Xiao Haigang, Ye Wei, Song Xiaoping, Ma Yuantai, Li Ying
Laboratory for Corrosion and Protection, Institute of Metal Research, Chinese Academy of Sciences, Wencui Rd. 62, Shenyang 110016, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Materials (Basel). 2017 Nov 2;10(11):1262. doi: 10.3390/ma10111262.
The evolution of akaganeite in rust layers strongly impacts the atmospheric corrosion behavior of steel during long-term exposure; however, the factors affecting the evolution of akaganeite and its mechanism of formation are vague. In this work, wet-dry cyclic corrosion tests were conducted to simulate long-term exposure. Quantitative X-ray diffraction analysis was employed to analyze variations in the relative amounts of akaganeite; scanning electron microscopy and electron probe microanalysis were used to study the migration of relevant elements in the rust layer, which could help elucidate the mechanism of akaganeite evolution. The results indicate that the fraction of akaganeite tends to decrease as the corrosion process proceeded, which is a result of the decrease in the amount of soluble chloride available and the ability of the thick rust layer to block the migration of relevant ions. This work also explores the location of akaganeite formation within the rust layer.
锈层中赤铁矿的演变对长期暴露期间钢的大气腐蚀行为有强烈影响;然而,影响赤铁矿演变的因素及其形成机制尚不清楚。在这项工作中,进行了干湿循环腐蚀试验以模拟长期暴露。采用定量X射线衍射分析来分析赤铁矿相对含量的变化;使用扫描电子显微镜和电子探针微分析来研究锈层中相关元素的迁移,这有助于阐明赤铁矿演变的机制。结果表明,随着腐蚀过程的进行,赤铁矿的比例趋于降低,这是由于可用可溶性氯化物量的减少以及厚锈层阻碍相关离子迁移的能力所致。这项工作还探究了锈层中赤铁矿的形成位置。