Cable Effects in Ground-Penetrating Radar Data and Implications for Quantitative Amplitude Measurements

Author:

Babcock Esther L.12,Annan A. Peter3,Bradford John H.4

Affiliation:

1. Geotek Alaska, Inc., 907 Dowling Rd., Anchorage, AK 99511Email:

2. Now at United States Geological Survey, 4210 University Dr., Anchorage, AK 99508

3. Sensors & Software, 1040 Stacey Ct., Mississauga, ON L4W 2X8

4. Boise State University Department of Geosciences, 1910 University Dr., Boise, ID 83725

Abstract

Conductive cables have always represented a source of noise in ground-penetrating radar (GPR) data. In some instances, commercially available GPR systems use data processing tools to reduce cable noise. Such processes seldom respect the amplitude fidelity of the signal. For the purpose of careful, quantitative amplitude measurements, use of the raw recorded data is a critical starting point for reliable interpretation of results. During subsequent processing, users can compensate for cable effects to varying degrees. To illustrate the issues inherent with cable noise, we show an example where cable movement during data acquisition generates deviations in reflection amplitude up to 19%. We then present the ramifications of these variations for quantitative data analysis. We conclude that precise cable handling can improve data quality and subsequent data interpretation. Our results are particularly pertinent for quantitative analysis and inversion of GPR data where precise amplitude information is crucial.

Publisher

Environmental and Engineering Geophysical Society

Subject

Geophysics,Geotechnical Engineering and Engineering Geology,Environmental Engineering

Reference8 articles.

1. Annan, A.P. 2005, Ground-penetrating radar: inNear-surface geophysics, Butler, D.K. (ed.), Society of Exploration Geophysicists, Tulsa, Oklahoma, 357–438.

2. Babcock, E.B, 2014, Targeted full-waveform inversion for recovering thin- and ultra-thin-layer properties using radar and seismic reflection methods: Ph.D. thesis, Boise State University, Boise, Idaho.

3. Ground-penetrating radar theory and application of thin-bed offset-dependent reflectivity

4. Bradford, J.H. Clement, W.P. and Barrash, W. 2009, Estimating porosity with ground-penetrating radar reflection tomography: A controlled 3-D experiment at the Boise Hydrogeophysical Research Site: Water Resources Research,45, W00D26.

5. Analysis of a guided wave along a conducting structure in a borehole

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