The overheating characteristics of several commercial and experimental low-alloy steels have been investigated. Overheating is characterized by the appearance of ductile intergranularfacets onfracture surfaces caused by the precipitation of a-MnS particles at prior austenite grain boundaries. The cooling rate through the overheating rangeproduced a marked variation in the size and dispersion of intergranular a-MnS particles. Cooling rates in the range 10°-400°C/min produced the most severe grain-boundary embrittlement and were consistent with an MnS particle size of 1–2 μm for a commercial En39B steel. A marked refinement in the size distribution of inclusions was apparent following overheating treatments on all steels and was due to the solution and reprecipitation of the sulphide inclusions. Rare-earth-treated En39B steels, when subjected to high-temperature ‘overheating’ treatments, contained no areas of intergranular failure on impact fracture surfaces and no marked deterioration in mechanical properties was observed following such treatments. A critical Ce/S ratio of ∼2:1 resulted in the complete modification of MnS inclusions to rare-earth sulphides and oxysulphides. Values below this critical level resulted in the presence of ‘free MnS’ which dissolved and reprecipitated at prior austenite grain boundaries following overheating treatments.
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