Gradient of travel time in layered media?

In summary, the conversation discusses a problem with a fixed picture and variables x_0, y_0, z_0, V_0, and V_1. The travel time equation is given and a publication is mentioned, stating the derivative of travel time with respect to x_1. The accuracy of the publication is questioned and a hint is requested.
  • #1
ytht100
20
0
I have a problem of the following picture. x_0, y_0, z_0, V_0, and V_1 are fixed.

http://postimg.org/image/6r0ogcx3f/

gradient.jpg
The travel time is obviously [tex]t = \frac{1}{{{V_1}}}{[{({x_1} - {x_c})^2} + D_1^2]^{1/2}} + \frac{1}{{{V_0}}}{[{({x_c} - {x_0})^2} + D_0^2]^{1/2}}[/tex]

According to a high-profile publication, the derivative of traveltime with regard to x1 is [tex]\frac{{\partial t}}{{\partial {x_1}}} = \frac{1}{{{V_1}}}\frac{{({x_1} - {x_c})}}{{\sqrt {{{({x_1} - {x_c})}^2} + D_1^2} }}[/tex]. Here, it seems to ignore dx_c/dx_1, is it correct?

I guess it is wrong.

Thanks a lot!
 
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  • #2
Please, someone give me a hint.
 
  • #3
What is that publication? Can you give a reference to the article?
 

Related to Gradient of travel time in layered media?

1. What is the gradient of travel time in layered media?

The gradient of travel time in layered media refers to the change in travel time of a seismic wave as it passes through different layers of rock or other materials. It is a measure of the variation in the speed of the wave as it travels through the layers.

2. How is the gradient of travel time calculated?

The gradient of travel time is calculated by taking the derivative of the travel time function with respect to the distance traveled. This can be done using mathematical formulas or through numerical methods such as finite difference methods.

3. Why is the gradient of travel time important in seismic imaging?

The gradient of travel time is important in seismic imaging because it can provide valuable information about the subsurface structure and composition. By analyzing the changes in travel time, scientists can infer the presence of different rock layers and other geological features.

4. How does the gradient of travel time affect seismic data processing?

The gradient of travel time affects seismic data processing by influencing the accuracy and quality of the resulting images. Inaccuracies in the gradient of travel time can lead to artifacts and distortions in the final images, making it crucial to accurately calculate and account for this parameter.

5. What factors can affect the gradient of travel time in layered media?

Several factors can affect the gradient of travel time in layered media, including the velocity of the seismic wave, the thickness and composition of the layers, and the angle of incidence of the wave. Other external factors such as topography and near-surface structures can also contribute to variations in the gradient of travel time.

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