Abstract
An electrobalance was used to study the reactive wetting of a series of Mn-containing steels ranging in composition from 0.14 wt.% to 5.1 wt.% Mn by a 0.20 wt.% dissolved Al continuous galvanizing bath as a function of immersion time, alloy Mn content and annealing atmosphere pO 2. It was found that the wetting force for the 1.4–5.1 wt.% Mn alloys was significantly less than that for the 0.14 wt.% Mn alloy due to the formation of a significant MnO layer on the higher Mn alloys. For all alloys and process atmospheres, reactive wetting and the formation of a well-developed interfacial Fe–Al intermetallic layer was achieved with the wetting force being directly related to the thickness of the external MnO layer. The wetting force was a strong function of the process atmosphere pO 2, which was in turn strongly related to the thickness of the external MnO layer. A reactive wetting model in which the motion of the triple line and the wetting force is limited by the oxide layer thickness is proposed.
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