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Corrosion at the carbon steel-clay borehole water interface under anoxic alkaline and fluctuating temperature conditions
Corrosion Science ( IF 7.4 ) Pub Date : 2018-05-01 , DOI: 10.1016/j.corsci.2018.02.052
Michel L. Schlegel , Sophia Necib , Sylvie Daumas , Marc Labat , Cécile Blanc , Eddy Foy , Yannick Linard

Abstract Coupons of carbon steel were corroded in situ in anoxic clay porewater under slightly alkaline conditions. Sample damage was less than 1 μm for 9 months at 85 °C only, and corrosion interfaces were covered by a thin, protective layer of Fe-silicate. The damage was more significant for samples exposed to room temperature transients (up to 38 μm for two years), and the long-term surface differentiated in cathodic (Fe-silicate covered) areas and anodic crevices filled with siderite, chukanovite, β-Fe2(OH)3Cl, and covered by tubercles. Sulfide compounds were detected, and were related to the metabolism of sulfate-reducing prokaryotes detected by microbiological techniques.

中文翻译:

缺氧碱性和温度波动条件下碳钢-粘土钻孔水界面的腐蚀

摘要 在弱碱性条件下,在缺氧粘土孔隙水中对碳钢试样进行原位腐蚀。仅在 85 °C 下 9 个月,样品损伤小于 1 μm,腐蚀界面被一层薄薄的硅酸铁保护层覆盖。对于暴露于室温瞬变(两年高达 38 μm)的样品,损坏更为显着,并且长期表面在阴极(覆盖硅酸铁)区域和充满菱铁矿、chukanovite、β-Fe2 的阳极裂缝中分化(OH)3Cl,并被结节覆盖。检测到硫化物化合物,并与微生物技术检测到的硫酸盐还原原核生物的代谢有关。
更新日期:2018-05-01
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