Ground Penetrating Radar (GPR)
 

Introduction

The GPR technology has been used for about 15 years in civil engineering, geology
and archeology for the detection of buried objects and soil study.

GPR works by emitting into the ground, through a wideband antenna, an
electromagnetic wave covering a large frequency band. This can be done by using a
short pulse or a pure sine wave whose frequency is varied continuously or by steps to cover the desired range. Reflections from the soil caused by dielectric variations such as the presence of an object are measured. By moving the antenna it is possible to
reconstruct an image representing a vertical slice of the soil..

A wide frequency band is needed to achieve a good resolution, but since higher
frequencies do not propagate well, the chosen range is always a tradeoff between
resolution and penetration depth. For antipersonnel mines, a center frequency of 1 to 2 GHz seems to be a good choice for most types of soil.

The GPR is able to detect non-metallic materials as long as their dielectric
characteristics are sufficiently different from the surrounding media.

It must be noticed that systems used in civil applications do not have any automatic
recognition algorithms implemented; this is therefore the domain where most of the
work has to be done, to allow the use of this technology for mine detection.
 

GPR basic principles

Basically, GPR systems work by emitting a short electromagnetic pulse in the ground
through a wideband antenna. Reflections from the ground are then measured to form a vector. The displacement of the antenna allows to build an image by displaying
successive vectors side by side.

Any dielectric discontinuity in a propagating media, as for example the presence of an object, will cause a reflection; its intensity will be higher with increasing difference
between the dielectric coefficients. Typical soils permittivity vary from about 4 to 40,
wet soils having a higher permittivity than dry ones (water has a permittivity of 80).
Permittivity of plastic objects is in the range of 2 to 6.

Typical pulses have a width of the order of a nanosecond or less, with rise time of
some hundred of picoseconds, which correspond to a frequency spectrum of some
hundreds of MHz to 1-2 GHz.

High frequencies are needed to achieve a good spatial resolution, but penetration
depth of electric fields being inversely proportional to the frequency, too high
frequencies are useless after some centimeters. Hence the choice of the frequency
range is a tradeoff between resolution and penetration depth. A system working with
an antenna whose center frequency is at 1 GHz is considered by experts as being a good compromise for anti-personnal mines, allowing to work at depths of 50 cm to 1
m in most soils with a resolution of the order of some centimeters.

Penetration depth will also depend on the nature of the soil which have different
attenuation. For example desert sand has an attenuation of about 1 dB/m for 1 GHz
frequency, clay having attenuation of 100 dB/m at the same frequency.

The reflected wave is sampled and digitized by an A/D converter. The region of
interest is quite short, for example in sand, 1 meter depth corresponding to about 20
ns. Typically 512 points are taken through the region of interest, which correspond to
a sampling rate far too high for standard converters. The solution is to repeat the
generation of the pulse (typical repetition rates range from some tens of KHz to 1
MHz) and to acquire only one sample in each reflected wave, the sampling time being shifted by some tens of ps for each pulse. This allows to use standard and relatively
low cost converters.

By moving the antenna along a line and taking regularly spaced acquisitions, it is
possible to construct an image representing a vertical slice of the ground. These
images show hyperbolas whose apex is located at the objects positions. These
hyperbolas result from the fact that antennas have a certain aperture and capture all
reflections coming from a cone-shaped area below them. These hyperbolas can be
focused by software (migration algorithms) to obtain the real image of the objects.

Typical GPR Output

An alternative to the most used (real pulse) GPR is to work with so called synthetic
pulses. The response to pure sine waves of discrete frequencies of the spectrum of a theoretical pulse are measured. Using the appropriate signal processing algorithms
the response to the theoretical pulse can be reconstructed.
 

Research studies: