Mechanisms of Microstructure Evolution during Deformation of Undercooled Austenite in a Low Carbon Steel
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摘要: 低碳鋼過冷奧氏體形變過程將發生形變強化相變及鐵素體的動態再結晶,導致晶粒超細化.與未形變的過冷奧氏體等溫轉變相比,形變極大地促進了奧氏體向鐵素體的轉變,使鐵素體形核率急劇升高,鐵素體晶粒尺寸顯著降低.形變強化相變是一以形核為主的過程.在形變后期,當形變強化相變鐵素體轉變基本完成后,將發生鐵素體的動態回復和動態再結晶.比較不同應變速率對組織演變影響的結果表明,應變速率較低條件下,易形成鐵素體與第2組織層狀分布的條帶特征;應變速率較高時,組織的條帶特征不顯著.Abstract: Two mechanisms-deformation enhanced transformation and dynamic recrystallization of ferrite are involved during deformation of undercooled austenite in a low carbon steel, leading to effective ferrite grain refinement. In comparison with isothermal transformation, deformation significantly accelerates austenite to ferrite transformation, leading to a very high nucleation rate. Deformation enhanced transformation is a nucleation dominant process. The results of EBSD and TEM indicate that ferrite dynamic recrystallization also plays an important role on grain refinement as well as deformation enhanced transformation. The misorientation of sub-grain boundaries is assumed to increase by further straining, accompanied by grain rotation, finally leading to the recrystallized small ferrite grains. Study on the effect of strain rate on microstructure homogeneity indicates that microstructure tends to be distributed in a laminar manner at lower strain rate.
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