To illustrate the mechanism of the formation and evolution of inclusions in Si-deoxidized spring steel, pilot trials and systematic samplings were conducted, and detailed information about the inclusion density, morphology… Click to show full abstract
To illustrate the mechanism of the formation and evolution of inclusions in Si-deoxidized spring steel, pilot trials and systematic samplings were conducted, and detailed information about the inclusion density, morphology and composition was elucidated by electron probe X-ray microanalysis. The steel samples were collected from the vacuum degassing furnace, tundish furnace and spring rods after hot rolling. Based on the relationship between the mass ratio of $$ X_{{\left( {\text{CaO}} \right)}} /X_{{\left( {{\text{SiO}}_{ 2} } \right)}} $$XCaO/XSiO2 and diameters of inclusions, CaO-SiO2 inclusions were found to be formed by the coalescence between SiO2 and CaO-SiO2 inclusions. Most CaO-SiO2 inclusions > 10 μm were located in the melilite areas with liquidus temperatures < 1400 °C. The Al2O3-SiO2-CaO inclusions in the steel samples from the vacuum degassing and tundish furnaces were considered to be formed by reduction of CaO-SiO2 inclusions by Al dissolved in steel. The increased number density of Al2O3-SiO2-CaO inclusions in spring rods was primarily attributed to the entrapment of Na2O-contained mould flux particles and inclusions crushed after hot rolling. Many Al2O3-SiO2-MnO and SiO2-MnO inclusions were observed in tundish furnace samples, which originated from inherent reactions between [Al], [Si], [Mn] and [O] in the molten steel. The SiO2 precipitation of Al2O3-SiO2-MnO inclusions was attributed to the solubility decrease during the solidification process with temperature drop.
               
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