奥氏体一贝氏体组织 austenite-bainite structure
奥氏体-贝氏体组织 Bainite-Austenite microstructure
下贝氏体-马氏体组织 lower bainite-martensite structure
在低碳范围几乎得到全部贝氏体组织。
Within the low carbon range the whole bainitic microstructure is available.
提出了划分低碳贝氏体与高碳贝氏体组织的建议。
And a new way is suggested to classify the bainite structures morphologically. into "low carbon bainite"...
论证了所谓粒状贝氏体组织实际上是这种演化过程的阶段性组织特征。
It is proved that the so-called granular bainite microstructure is nothing else but the structural characteristic at a certain stage of this evolution.
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