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     Polarization

Fresnel Reflection Coefficient

[Under Construction]

     The Fresnel reflection coefficient describes the impedance contrast at a change in electrical and magnetic properties in a material.   It describes the amplitude of the amount of energy that is reflected and transmitted across the boundary where the change in properties occurs.  The classical equation describing this behavior is for a very thick interface, such as the interface between two half spaces.  In thin-layered media (thin compared to a wavelength), the classical Fresnel reflection coefficient requires modification.

    Fresnel zone...

(equations)

(references)

(illustrations)

 

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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