通常的内耗仪，应为低频力学弛豫谱仪。
The usual internal friction instrument is low-frequency mechanical relaxation instrument.
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。
From the experiments of low frequency sub resonance vibration for different fluid saturated rocks, the internal friction peak was found to be a typical relaxation peak.
初步认为该内耗峰来源于非稳定界面的弛豫过程。
This internal friction peak is suggested to be associated with the relaxation process of the unstable interface.
结果表明内耗峰来源于样品中界面的弛豫过程。
The results show that this internal friction peak is originated from the relaxation process within the interfaces.
结果表明内耗峰来源于样品中界面的弛豫过程。
The results show that this internal friction peak is originated from the relaxation process within the interfaces.
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