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Modeling of the Iron Anodic Dissolution

机译:铁阳极溶出度的建模

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Patterns of anodic dissolution of iron are interpreted in the light of notion of the cooperative nature of the electronic subsystem of metal and the proton subsystem acidic electrolyte. Admitted, that speed limiting process of anodic ionization of the metal in the low-voltage surge is a doubly charged ion desorption from the surface, requiring "embedding" it in the near-electrode layer of electrolyte. The article presents a mathematical model of the anodic dissolution of iron in acidic media, based on the phenomenological picture of the processes occurring on the surface of the metal. The model allows for the possibility of dissolution as a set of consecutive outputs of the iron atoms from the kink at low voltage and cooperative processes at high anodic overpotentials, such as solitons of dissolution. Comparison of calculated and experimental data shows that the model largely agrees with the experiment. Obviously, that needs clarification of the soliton model for a more complete description of all available sets of experimental data on anodic dissolution of iron.
机译:根据金属电子子系统与质子子系统酸性电解质的协同性质的概念来解释铁的阳极溶解方式。公认的是,低压电涌中金属的阳极电离的速度限制过程是从表面解吸的双电荷离子,需要“嵌入”在电解质的近电极层中。本文基于在金属表面上发生的过程的现象学现象,提供了铁在酸性介质中阳极溶解的数学模型。该模型允许以低电压从扭折中连续输出铁原子,以及在高阳极超电势(例如溶解孤子)下的协同过程,产生一组连续的铁原子输出。计算和实验数据的比较表明,该模型与实验基本吻合。显然,这需要对孤子模型进行澄清,以便对铁的阳极溶解的所有可用实验数据集进行更完整的描述。

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