previous up next print clean
Next: BOUNDARY BETWEEN POROUS ROCK Up: Blondel: Interpretation of the Previous: Blondel: Interpretation of the

INTRODUCTION

The insights of diffraction theory are useful in the interpretation of P-velocity measurements of suspensions. After introducing the notion of suspension, this paper compares some experimental P-velocity measurements presented by Marion 1990 with an acoustic modeling of the same experiment on a computer. Finally, a diffraction-oriented study shows that in comparison to Biot's theory, the P-velocity measured at a low frequency is slower than the high-frequency measurement. Moreover, the critical frequency between the high-frequency and low-frequency domains is directly related to the radius of the grains.


previous up next print clean
Next: BOUNDARY BETWEEN POROUS ROCK Up: Blondel: Interpretation of the Previous: Blondel: Interpretation of the
Stanford Exploration Project
11/17/1997