Next: Velocity vs. pore pressure
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The core samples were found to be very sensitive to pressure and
temperature conditions. Vp decreases of 10-15% were measured for
temperature increases from 75
F to 250
F at fixed overburden pressures
of 430-600 psia for samples in the upper and lower P formation,
and the K formation (Figure 11).
Above 250
F, the P-wave velocity decreases a further 25%
out to 350
F since the water component vaporizes to steam.
Next: Velocity vs. pore pressure
Up: ROCK PHYSICS
Previous: Core measurements
Stanford Exploration Project
11/12/1997