Haitao Cao, Seiji Nakagawa, Roohollah Askari
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 126(10) 2021年10月
The Krauklis wave is a slow dispersive wave, generated in fluid-filled fractures. By analyzing the resonant frequency and quality factor of the Krauklis wave, the fracture dimension and fluid properties can be estimated. However, the accuracy of the estimation of fracture dimension and fluid properties depends on deciphering factors affecting the Krauklis wave such as fluid viscosity, fracture geometry, fracture compliance, and stiffness ratio, some of which have not been experimentally studied yet. We have developed an experimental apparatus to study the Krauklis wave within a trilayer model consisting of a pair of aluminum plates and a mediating viscous fluid layer. We utilize a piezoelectric source and miniature pressure transducers in our measurements. To evaluating the effects of the fracture aperture and fluid viscosity, we examine the impact of complex and realistic fracture geometry by introducing spatially varying aperture, surface roughness, and compliant partial surface contact provided by springs. The phase velocity, resonant frequencies, and quality factors (a) increase with the expansion of fracture aperture and (b) decrease with the increase of the fluid viscosity. Additionally, (c) phase velocity, resonant frequencies, and attenuation decrease with the increase of mechanical compliance. Furthermore, rough and wedge-shaped fracture surfaces tend to slow down the Krauklis wave. Since the Krauklis wave is used by different disciplines such as volcanology, glaciology, and the petroleum industry to characterize fracture dimensions and properties of the fluids involved, our experimental findings can be used as a benchmark to develop comprehensive theoretical models to better interpret the Krauklis waves.Plain Language Summary Fractures play an important role in fluid transports in geological settings (e.g., impermeable bedrock aquifers, volcanos, and petroleum reservoirs). To determine the scale of the fluid transport (e.g., the volume of gases that reaches the surface from magma), it is necessary to estimate the size of subsurface fractures. There is a specific seismic mode, called the Krauklis wave, that is generated from fractures when the fluid pressure within the fractures is disturbed. Since the Krauklis wave is initiated from fractures, it can be used to estimate their sizes and the fluids involved. However, an accurate interpretation of the Krauklis wave requires understanding the fundamental parameters that affect the Krauklis wave. These parameters include fracture aperture, fluid viscosity, fracture geometry, and fracture mechanical compliance. By conducting a comprehensive experimental study, we investigate the effects of the aforementioned parameters on the Krauklis wave. Our results can facilitate analyzing the Krauklis wave's dispersion, dissipation, and resonances properties to enhance fracture characterization.