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The amplitude of the reflected wave is predicted by multiplying the amplitude of the incident wave by the seismic reflection coefficient, determined by the impedance contrast between the two materials. [4] For a wave that hits a boundary at normal incidence (head-on), the expression for the reflection coefficient is simply
In geophysics and reflection seismology, the Zoeppritz equations are a set of equations that describe the partitioning of seismic wave energy at an interface, due to mode conversion. They are named after their author, the German geophysicist Karl Bernhard Zoeppritz , who died before they were published in 1919.
In telecommunications and transmission line theory, the reflection coefficient is the ratio of the complex amplitude of the reflected wave to that of the incident wave. The voltage and current at any point along a transmission line can always be resolved into forward and reflected traveling waves given a specified reference impedance Z 0.
Seismic reflection capitalizes on the echo of seismic waves off boundaries where acoustic impedance varies between earth layers. [81] By recording the differences in travel time and wave amplitude, researchers correlate these measurements with subsurface properties to map out velocity structures, akin to seismic refraction but focusing on wave ...
This is known as a Common Midpoint Gather [8] (a midpoint being the area of the subsurface that a seismic wave reflects off before returning to the receiver) and in a typical seismic reflection processing workflow, the average amplitude would be calculated along the time sample, in a process known as "stacking". This process significantly ...
After the seismic wavelet is estimated, it is used to estimate seismic reflection coefficients in the seismic inversion. When the estimated (constant) phase of the statistical wavelet is consistent with the final result, the wavelet estimation converges more quickly than when starting with a zero phase assumption. Minor edits and "stretch and ...
Seismic wide-angle reflection and refraction is a technique used in geophysical investigations of Earth's crust and upper mantle.It allows the development of a detailed model of seismic velocities beneath Earth's surface well beyond the reach of exploration boreholes.
Zoeppritz used Wiechert's work and went on to derive a full set of transmission and reflection coefficients for a plane wave approaching a discontinuity. Zoeppritz was not the first to mathematically describe this phenomenon as the British seismologist Cargill Gilston Knott used a different approach to derive Knott's equations in 1899, [ 6 ...