Murowchick, J.B., Oldroyd, A. and Rickard, D. ![]() ![]() |
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Official URL: http://dx.doi.org/10.1016/j.corsci.2024.111949
Abstract
The reaction between aqueous sulfide and α-iron at ambient temperatures produces a ferrous monosulfide with a tetragonal mackinawite structure, FeSm. The reaction is epitactic with the Fe structure in FeSm being similar, but not identical, to the Fe structure in α-iron. The strain induced by these small structural differences results in spallation of the FeSm product. This causes the exposure of new α-iron sites and determines the rate of sulfide corrosion of α-iron. The results provide a fundamental explanation for the real-world observation that pitting of steel pipes in sulfide environments is a major source of corrosion and pipe failure.
Item Type: | Article |
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Date Type: | Publication |
Status: | Published |
Schools: | Schools > Earth and Environmental Sciences |
Publisher: | Elsevier |
ISSN: | 0010-938X |
Date of First Compliant Deposit: | 3 April 2024 |
Date of Acceptance: | 23 February 2024 |
Last Modified: | 05 Mar 2025 02:45 |
URI: | https://orca.cardiff.ac.uk/id/eprint/167671 |
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