Geological inversion method based on land and underwater direct current combined measurement
A direct current and terrestrial technology, applied in geophysical surveying, radio wave measuring systems, measuring devices, etc., can solve problems such as technical incompleteness, and achieve the effect of eliminating the impact
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Embodiment 1
[0069] Such as figure 1 As shown, in order to achieve the transition from the shore to the deep water gradually, so as to achieve the purpose of effectively controlling the relevant geological bodies below and around the water body, the present invention first requires that the electrode array be gradually arranged from the land to the water, and then arranged on the land again;
[0070] In order to reduce the impact of the water body on the inversion, the present invention requires the use of sonar devices to control the three-dimensional model of the water body and bottom topography in the current entire work area before the design of the observation system and inversion, and to collect water samples at different depths and points , to analyze the three-dimensional distribution of the resistivity of the water body, and whether there is an obvious macroscopic stratification of the resistivity.
[0071] according to figure 1 For the land and underwater resistivity layout show...
Embodiment 2
[0078] Such as figure 2 As shown, the present invention discloses a geological inversion method based on joint measurement of land and underwater direct current, comprising the following steps:
[0079] 1. Land-underwater-land electrode arrangement
[0080] Such as image 3 As shown, the vertical Z in the figure represents the elevation, and the horizontal X represents the horizontal distance. It is necessary to arrange the electrodes from the land to the underwater, and then to the land. The underwater electrodes are in contact with the bottom of the water, and the water depth is about 1.5 meters. The electrodes pass through the water from the left bank to the right bank.
[0081] 2. Establish a water body model
[0082] Such as Figure 4 As shown, according to the sonar detection results, the spatial distribution of the water body is established; the actual water surface and the elevation of the water body are obtained according to the GPS measurement; according to the ...
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