Three-dimensional Numerical Simulation Method Based on Arbitrary Dipole-Dipole Device
A technology of three-dimensional numerical and simulation methods, applied in CAD numerical modeling, measuring devices, electrical/magnetic exploration, etc., can solve problems such as limited three-dimensional information, inconvenient construction, and too dense measurement data
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Embodiment 1
[0100] Example 1: 3D IP forward modeling of uplift structure model in horizontal terrain
[0101] Construct a three-dimensional double-layer dielectric uplift structure resistivity model, the first layer dielectric resistivity is 40Ω·m, polarizability is 0, and the thickness is 100m; the second layer dielectric resistivity is 100Ω·m, polarizability is 0; the uplift The structure is 150m away from the top interface, and the thickness is 100m. The top interface is 200m along the x direction and 360m along the y direction. , the resistivity of the lower layer medium is 100Ω·m, and the polarizability is 0.
[0102] like Figure 4 Shown is the cross-sectional view of the double-layer medium uplift structure model, in which, Figure 4 Middle (a) is the yz profile, in which the uplift structure is trapezoidal, with a top width of 360m, a bottom width of 760m, and a thickness of 100m; Figure 4 Middle (b) is the xz profile, in which the uplift structure is rectangular, with a width...
Embodiment 2
[0128] Example 2: 3D IP forward modeling under complex undulating terrain conditions
[0129] designed as Figure 8 The resistivity model of the three-dimensional concave terrain structure shown (model yz profile), the resistivity of the model is 100Ω·m, and the polarization rate is 1%; the concave terrain is 30m away from the horizontal surface, the bottom of the terrain is the positive direction, and the side length It is 800m long; a low-resistance anomalous body with a resistivity of 20Ω·m and a polarizability of 20% is placed below the terrain. The anomalous body is 70m away from the top interface, has a thickness of 40m, and is 200m long along the x and y directions.
[0130] The effect of terrain on the normalized transfer function:
[0131] The normalized resistivity transfer function R ρ and the polarizability-normalized transfer function R η , where the dipole source S1 is located on the surface (such as image 3 shown). Calculated as Figure 9 As shown, compar...
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