Ground Roll Identification and Fresnel zone

In summary, the conversation discussed the identification of Ground roll on a shot record and its polarized nature. The importance of the Fresnel zone and its dependence on the wavelength of the ray was also mentioned. The concept of travel time of a ray and its sensitivity to the velocity of the medium around it was also brought up.
  • #1
mcmzie
5
0
(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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  • #2
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?
 
  • #3
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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1. What is ground roll identification?

Ground roll identification is the process of distinguishing ground roll, which is the low-frequency noise generated by the ground, from other seismic signals. This is important in seismic data processing, as ground roll can obscure important geological features.

2. How do you identify ground roll in seismic data?

Ground roll can be identified by its characteristic appearance on a seismic record, typically appearing as a semi-circular or curved line. It also has a lower frequency compared to other seismic signals. Additionally, ground roll can be identified by its consistent appearance across multiple channels on a seismic record.

3. What is the Fresnel zone in seismic data processing?

The Fresnel zone is a volume of rock surrounding a seismic source or receiver that contributes significantly to the recorded signal. It is important in seismic data processing because it affects the resolution and quality of seismic images.

4. How is the Fresnel zone calculated?

The Fresnel zone is calculated using the wavelength of the seismic signal and the distance between the source and receiver. The formula for calculating the Fresnel zone is: Z = √(λd/2), where Z is the Fresnel zone, λ is the wavelength, and d is the distance between the source and receiver.

5. Why is it important to consider the Fresnel zone in seismic data processing?

Considering the Fresnel zone in seismic data processing is important because it affects the resolution and quality of seismic images. By understanding and controlling the size of the Fresnel zone, the seismic data can be processed to produce clearer and more accurate images of subsurface structures.

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