The lower interphase energy in the martensitic transformation results in a lower value of internal friction peak as compared with that in diffusional transformation.
马氏体相变中相界面能量较低，导致其内耗峰值低于扩散型相变的峰值。
The research results provide the reference value for the choice of the cohesion and internal friction Angle of rock samples in the process of geo-engineering design and numerical simulation.
研究结果对于岩土工程设计和数值计算时岩样黏聚力和内摩擦角的选取具有参考价值。
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