J. Groenenboom et al., Time-lapse ultrasonic measurements of laboratory hydraulic-fracture growth: Tip behavior and width profile, SPE J, 6(1), 2001, pp. 14-24
We performed acoustic measurements in a time-lapse sequence in scaled labor
atory tests. The advantage of time-lapse measurements is that the fracture
response can be separated from the background signal. As a consequence, not
only can the hydraulic fracture be detected, but its shape and geometry ca
n be measured during its growth. This application requires the combined inf
ormation of both compressional- and shear-wave measurements. We apply this
technique to propagation, flowback tests, and reopening of hydraulic fractu
res.
Acoustic waves excite diffractions at the fracture tip. These diffractions
are used to locate and to characterize the fracture tip. The acoustic measu
rements indicate that we can distinguish between a dry tip and the fluid fr
ont of the fracture.
Shadowing of shear-wave transmissions allows estimation of the moment of fr
acture initiation. The width profile of the fracture is determined with com
pressional-transmission measurements. This application is based on the fact
that the attenuation and time delay of compressional transmissions are pro
portional to the fracture width. Analysis of a flowback test shows that the
fracture closed at the wellbore but remained open farther away from the we
llbore.