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Abstract

Ground penetrating radar (GPR) is a relatively new technique for<br>investigating shallow geologic, engineering and hydrologic features. The principles<br>and theory are based on the wave equation derived from Maxwell’s Equations for<br>electromagnetic wave propagation, and the antenna designs have evolved from field<br>testing. GPR data is presented in the form of time-distance plots that are analogous<br>to conventional seismic records. This paper presents an overview of: 1) the<br>theoretical basis for GPR, 2) guidelines for GPR interpretation, and 3) practical<br>field examples of GPR data.

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/content/papers/10.3997/2214-4609-pdb.213.1989_002
1989-03-13
2024-04-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.213.1989_002
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