A Multi-source Seismic Interferometry Method for Advance Geological Prediction of Tunnels
A technology of advanced geological prediction and earthquake interference, which is applied in seismology, seismic signal processing, seismic signal receiver, etc., can solve the problems of insufficient research on advanced geological prediction, and achieve outstanding substantive features, no safety hazards, and pertinence strong effect
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Embodiment 1
[0064] Embodiment 1, adopt as Figure 5 The numerical simulation model of the cave shown. The size of the model is 370m in the horizontal direction and 350m in the vertical direction, and the tunnel section is 10m wide, located at 150-160m in the vertical direction of the model. The tunnel at the end of the blasting source layout has been excavated for 30m, and the tunnel at the end of the geophone layout has been excavated for 50m; on the central axis of the tunnel, a circular karst cave with a radius of 2m filled with air is set at 150m in the horizontal direction. In order to ensure that the numerical simulation is closer to the construction situation of the tunnel drilling and blasting method, 20 blasting sources are used, which are evenly arranged on the end face; 21 geophones are used, which are also evenly arranged on the end face.
[0065] After the blasting source is blasted according to the method of the present invention, the data is collected by the geophone group...
Embodiment 2
[0066] Embodiment 2, adopt as Figure 7 The fault numerical simulation model shown. The size of the model, the location of the tunnel, the excavation of the tunnel, and the location and quantity of blasting sources and geophones are the same as those in Embodiment 1 above. The set fault 1 is 30m away from the face of the geophone end, and the set fault 2 is 100m away from the face of the geophone end. Both faults are 2m wide and run through the entire model longitudinally.
[0067] After the blasting source is blasted according to the method of the present invention, the data is collected by the geophone group and subjected to seismic interference processing, and the obtained characteristic map is as follows: Figure 8 shown. It can be seen from the figure that there is an anomaly area 1 around 0.135 s, which is in the form of an interface, and its position is obtained at 29.7m by using the relationship between time and surrounding rock velocity, which is basically consisten...
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