Abstract
Calcareous deposits were formed on steel under cathodic protection conditions in artificial sea water at various potentials from −0·900 to −1·400 V(SCE). The deposition calcareous layers were characterised by electrochemical impedance spectroscopies, scanning electron microscopy observations and X-ray diffraction analyses. At 20°C, the deposits were composed of calcite CaCO3 when formed at various potentials in solution 1, of brucite Mg(OH)2 and aragonite CaCO3 when formed at potentials from −0·900 to −1·200 V(SCE) and only of brucite when formed at potentials E⩽−1·300 V(SCE) in solution 2. Magnesium seems to influence the corrosion behaviour of freely corroding steel by causing calcium carbonate to precipitate as aragonite. Aragonite is more effective in covering the surface than calcite and is therefore more functional in preventing oxygen from reaching the steel surface, thereby lowering the corrosion rate.
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