JYT-C1 Borrowing-line Telecontrol High-density Expansion Survey System

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Dispatch in 3 to 7 working daysShips in 3–7 days · DDP / CIF / FOB
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Overview

About the JYT-C1

In order to promote the integration of resistivity/induced polarization sounding arrays and upgrade traditional centralized high-density electrical method instruments, we optimized the "Electrical Exploration Electrode Array Line Borrowing Remote Control" (invention patent ZL.201711013579.5, inventors: Liang Binghe and Ge Weizhong). This system not only reduces the number of wiring electrodes for field exploration, but also breaks through the exploration depth, reaching a detection depth of 600-800 meters. Borrowing-line Telecontrol High-density Expansion System R&D Since 1973 Precise & Efficient Smart & Simple Free upgrading at the original price after purchasing within six months Using the remote control low-density electrical method system through borrowed wires, it changes the traditional high-density electrode layout method to solve the problems of shallow exploration depth and large blind spots in traditional high-density electrical exploration. It is a new conceptual method for electrical exploration that can be used with traditional high-density electrical instruments. The power electrodes AB are placed at both ends of the measurement area, and the receiving electrodes MN are placed in the middle of the measurement area. With the minimum variation of electrode combinations, the most effective resistivity data can be obtained, greatly improving the measurement depth of traditional high-density electrical instruments. It can effectively measure high-precision data withi

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This innovative electrical array does not require the use of multi-core cables, but only relies on power supply AB wires for remote control, changing the detection depth

Key Advantages

Applications Qicha Hainan 2015 Hainan 2017 Low-density inversion resistivity cross-section The yellow represents the designed underground curtain wall, which adopts a three-dimensional dragon-shaped array to expand the effective range and increase the depth of inversion. It is several times more effective than the three-dimensional snake-shaped high-density inversion. Stereo anomaly inversion resistivity image The red is the survey line coordinate axis X, direction from west to east; black is the vertical survey line coordinate axis Y, direction south to north; blue is the elevation coordinate axis Z, direction from bottom to top, and the color mark on the left is the ground contour scale. The gray surface is the 500Ωm isosurface, and the resistivity in the enclosed area is greater than 500Ωm; the purple surface is the 300Ωm isosurface, and the resistivity in the enclosed area is less than 300Ωm; the three-dimensional resistivity image shows the distribution of low-resistance areas, with an altitude of 2760m and shallower than the north and south. There are low-resistivity anomalies in the direction, which is inferred to be an underground river or karst development zone; no low-resistivity anomaly is found below an altitude of 2750m, and it is inferred that the deep karst development is weak. Drilling and interwell electromagnetic wave CT were arranged to verify the 3D array resistivity results.

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