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WDA-1 IP Sounding Meter
PRODUCT PARAMETERS
- Unique and open measuring process control
- Measuring various parameters, wide application
- High power supply, wide current range, high accuracy
- Bluetooth technology facilitating wireless remote control
- extending data storage capacity and collection software functions
Description
WDA-1 DC Electrical Resistivity IP Sounding Meter
Abstract
WDA-1 super digital DC resistivity/IP meter, is a newly developed electricalmethod instrument, adopting many advanced technologies such as tablet PC, Bluetooth,24bit A/D, and high power control. WDA-1 is specific instrument for the variousgeophysical explorations, with the most parameters, various funcitons, and the mostadvanced performance at present.
Working principle
Electrical prospecting is a group of geophysical prospecting methods that use the electrical properties of rocks and ores (such as conductivity, electrochemical activity, magnetic conductivity and dielectric properties, the so-called “electrical differences”) to find minerals and study geological structures. It uses instruments to observe artificial and natural electric fields or alternating electromagnetic fields, analyze and interpret the characteristics and laws of these fields to achieve the purpose of prospecting.
Vertical electrical sounding (VES) is a geophysical method for investigation of a geological medium. The method is based on the estimation of the electrical conductivity or resistivity of the medium. The estimation is performed based on the measurement of voltage of electrical field induced by the distant grounded electrodes (current electrodes).
Applications
●Energy resource exploration
●City geophysical exploration
●Railway and bridge prospecting
●Metal and non-metal mineral resources prospecting
●City geophysical exploration
●Hydrology and engineering geology to inspect base of dam
●Flood protection levee for incipient faults
Features
●Unique and open measuring process control
●Measuring various parameters, wide application
●High power supply, wide current range, high accuracy
●Bluetooth technology facilitating wireless remote control
●extending data storage capacity and collection software functions
Detailed description
WDA-1 can works with intelligent cable system for multi-electrode 2D/3D Resistivity/IP imaging survey.


● The transmitter and the receiver are designed in one unit, portable and light. The 200V internal transmitting power of WDA-1 can conduct Res survey in wide variety of explorations.
● It is available to measure data of voltage (VP), current (IP), apparent resistivity (ρS), Self-Potential (SP), apparent polarizability (M~M7), metal factor (G1~G7), half decay time (TH), deviation (r), induce polarization ratio (J) and voltage decay curve, etc.
● Max power up to 9000W (1500V*6A), voltage input range is 160Vp-p, high measuring precision of small signal.
● Bluetooth technology enables the tablet PC to control the WDA-1 mainframe in 10 meters.
● Data collecting and data storage are controlled by tablet PC. Software is flexible to be upgraded and extended.
● Integrated with multistage filtration and signal enhancement technologies and suppression against common mode interference and differential mode interference. Measurement precision is high.
● Transmitting unit supports over-voltage protection, over-current protection and AB open-circuit protection as well as DC high voltage reverse connection protection.
Specifications
Receiving section
| Item | Parameters |
| Voltage | ±32V (24 bit A/D). If Vp≥5mV, accuracy is ±0.2% ±1LSB If 0.1mV≤Vp<5mV, accuracy is ±1% ±1LSB |
| Apparent polarizability measurement accuracy | ±0.2%±1LSB |
| Input impedance | >50MΩ |
| SP compensation range | ±10V |
| Maximum supply current | 6A (24bit A/D with WDZJ-3, no more than 2.5A) If Ip≥5mA, accuracy is ±0.2% ±1LSB If 0.1mA≤Ip<5mA, accuracy is ±1% ±1LSB |
| Suppression | For 50Hz industrial frequency interference (common mode and differential mode interference), suppression is more than 80dB. |
Transmitter
| Item | Parameters |
| Maximum transmitting power | 9000W |
| Maximum supply voltage | 1500V (with WDZJ-3, no more than 450V) |
| Supply current | 6A |
| Transmitting power pulse width | 1~60s, duty cycle is 1:1 |
Other parameters
| Item | Parameters |
| Power supply | Internal 7.4V 4Ah rechargeable battery continuously lasts for 20 hours (or 12V external power supply). |
| Ports support (transmitting unit) | A, B, M and N connecting ports, DC high voltage input ports and external battery terminals, 2 cable ports, RS-232, Bluetooth. |
| Working temperature | -10℃~+50℃, 95%RH |
| Storage temperature | -20℃~+60℃ |
| Weight | ≤4kg |
| Dimension | 270mmx246mmx123mm |
| Internal power source | Mximum voltage 96V (two notches, 48V and 96V); Maximum current is 0.7A |
FAQ
① In SI, it is m·s-2, and one percent of it is the international unit abbreviation g.u.;
② Conversion between SI and CGS: 1g.u.=10-1 mGal
Gravitational field: The space around the earth with gravity is called the gravitational field.
Gravitational potential: The gravitational potential W in the gravitational field is equal to the work done by a particle of unit mass moving from infinity to that point.
① The normal gravity field of the earth: Assuming that the earth is a rotating ellipsoid (reference plane), the surface is glossy, the internal density is uniform, or it is distributed in concentric layers, the density of each layer is uniform, and the deviation of the shape of the ellipsoid from the geoid is very small, then the gravity field generated by the earth is the normal gravity field.
② The normal gravity value is only related to the latitude, the smallest at the equator and the largest at the poles, with a difference of about 50,000 g.u.; the rate of change of the normal gravity value with latitude is the largest at 45° latitude, and zero at the equator and the poles; the normal gravity value decreases with increasing altitude, and its rate of change is -3.086 g.u.. The main feature of the long-term change is the "westward drift" of the geomagnetic elements, both the dipole field and the non-dipole field drift westward, and have a global nature.
The gravitational field strength is equal to the gravitational acceleration in both numerical and dimensional terms, and the two are in the same direction. In gravity exploration, all references to gravity refer to gravitational acceleration. The gravitational field strength at a point in space is equal to the gravitational acceleration at that point.
Gravity exploration is an exploration method that is based on the density difference of rocks and ores. Since density difference will cause local changes in the normal gravity field of the earth (i.e. gravity anomaly), it is used to solve geological problems by observing and studying gravity anomalies.
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