子显微照片显示,只有来自 KA1 培养物的试样被严重腐蚀,并且这些试样被主要由 FeCO3 组成的结晶沉积物覆盖。

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