water-saturated rocks 饱和水岩石
fluid saturated rocks 饱和流体岩石
TIME-TEMPERATURE EQUIVALENCE OF SATURATED ROCKS 饱和岩石的时温等效关系
saturated soft rocks 饱水软岩
Amplitude has exponential decrease with increasing frequency in brine-saturated rocks.
在饱和盐水的岩石中，声波振幅随频率的增高而呈指数衰减。
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.
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。
Through constitution of PM space density function, the stress-strain state equation for saturated rocks has been defined and the hysteresis loops of axial stress-radial stress has been simulated.
通过构筑PM空间密度函数，求出饱和岩石的应力—应变状态方程，并模拟了其轴向应变—径向应变滞后回线。
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