s400 300m groundwater detection equipment is to use the natural soil source, and to save the heavy power supply system without passing through the artificial field, so as to achieve the purpose of simplicity and portability.After data acquisition, the instrument can automatically present the figure through the unique built-in calculation function, and the collected data can also be transmitted to the computer drawing to form the cross section. Through the clear understanding of the specific information of the section water (aquifer), the geological layer structure can be quickly determined.
Technical parameters of 300 meter groundwater detection equipment
Product model: s400
1. measurement depth: 100M / 150m / 300m (optional)
2. measurement parameters: electric field components vs " (MV) of different frequencies of magnetotelluric field
3. measuring range: 0mv-1500mv, automatic range conversion of the instrument
4. measurement accuracy: 0.001mv
5Channel gain: 1-300000 times
6. measurement method: three frequency, two pole profile
7. measurement frequency: single frequency, three frequency, 36 frequency, 40 frequency
16. it has the function of electrode detection and power supply monitoring
17Humanized human-computer interface, high-speed CPU control, menu prompt function.
Detection depth of 300s hand held water detector
300rice
measuring method
Bipolar section
Automatic noise reduction, super anti-interference ability
Using the three-stage gain technique, the field source signal can be enhanced in the weak field source
Human machine interface, high speed CPU control, menu prompt
Automatic side volume, automatic data storage, no need to record data
It can store 99 measuring lines and 99 measuring point data of each measuring line
The measurement data can be displayed, and the data line can also be directly connected to the computer and instrument to input the data into the computer
display
128X64 LCD
A/D conversion
16Bit 1MSP
Power resources
Rechargeable battery
With electrode detection and power supply monitoring
Measurement parameters
Electric field component of different frequency magnetotelluric field Δ vs "(MV)
