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Mathematical modelling of the diffusion controlled phase in marine immersion corrosion of mild steel

机译:低碳钢海洋浸没腐蚀中扩散控制相的数学模型

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In the mathematical modelling of the 'general' corrosion of mild and low alloy steels and of some other metals oxygen diffusion through the corrosion products to the corroding surface controls the rate of corrosion at least during some period in the corrosion-time behaviour relationship. Under slightly different theoretical assumptions various early authors derived expressions for this phase. It was usually assumed the derived relationship applied from initial immersion. Only very limited laboratory support for the derived relationships exists. They have been applied to field data for atmospheric corrosion but with constants and exponents modified empirically. In the present paper the theory is reviewed and extended. It is argued that diffusion control cannot apply from first immersion and that this provides considerably greater freedom to mathematical modelling. Allowance is made for non-uniform corrosion product density and permeability and for loss of corrosion product. Recent detailed 'at-sea' experimental observations obtained on the Eastern Australian seaboard are applied to test the theory for mild steel. It is shown that the most likely competing mathematical relationships produce relatively similar results. The derived relationship is fitted to literature data to deduce its temperature dependence.
机译:在对低碳钢和低合金钢以及某些其他金属的“一般”腐蚀进行数学建模时,氧至少会在一定时期内在腐蚀时间行为关系中,通过腐蚀产物扩散到腐蚀表面,从而控制腐蚀速率。在稍有不同的理论假设下,各种早期作者得出了该阶段的表达式。通常假定派生关系是从最初的浸入中应用的。对于派生关系,只有非常有限的实验室支持。它们已应用于大气腐蚀的现场数据,但常数和指数根据经验进行了修改。本文对该理论进行了回顾和扩展。有人认为,扩散控制不能从最初的浸入中应用,这为数学建模提供了更大的自由度。允许不均匀的腐蚀产物密度和渗透率以及腐蚀产物的损失。最近在澳大利亚东部沿海获得的详细的“海上”实验观察结果被用于测试低碳钢的理论。结果表明,最可能的竞争数学关系产生了相对相似的结果。推导的关系适合于文献数据,以推断其温度依赖性。

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