Time domain aero-electromagnetic data inversion method based on conductivity-depth imaging
An airborne electromagnetic and data inversion technology, applied in the field of data inversion, can solve the problems of low accuracy of fast imaging method and difficult selection of initial model of inversion method, and achieve fast and stable inversion method, high convergence rate and imaging accuracy. , the effect of solving difficult choices
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Embodiment 1
[0028] The workflow of the present invention is as figure 1 shown, including the following steps:
[0029] (1) Assume that the time-domain aeronautical electromagnetic detection system maintains a stable flight state when the aircraft is flying, the coil maintains a horizontal state during the flight, and the coil height is 30m. Using the central loop source time-domain airborne electromagnetic one-dimensional forward modeling algorithm, calculate the conductivity of the uniform half-space geoelectric model in the range of 0.0001S / m-100S / m and the vertical direction two of 26 time channels within 10ms after power failure Secondary field electromagnetic response value, according to the electrical conductivity and electromagnetic response value to establish a functional relationship table between the electromagnetic response and electrical conductivity;
[0030] (2) Substitute the one-dimensional forward modeling electromagnetic response simulation data of the three-layer H-typ...
Embodiment 2
[0049] The steps of this embodiment are basically the same as those of Embodiment 1, except that the one-dimensional forward modeling electromagnetic response simulation data of the three-layer H-type geoelectric model input in step (2) of Embodiment 1 is changed to that of the inclined low-resistivity layer geoelectric model. The one-dimensional forward modeling electromagnetic response data, the sampling time of the secondary field is consistent, the height of the transmitting coil is still 30m, and the geoelectric model of the inclined low-resistance layer is shown in the figure Figure 4 As shown, the resistivity of the middle inclined low-resistivity layer is 50Ω·m, and the resistivity of the surrounding rock is 500Ω·m.
[0050] The inversion result is shown in Fig. Figure 5 , 6 , as shown in 7, Figure 5 is the conductivity-depth imaging result map, Figure 6 is the inversion result map of the initial model constructed from the conductivity-depth imaging results, F...
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