Ground Penetrating Radar
GRORADAR™ by Gary R. Olhoeft, PhD
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Introduction and History        Electromagnetic Wave Propagation

Velocity   Wavelength    Attenuation   Dispersion

Rocks, Soils and Fluids:  Electrical Properties    Magnetic Properties

Environmental Influences        Heterogeneity, Anisotropy and Scale       Radar Equation

Scattering

Antenna Polarization

[Under Construction]

     Electromagnetic waves are polarized.  This means the electric field is a vector pointed in a particular direction.  Generally, the magnetic field is perpendicular to the electric field, and the direction of propagation is perpendicular to both electric and magnetic field directions.  This is a different context than used previously for magnetic or dielectric polarization properties in which polarization was describing energy storage properties of materials.   Most commercial ground penetrating radar systems use linearly polarized antennas.   The most common antenna arrangement is with the electric fields of the transmitter and receiver antennas aligned in parallel with each other, parallel with the earth, and towed in a traverse direction perpendicular to the electric field direction.  This results in a wave propagating perpendicular to the surface of the earth, into the earth.   If such an arrangement is pulled across a buried metallic pipe (or wire or rebar) with the electric fields aligned parallel to the length of the pipe, the pipe appears in the ground penetrating radar data as an excellent reflector, with a hyperbolic shape (the shape is the result of the antenna pattern and geometry of traverse motion).  If the antennas are rotated 90 degrees, so they cross the pipe with the electric field direction at right angles to the long axis of the pipe, the pipe disappears (it's still there, but very tough to see).  This latter arrangement is a good way to see past rebar in concrete.   The electric field parallel alignment is also an excellent polarization to measure subsurface layering.   If the antennas are reconfigured with one antenna electric field perpendicular to the other (called cross-polarized), they become insensitive to layering and more sensitive to scatterers like pipes, independent of alignment of the pipe compared to the antennas.   In general, three sets of measurements are required with antennas oriented (relative to the electric fields) parallel to the surface of the earth and: 1) parallel to each other and perpendicular to traverse direction, 2) parallel to each other and parallel to traverse direction, and 3) perpendicular to each other (cross-polarized).  The change in polarization that occurs as a propagating wave encounters a contrast in electromagnetic properties (and is scattered) is described by the Stokes-Mueller Matrices.
     There are also other kinds of antennas and polarization, such as left and right hand circularly polarized logarithmic spiral antennas... (more)

(references)

(illustrations)

 

Fresnel Reflection     Snell Angle      Stokes-Mueller Matrices     Poincare Sphere

Antennas     Coupling     Near / Far Fields     Waveguides   Multipathing     Resonance

Survey Design     Contrast     Geometry      Resolution     Depth of  Investigation     Orientation  

Noise     Interference     Logistics

Data Acquisition   Data Processing   Modeling   Interpretation   Uncertainty

Applications:     Noninvasive Surface     Borehole      Airborne     Satellite and Space  

GPR Bibliography


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