John DeVilbiss
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View article: Compressional and shear wave velocities in water filled rocks during water-steam transition
Compressional and shear wave velocities in water filled rocks during water-steam transition Open
Both compressional and shear wave velocities were measured in water-filled Berea sandstone as a function of pore pressure under a constant confining pressure of 200 bar. At 145.5 C, compressional velocity increased from steam-saturated (lo…