pore-fluid pressure 孔隙流体压力
Pore Fluid Distribution 孔隙流体分布
abnormal pore fluid pressure 异常孔隙流体压力
High Pore Fluid Pressure 高孔隙流体压力
Pore Fluid Volume Decrease 孔隙流体体积减小
express pore fluid stress 超孔隙水压力
pore-fluid 孔隙流体
This kind of soil is assumed as saturated porous media. Whereas, for soil whose saturation is less than 90%, there is no interaction between solid-skeleton and pore fluid.
当弹性波在土中传播时,对于饱和土和基本饱和土,孔隙水与土骨架之间存在动力相互作用,可用Biot动力学理论描述,将这类土假设为两相饱和多孔介质;但对于饱和度小于90%的土,孔隙水与土骨架之间的相互作用可以忽略,将这类土假设为单相固体介质,用弹性动力学理论描述。
参考来源 - 饱和两相与单相土互层场地中地铁车站地震反应分析·2,447,543篇论文数据，部分数据来源于NoteExpress
The influence of pore fluid on rock elastic properties at low saturation is analyzed.
分析了低饱和度时流体对岩石弹性性质的影响。
Fifth, the effects of pore fluid and its distribution on seismic properties were studied.
第五，讨论了孔隙流体及其分布对地震属性的影响。
An uncompacted belt can be described as an abnormal pore fluid pressure belt surrounded by "shell".
欠压实带可描述成被“壳”包围的一个异常孔隙流体压力带。
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