Ground Roll Identification and Fresnel zone

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SUMMARY

This discussion focuses on the identification of ground roll on shot records and the significance of the Fresnel zone in seismic analysis. Ground roll is characterized by its linear, high amplitude, and steep nature on shot records, appearing as a late-arriving packet of energy known as the coda. The Fresnel zone, which is crucial for understanding wave propagation, depends on the wavelength of the ray and highlights the sensitivity of travel time to the surrounding medium's velocity, rather than the velocity along the ray path itself.

PREREQUISITES
  • Understanding of seismic wave propagation
  • Familiarity with shot records and seismograms
  • Knowledge of the Fresnel zone concept
  • Basic principles of ray theory in geophysics
NEXT STEPS
  • Research methods for identifying ground roll in seismic data
  • Study the mathematical implications of the Fresnel zone in wave propagation
  • Explore the impact of wavelength on seismic sensitivity
  • Learn about advanced ray theory and its applications in geophysics
USEFUL FOR

Geophysicists, seismic data analysts, and students studying wave propagation and seismic interpretation will benefit from this discussion.

mcmzie
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(1) How do you identify Ground roll on a shot record?
Is it just the polarized nature of the ground roll that leads to its recognition on a shot record?

(2) What is the importance of the Fresnel zone? and What does it depend on?
 
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You make the assumption that we know exactly what you are talking about.


Please tell us what you mean by ground roll and shot record?
 
On a shot record it will be linear and high amplitude and quite steep (slow). On a single trace (or seismogram) it will be the late arriving packet of high amplitude energy at the end which tails off and sometimes is called the coda.

The Fresnel zone is the zone of sensitivity to the travel time of a ray, it depends on the wavelength of the ray. Did you know, the sensitivity of a ray's velocity is exactly zero to the velocity of the medium exactly on the ray path itself (in contrast to ray theory which adopts an infinite frequency approximation)? The travel time of a ray (a mathematical concept) is actually sensitive to the velocity of the medium around the ray, due to scatterers off the ray which interfere with the wavefront.
 
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