Effect of MgO and SiO2 Contents in Slag on the Control of Non-metallic Inclusions in Al-Killed Steel and the Erosion of MgO-Based Refractory
摘要
A series of laboratory-scale experiments were conducted to investigate the effects of MgO and SiO2 contents in slag on the control of inclusions in steel and the erosion of MgO-based refractory. The results demonstrated that both CaO–Al2O3 slag in Experiments A and CaO–Al2O3–MgO slag in Experiments B achieved high cleanliness of steel, with T[O] and [S] contents below 0.0007 and 0.0006 pct, respectively, after 60 min of refining. However, as SiO2 content in slag increased from 0 to 30 pct, the desulfurization rates of steel in Experiments A and B decreased from 95.71 and 96.43 pct to 34.29 and 29.29 pct, respectively. Moreover, when SiO2 exceeded 10 pct, the T[O] content began to increase. Regarding inclusions, when no SiO2 was added to slag, the inclusions in both Experiments A and B were mainly MgO-based, MgO–Al2O3, CaO–MgO–Al2O3, and a few Al2O3-based, with number density of 9.45/mm2 and 11.58 to 12.68/mm2, respectively. As SiO2 content increased, the proportion of MgO-based decreased in both experiments, while the proportion of MgO–Al2O3 first increased and then decreased. When SiO2 content reached 30 pct, the inclusions were primarily MgO–Al2O3 and MnO–SiO2–Al2O3. The number density reached its minimum at 15 pct SiO2 and then gradually increased, although the average size remained below 3 μm. Additionally, the refining slag eroded the MgO crucible, with penetration occurring along the gaps among MgO grains. The extent of erosion first increased linearly with rising SiO2 content in slag and then followed a parabolic trend. The addition of an appropriate amount of MgO effectively suppressed the erosion. Thermodynamic analysis revealed that although the initial slag compositions in both experiments did not meet the conditions for MgO–Al2O3 formation, the gradual addition of SiO2 coupled with MgO dissolution from the crucible led to the formation of MgO–Al2O3 in slag. This phase precipitated extensively during cooling, resulting in a significant increase in its size and number.