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Formation mechanism of the outer layer of duplex scales on stainless steels in oxygenated supercritical water
Materials Letters ( IF 3 ) Pub Date : 2020-07-01 , DOI: 10.1016/j.matlet.2020.127731
Yanhui Li , Zhuohang Jiang , Shuzhong Wang , Jianqiao Yang , Yishu Zhang , Donghai Xu , Yang Guo

Abstract The dependence on water density of the formation and growth of the outer scale layer was revealed by using scanning electron microscopy (SEM), X-ray photoelectron spectroscopy (XPS) and X-ray diffraction (XRD) to analyze the effects of additive phosphates on morphology and composition of oxide scales formed on 316 stainless steel in supercritical water (SCW) with an initial dissolved oxygen of 100 mg·L−1 at 400 °C and 600 °C. In 400 °C SCW with a high density (exceeding 100 kg·m−3) the outer layer thickens via a precipitation process, hence the promotion of pre-existent phosphates in cationic precipitation results in the presence of smaller product particles and phosphorus on the scale surface. In 600 °C SCW with a low density, the formation of the outer scale layer follows a solid-state growth mechanism.

中文翻译:

含氧超临界水中不锈钢表面双相水垢外层的形成机理

摘要 通过使用扫描电子显微镜 (SEM)、X 射线光电子能谱 (XPS) 和 X 射线衍射 (XRD) 分析添加剂磷酸盐的影响,揭示了外垢层形成和生长对水密度的依赖性。 316 不锈钢在超临界水 (SCW) 中形成的氧化皮的形态和组成,在 400 °C 和 600 °C 下,初始溶解氧为 100 mg·L-1。在 400 °C 的高密度(超过 100 kg·m-3)SCW 中,外层通过沉淀过程变厚,因此在阳离子沉淀中促进预先存在的磷酸盐导致更小的产物颗粒和磷的存在刻度表面。在 600 °C 的低密度 SCW 中,外部氧化皮层的形成遵循固态生长机制。
更新日期:2020-07-01
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