通过3组实验证实了下贝氏体碳化物是在α/γ界面的奥氏体一侧析出,并向奥氏体中生长,同时也在贝氏体亚单元之间析出.在形态上,碳化物存在于铁素体内,也可跨越α/γ或α/α界面;在整个相变过程中,铁素体与碳化物的长大呈相互竞争机制,碳化物从α/γ界面的γ一侧析出,但铁素体的长大速度远高于碳化物,二者长大的结果是铁素体将碳化物包围,导致碳化物似乎是由铁素体中析出的假象;用热力学及台阶理论对实验结果做了分析,在实验证据及理论分析的基础上,提出了下贝氏体碳化物的析出及长大模型;下贝氏体碳化物是由富碳残余奥氏体中析出而不是由碳过饱和的铁素体中析出,其实质是确定新形成的贝氏体铁素体中是否含有过饱和碳,这直接涉及贝氏体相变机制的类型.
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