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
pore-fluid 孔隙流体
pore fluid flow 孔隙流体流动
pore-fluid anomaly 裂隙流体异常
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
Therefore, resistivity logs have long been used by reservoir geologists and engineers to identify rock types, describe the variations of pore fluid and determine well completion characteristics.
因此，长期以来油藏地质学家和工程师一直把电阻率测井用于识别岩石类型，描绘孔隙流体变化和确定完井特征。
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。
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