Wave Propagation In A Fluid-Filled Fracture-An Experimental Study
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1989.4 Tang_Cheng.pdf
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Author(s)
Tang, X. M.
Cheng, C. H.
Date Issued
1989
Publisher
Massachusetts Institute of Technology. Earth Resources Laboratory
Series/Report no.
Earth Resources Laboratory Industry Consortia Annual Report;1989-04
Abstract
A laboratory experimental study has been carried out to investigate the mode trapping
characteristics of a fluid-filled fracture between two elastic solids. Using a small circular cylindrical receiver of 2.7 mm diameter, we were able to measure the wave motion
directly inside a 2.8 mm thick fracture and to obtain array data for the propagating
waves. The data was processed using Prony's method to give velocity of the wave
modes as a function of frequency. The experimental results agree with the theoretical
predictions quite well. Specifically, in a "hard" (aluminum) fracture where the shear
velocity of the solid is greater than the fluid velocity, four normal modes were detected
in the frequency range up to 2.4 MHz. Whereas in a "soft" (lucite) fracture where the
shear velocity is smaller than the fluid velocity, four leaky-P modes were detected in the same frequency range. In both cases, a fundamental mode analogous to Stoneley waves
in a borehole was detected. In particular, the velocity of this mode approaches zero in
the low frequency limit, as indicated by the theory and confirmed by the experiment
in a low frequency range down to 25 kHz.
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