Method for detecting tunnel overlying formation cavities and uncompacted areas
A technology for stratum cavities and tunnels, which is applied in engineering geophysical prospecting and tunnel engineering fields, can solve problems such as unsatisfactory detection results, high cost, and time-consuming construction, and achieve the effects of convenient testing, low cost, and avoiding interference
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Embodiment 1
[0046] Embodiment 1, for as Figure 5The theoretical numerical model is shown for inversion imaging. The size of the model is 50m and 50m in the horizontal and vertical directions, respectively. In order to be close to the actual geological model, the theoretical numerical model is set as follows: the burial depth of the overlying strata of the tunnel is set to 0m-19.5m; the upper and lower interfaces of the tunnel lining are respectively set, and the burial depth of the upper interface of the lining is 19.5m-20.5m. The buried depth of the lower interface is 29.5m-30.5m; the buried depth of the tunnel space layer is 20.5m-29.5m; the buried depth of the underlying bedrock layer of the tunnel is 30.5m-50m, and the velocity and density values set for each layer are detailed in the table 1. Example 1 is a model without anomalies, that is, the stratum overlying the tunnel is set as a homogeneous medium, and the velocity values are the same. The source points are located on t...
Embodiment 2
[0048] Embodiment 2, adopt as Figure 8 The anomaly model with holes is shown. The size of the model, the distribution of dielectric layers, the location and quantity of seismic sources and geophones are all the same as those in Embodiment 1 above. In addition, a cavity anomaly with a diameter of 2m is set in the overlying strata of the tunnel. The anomaly is located at the lateral position of the model at 24-26m and the longitudinal position at 9-11m. The set anomaly model P-wave velocity value is 340m / s.
[0049] According to the method of the present invention, the model is sequentially excited by seismic waves, the data is collected by the geophone (group) and the seismic wave reflection CT inversion imaging is performed, Figure 9 The initial model input for the inversion in this embodiment is consistent with the initial input model in Example 1, and the resulting characteristic map obtained by inversion imaging is as follows Figure 10 shown. It can be seen from the f...
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