WebA plane-wave method for computing the three-dimensional scattering of propagating elastic waves by a planar fracture with heterogeneous fracture compliance distribution is … WebSep 5, 2024 · P wave velocities increase with stress in the propagation direction and follow a power law of the form V p = α(σ’/kPa) β; analyses and experimental results show that stress-sensitive fracture stiffness and fracture density define the α-factor and β-exponent; conversely, long-wavelength velocity versus stress data can be analyzed to ...
Analysis for oblique wave propagation across filled joints based …
Web9.1 Waves at planar boundaries at normal incidence 9.1.1 Introduction Chapter 9 treats the propagation of plane waves in vacuum and simple media, at planar boundaries, and in combinations confined between sets of planar boundaries, as in waveguides or cavity resonators. Chapter 10 then discusses how such waves can be generated and received by WebABSTRACT We use 2D and 3D finite-difference modeling to numerically calculate the seismic response of a single finite fracture with a linear-slip boundary in a homogeneous elastic medium. We use a point explosive source and ignore the free surface effect, so the fracture scattered wavefield contains two parts: P-to-P scattering and P-to-S scattering. … inbox is not showing up in outlook
5.1: Plane Waves at Normal Incidence on a Planar Boundary - Engineering
WebMar 5, 2024 · Reflection from transmissive boundaries. Often more than one wave must be added to the given incident wave to satisfy all boundary conditions. For example, assume … WebMay 23, 2024 · The GWP ( p = 64, γ = 0.6, ε = 40) is incident on the interface with an incidence angle of 30° (Fig. 2 a). The wave packet behaves as a particle travelling along the straight seismic ray. When it hits the interface, it splits into a reflected packet and a transmitted packet (Fig. 2 a). Figure 2. Open in new tab Download slide WebJournal of Geophysical Research, B, Solid Earth and Planets 101(11): 25,337-25,346 incledon parow