Earthquake wave equation generation method and system
A wave equation and generation system technology, applied in the fields of seismic exploration and geological exploration, can solve the problems of difficult to deal with the change of medium speed, low precision, insufficient hardware conditions, etc., to improve the calculation accuracy and stability, good numerical stability, good stability
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example 1
[0208] Example 1: dt=0.00025s, vΔt Δx = 1.228 .
[0209] in, image 3 The result of the finite difference method of the left figure is unstable and the solution diverges;
[0210] image 3 the right Figure II The result of the order ADPI method is stable and the solution is correct.
example 2
[0211] Example 2: dt=0.00075s, vΔt Δx = 1.165 .
[0212] in, Figure 4 The result of the finite difference method in the left figure is unstable and the solution diverges
[0213] Figure 4 the right Figure II The results of the first-order ADPI method are stable and the solution is correct
[0214] Boundary condition analysis:
[0215] Absorbing boundary conditions are very important when modeling seismic records using the wave equation. In a limited area, when numerical methods are used to calculate, if the boundary is not processed, boundary reflection will occur. There are many methods for eliminating boundary reflections. Cerjan et al. attenuate outwardly propagating waves by introducing a lossy medium near the computational boundary. Since there will be reflection at the interface of two lossy media with different absorption coefficients, more absorbing layers are required to have a bette...
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