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To understand the importance of Fermat’s principle in deriving Snell’s law in the reflection and refraction cases.
Introduction(介绍)
Fermat’s principle states that a wave will take that path which will make the traveltime stationary (i. e., maximum or minimum). Mathematically:
dT / dX = 0,
where T is the total traveltime along the wave path and X is the distance from the source to the point where the wave changes its direction (e.g., point of reflection or refraction). In most situations in the earth, the stationary path is the minimum-time path.
大家也可以思考一下如何证明透射定律。
Objective
To calculate the reflection coefficients(反射系数) between different lithologies and determine the effect of ignoring the density in calculating the reflection coefficient.
Introduction
The reflection and transmission coefficients (R, T) are defined as:
R = (Z2 – Z1) / (Z2 + Z1)
T = 1 – |R| = 2Z1 / (Z2 + Z1);
where Z = D V is the acoustic impedance, D and V are the density and velocity, respectively.
Exercises
Given the attached velocity-density model(如图2):
1. Calculate R = R(V,D) at each interface(界面).
2. Calculate T = T(V,d) at each interface.
3. Calculate R = R(V) at each interface using only velocities (i.e., drop r from the formula).
4. Calculate the absolute error between R found in steps 1 & 3. The absolute error is defined as:
5. Plot E(%) versus:
a. |R|
b. V2/V1
c. D2/D1
6. How does E(%) changes with:
a. |R|
b. V2/V1
c. D2/D1
7. What would you do if you were given only V and have been asked to calculate R?
图2 某口井速度和密度随深度的变化关系
代表密度的意思()里面是单位----与作业里面的D意思相同-----
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