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.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609-pdb.157.sageep008
2009-03-29
2024-03-29
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.157.sageep008
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error