The WARR Machine: System Design, Implementation and Data

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.

[1]  C. H. Dix SEISMIC VELOCITIES FROM SURFACE MEASUREMENTS , 1955 .

[2]  R L Johnson,et al.  Air distribution in the Borden aquifer during in situ air sparging. , 2003, Journal of contaminant hydrology.

[3]  D. Freyberg,et al.  A natural gradient experiment on solute transport in a sand aquifer: 1. Approach and overview of plume movement , 1986 .

[4]  Nectaria Diamanti,et al.  Anisotropy effect on GPR signals , 2015, 2015 8th International Workshop on Advanced Ground Penetrating Radar (IWAGPR).

[5]  M. Toksöz,et al.  Velocity variations and water content estimated from multi-offset, ground-penetrating radar , 1996 .

[6]  Johan Alexander Huisman,et al.  Measuring soil water content with ground penetrating radar , 2003 .

[7]  S. M. Doherty,et al.  Seismic Data Analysis: Processing, Inversion, and Interpretation of Seismic Data , 2000 .

[8]  Francesco Soldovieri,et al.  GPR Response From Buried Pipes: Measurement on Field Site and Tomographic Reconstructions , 2009, IEEE Transactions on Geoscience and Remote Sensing.

[9]  Tavi Murray,et al.  Semblance response to a ground-penetrating radar wavelet and resulting errors in velocity analysis , 2010 .

[10]  Gary R. Olhoeft,et al.  Geophysics and solvents: The Borden experiment , 1993 .

[11]  A. P. Annan,et al.  Impulse radar sounding in permafrost , 1976 .

[12]  M. Moskalevsky,et al.  Velocity of radio waves in glaciers as an indicator of their hydrothermal state, structure and regime , 1993, Journal of Glaciology.

[13]  M. Taner,et al.  SEMBLANCE AND OTHER COHERENCY MEASURES FOR MULTICHANNEL DATA , 1971 .

[14]  John H. Bradford,et al.  Cable Effects in Ground-Penetrating Radar Data and Implications for Quantitative Amplitude Measurements , 2016 .

[15]  R. Yelf,et al.  Where is true time zero ? , 2004, Proceedings of the Tenth International Conference on Grounds Penetrating Radar, 2004. GPR 2004..

[16]  Tavi Murray,et al.  Englacial water distribution in a temperate glacier from surface and borehole radar velocity analysis , 2000, Journal of Glaciology.

[17]  D. Daniels Ground Penetrating Radar , 2005 .

[18]  George A. McMechan,et al.  Acquisition and processing of wide-aperture ground-penetrating radar data , 1992 .

[19]  A. Peter Annan,et al.  Ground‐penetrating radar monitoring of a controlled DNAPL release: 200 MHz radar , 1994 .

[20]  John H. Bradford,et al.  Ground-penetrating radar theory and application of thin-bed offset-dependent reflectivity , 2006 .

[21]  C. Bentley,et al.  Velocity of Electromagnetic Waves in Antarctic Ice , 2013 .