Inhaltsbereich
Ground Penetrating Radar (GPR)
GPR setup as common offset (COF): Receiver and transmitter antenna are fixed at a constant antenna separation. The ground wave (GW) velocity is derived from the antenna separation and the travel time of the GW.
Specification
- GSSI SIR20 multi-channel radar system
- Antenna (by GSSI)
- 1x 100MHz
- 2x 270MHz Model - 5104A
- 2x 400MHz Model - 5103A
- 2x 900MHz Model - 3101A
- 1x Off ground antenna 1.5GHz - Model 4108
- Survey wheel
- Antenna cables: 2 x 7m and 2 x 30 m
- Software: ReflexW, RADAN
Application
- General:
- Estimation of the soil water content: Concerning soil moisture estimation, the physical principle of GPR is the same as of TDR measurement. The physical principle is based on the relationship between the EM wave velocity and the dielectric constant/electrical permittivity of soils. For example, the permittivity of dry soils varies between 3 and 6, whereas water has a value of 80. The permittivity of soils depends on the volumetric proportion of solid, fluid and gaseous components. Therefore, the dielectric constant correlates directly with the water content, but also is influenced by other parameters of the soil, like density or content of organic matter. The main difference is that TDR uses a guided EM wave, whereas the GPR technique is based on an unguided wave. Different techniques can be applied for soil moisture estimation by GPR. Generally, we can differentiate in the surface reflection, the reflection/diffraction, the ground wave and the transmission analysis method.
- Exploring of hydro-geological structures: The spatial distribution of layers (e.g. ground water level) and structures within the soil can be identified by the analysis of the measured radargram.
- Projects:
- Study area:
- South African Geodynamic Observatory (SAGOS)
- Geodetic Observatory Wettzell, Germany
Maintenance/Support
Link
Common offset measurements on a plowed field.
3D Radargram: The velocity change of the ground wave indicates a change of soil moisture variations.