Ocean seismic wave simulation method and system based on index random distribution
A technique of random distribution, simulation methods, applied in the fields of seismology, seismic signal processing, etc. for areas covered by water
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Embodiment 1
[0044] Such as figure 1 Shown, the inventive method comprises:
[0045] Preparation steps:
[0046] Input data:
[0047] 1. The background velocity of seawater, which is usually a known constant, varies slightly between 1500-1520m / s in different sea areas.
[0048] 2. Exponential autocorrelation function x and z variables describing the disturbance, the unit is meter, describing the spatial scale of the velocity disturbance. According to different values, the influence of inhomogeneity on seismic wavefield propagation can be analyzed, ranging from a few tenths of meters to several meters (for example, 0.1 meters to 9 meters.), this variable is given different values according to different research purposes.
[0049] Step 1: Simulate the seawater medium as a combination of large-scale velocity background field and small-scale velocity disturbance, such as formula (1), and this tiny velocity anomaly can be regarded as a random event, which can be used as a two-dimensional o...
Embodiment 3
[0086] The size of the seawater velocity model is 4000m×3000m, the background velocity is 2000m / s, and the autocorrelation lengths are a=b=1m, for example figure 2 is the seawater velocity exponential random distribution model, from figure 2 It can be seen that the seawater velocity is 2000m / s as the background velocity, and there are random high and low velocity disturbances. Seismic wave forward modeling is carried out on this model, and the seismic records obtained are as follows: Figure 3-1 and Figure 3-2 as shown, Figure 3-1 The exponential random distribution model shown in the forward simulation shows that there are obvious scattered waves under the direct waves and reflected waves, while Figure 3-2 The forward modeling results of the uniform seawater velocity model shown do not show scattered waves, which cannot effectively reflect the phenomenon of seismic wave scattering in seawater. Extract single-channel records for partial zoom-in comparison, such as F...
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