Corrosion rates of mild steel immersed in synthetic acid mine waters (pH 2.5) containing Fe3+ or Fe2+, Cu2+, Mg2+, Ca2+, K+, SO42–, Cl−, and SO32– ions in various combinations were measured by weight loss technique. The corrosion rates were significantly increased by Fe3+ and Cu2+ due to their reduction to Fe2+ and metallic Cu, respectively. An empirical relationship between ferric ion reduction rate and corrosion rate was established. Changes in corrosion potential with an increase in Fe3+ ion concentration gave a slope of 50 mV for dE/dlog [Fe3+]. A similar slope was observed in presence of Cu2+ ions. The cathodic Tafel slopes were in the range -112 to -133 mV/decade in accordance with the well known H2-evolution reaction mechanism of Bockris. The agreement between the observed and calculated limiting current densities confirms that the corrosion process is predominantly under diffusion-controlled cathodic processes. The corrosion rates calculated by the Tafel extrapolation method were 30% lower than those obtained from weight loss measurements. Attempted methods for control of mild steel corrosion by acid mine waters are discussed.
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Subrahmanyam et al. (1975) studied this question.
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