The WARR Machine: System Design, Implementation and Data

Author:

Diamanti Nectaria12,Elliott E. Judith1,Jackson Steven R.1,Annan A. Peter1

Affiliation:

1. Sensors & Software Inc., 1040 Stacey Court, Mississauga, L4W 2X8, ON, Canada

2. Now at the Department of Geophysics, Aristotle University of Thessaloniki, 54124, Greece

Abstract

In this paper, we describe a ground penetrating radar (GPR) system called the wide angle reflection and refraction (WARR) machine, outline the design and discuss the implementation challenges. WARR and the closely related common-mid-point (CMP) GPR soundings have been standard survey methods to measure velocity since GPR first existed. Earliest efforts demonstrated the variation in ice sheet velocity versus depth. Although GPR multi-offset soundings are valuable survey methods, they have seen little adoption since many systems are not bistatic. In addition, surveys most often use a single transmitter with a single receiver deployed sequentially at varying antenna separations, making data acquisition slow. Modern instrumentation with recent advances in GPR timing and control technology has enabled deployment of systems with multiple concurrent sampling receivers. This development has resulted in the ability to continuously acquire multi-offset WARR data at the same rate as two dimensional (2D) common offset reflection surveys in the past. The concomitant issues of survey design plus organizing the WARR data storage, documentation and analysis present numerous challenges. The extraction of velocity information from the large volumes of GPR WARR/CMP data demands automated analysis techniques. We have explored the use of normal move out (NMO) stacking at creating enhanced zero offset section from multi-offset data. Furthermore, we investigated the use of semblance analysis at estimating move-out velocities in order to apply in the NMO stack. These traditional seismic processing steps have proven to be less effective with GPR. These conclusions point to the differences in data character between seismic and GPR. Results of in-field deployment are used to illustrate advances to date and point the way to further advancements.

Publisher

Environmental and Engineering Geophysical Society

Subject

Geophysics,Geotechnical Engineering and Engineering Geology,Environmental Engineering

Reference25 articles.

1. Annan, A.P. 2005, Ground-Penetrating Radar: inNear-Surface Geophysics, Butler D.K. (ed.), Society of Exploration Geophysicists13, 357–438, Tulsa, Okla. Society of Exploration Geophysicists, 2005.

2. Annan, A.P. 2015, Depth axes and NMO correction for finite offset GPR data. Sensors & Software Inc. Technical Note, PEMD0568, pp. 16.

3. Impulse radar sounding in permafrost

4. Annan, A.P. and Jackson, S.R. 2017, The WARR Machine: inNinth International Workshop on Advanced Ground Penetrating Radar (IWAGPR2017), Edinburgh, U.K.

5. Babcock, E.L. Annan, A.P. and Bradford, J.H. 2017, Cable effects in ground-penetrating radar data and implications for quantitative amplitude measurements: Journal of Environmental and Engineering Geophysics, 21, 98–103.

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