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Radial Waves In A Borehole And Stoneley Waves For Measuring Formation Permeability And Electroacoustic Constant

机译:钻孔中的径向波和斯通利波用于测量地层渗透率和电声常数

摘要

A Stoneley wave is generated in a borehole in a saturated porous earth formation. Measurements are made of the velocity of motion of the formation and the fluid in the formation. The difference in the velocities is indicative of formation permeability. An additional measurement of the electric field at the borehole wall enables determination of the electroacoustic constant.
机译:斯通利波在饱和多孔土层中的钻孔中产生。对岩层和岩层中流体的运动速度进行测量。速度的差异表示地层渗透率。在井眼壁处的电场的附加测量能够确定电声常数。

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