Ground
Penetrating Radar:
Soil Velocity: Pipe Test
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Because metals reflect nearly 100% of radar energy a metal pipe is ideal for this test, but its diameter should be large enough to be detected with the antenna wavelengths employed (a low frequency antenna with longer wavelengths will require a larger diameter pipe). Conyers and Goodman (1997:110) assert that the long axis of the antenna must be placed parallel to the pipe in order that a maximum amount of radar energy can hit the narrow target and that image enhancements may be required to "see" the reflection in the data, but I have not noticed this problem at depths of a meter or less.
This figure shows the resultant GPR profile obtained with a GSSI 400 MHz antenna. The tick marks at top represent meter marks obtained with a survey wheel, using 50 scans/m. The range setting was 40 nS (10-9 seconds) two-way travel time (TWTT). The ground surface reflection is approximately at 3 nS while the pipe, located at the peak of a characteristic hyperbolic reflection, is at approximately 13 nS.
Here are the relevant data:
Soil Velocity: V = 0.5 m / 5 nS = 0.1 m/nS This figure represents the average radar velocity through the first 50 cm of soil. Soil velocity may also be estimated, but less accurately, through analysis and measurement of hyperbolic form. Relative Dielectric Permittivity (RDP) With an estimate of soil velocity the relative dielectric permittivity (K) may be computed:
where C = speed of light in a vacuum (0.2998 m/nS) and V = velocity of radar energy as it passes through a material (in m/nS), so:
and K = 8.99 |
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Contribution
by: Kenneth
L. Kvamme, Archeo-Imaging Lab, University of Arkansas