1887

Abstract

In the GPR frequency range, electromagnetic wave attenuation is largely controlled by dielectric<br>relaxation processes. A primary relaxation commonly occurs in the 10 – 100 MHz range for many<br>earth materials in which the GPR signal propagates effectively. This relaxation leads to strong nonlinearity<br>in the frequency dependent attenuation and occurs in a frequency range that is often used for<br>groundwater investigations.

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/content/papers/10.3997/2214-4609-pdb.157.sageep008
2009-03-29
2020-03-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.157.sageep008
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