Deep Underground Water Detector

① Hi-Fi Signal Conditioning Amplifier Guaranteed signal accuracy
The analog circuit part of the front-end signal conditioning amplifier of the instrument adopts integrated packaging and shielding, which greatly enhances anti-interference, improves the signal input accuracy, and greatly improves the measurement accuracy of the instrument.

② High performance processor Run multiple algorithms
Adopt high-performance processor, run various algorithms, make the output stable and accurate, and ensure the measurement accuracy of the instrument

③ 10.1 inch touch screen operation
Real-time 2D/3D and curved images

① Handles ② Power Button ③ Charging Port ④ Multi-function Data Port ⑤ Cable Connector

① Cable ② Hammer ③ Electrodes x 16

④ Wired connection probe (optional)
Capable of operating on various terrains, including concrete, rock, and frozen soil. It can be operated by a single person.

⑤ Wireless connection golden rod (optional)
Fully wireless. Capable of operating on various terrains, including concrete, rock, and frozen soil. It can be operated by a
single person.

Image Interpretation: The high-resistivity red zone in the shallow subsurface (0-40m) indicates a dry, loose sedimentary cover. A
distinct low-resistivity purple anomaly is observed at 50-90m. The blue low-resistivity anomalous zone at 105-180m may represent a
well-developed aquifer. The high-resistivity zone below 255m is likely the aquifer's basement, a bedrock layer that prevents
further downward percolation of groundwater, consistent with the actual water-bearing geological structure. It is recommended to
drill at point 5, with an expected water depth between 110-200m.
Actual Drilling Results: The first water flow appeared at around 110m depth, primarily composed of quartz sandstone. As drilling
continued, the water volume increased significantly. The final drilling depth was 120m. The actual conditions align with the image
analysis.

Image Interpretation: The red high-resistivity zone at a shallow depth of 40m is likely an unconsolidated sedimentary cover. The zone between 60-140m may be a well-developed porous aquifer, with a maximum estimated thickness of 80m. The red high-resistivity zone between 140-240m is presumed to be a rock layer with poorly developed pores and low permeability. Below the blue low-resistivity zone at 240m, there may be a well-developed deep confined aquifer. Drilling into the deep confined aquifer can obtain overflow replenishment from other aquifers, ensuring a stable water supply. It is recommended to drill at point 3, with an expected water depth between 60-140m and below 260m.Actual Drilling Results: The aquifer top was encountered at a depth of 50m, and water flow increased significantly. Water flow slowed down at around 170m. To ensure a stable water supply for future needs, the customer continued drilling, and the final borehole depth was 295m, with a water yield of 40 cubic meters per hour. The actual results are consistent with the image analysis.