From the experiments of low frequency sub resonance vibration for different fluid saturated rocks, the internalfrictionpeak was found to be a typical relaxation peak.
通过饱和多孔岩石的低频亚共振试验，得到了饱和多孔岩石的内耗峰是典型的弛豫峰的结论。
2
This internalfrictionpeak is suggested to be associated with the relaxation process of the unstable interface.
初步认为该内耗峰来源于非稳定界面的弛豫过程。
3
The results show that this internalfrictionpeak is originated from the relaxation process within the interfaces.