材料科学
珠光体
连铸
铁氧体(磁铁)
降水
相(物质)
冶金
热力学
微观结构
复合材料
奥氏体
化学
物理
有机化学
气象学
作者
Yaqiang Li,Ziming Wang,Yingying Li,Baochen Han,Pengcheng Sheng,Yanting Liu
标识
DOI:10.1002/srin.202300172
摘要
The phase transformation of pearlite heat‐resistant steel during solidification is observed using high‐temperature confocal scanning laser microscopy. The precipitation of the δ‐ferrite (δ) phase proceeds in a cellular manner at cooling rates of 5 and 15 °C min −1 , whereas precipitation occurs in a dendritic manner at a cooling rate of 100 °C min −1 . Furthermore, a change in the solidification path is observed at high cooling rates. When the experimental steel is cooled at a low cooling rate of 5 °C min −1 , the sequence of continuous solidification is L → L + δ → L + δ + γ → δ + γ, which is consistent with that of equilibrium. However, when the cooling rate increases to 15 and 100 °C min −1 , the sequence of continuous solidification is L → L + δ → L + δ + γ → L + γ→γ. Furthermore, at various cooling rates, the interface of the peritectic transformation of δ → γ presents three different modes: planar and cellular modes controlled by solute diffusion and massive transformation controlled by the processes that occur at the transformation interfaces. The different δ → γ transformation modes and the associated different degrees of volume shrinkage are hypothesized to lead to uneven strand shell growth during continuous casting.
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