Modeling of GPR Clutter Caused by Soil Heterogeneity

Figure 3

GPR profiles on a 5 m long profile acquired on (a) April 15th, (b) April 21st, (c) April 28th, (d) May 5th, (e) May 26th, (f) June 3rd, and (g) June 17th. Travel time was converted to depth using mean permittivity measured by TDR (Figure 4). Amplitudes of the profiles were normalized throughout the measurements. Only a bandpass filter was applied.

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