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- W2008264302 startingPage "3731" @default.
- W2008264302 abstract "The velocity V sub p of compressional waves has been measured in rock samples of low porosity to confining pressures P sub c of 2 kb for a number of different constant pore pressures P sub p. An effective pressure defined by P sub e = P sub c-nP sub p, n less than or equal to 1, is found to be the determining factor in the behavior of V sub p rather than an effective pressure defined simply by the differential pressure Delta P = P sub c-P sub p. As pore pressure increases at constant effective pressure, the value of n increases and approaches 1, but as effective pressure increases at constant pore pressure, the value of n decreases. These observations are consistent with Biot's theory of the propagation of elastic waves in a fluid-saturated porous solid." @default.
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- W2008264302 date "1972-07-10" @default.
- W2008264302 modified "2023-09-26" @default.
- W2008264302 title "Effect of pore pressure on the velocity of compressional waves in low-porosity rocks" @default.
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- W2008264302 doi "https://doi.org/10.1029/jb077i020p03731" @default.
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