1887

Abstract

Borehole radar (BHR) measurements, collected adjacent to a landfill site, demonstrate the useful<br>application of this technique in understanding the near surface (upper 30m) hydrogeological conditions.<br>The stratigraphy consists of relatively uniform ice-contact sand deposits, with the water table at a depth<br>of 16.5 m. Zero offset gathers provide a simple technique for defining stratigraphy, water content and<br>contaminate delineation, Multiple offset gathers, before and during a water injection experiment,<br>demonstrate that velocity tomograms can image water content changes on the order of 0.5 percent.

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/content/papers/10.3997/2214-4609-pdb.205.1996_060
1996-04-28
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.205.1996_060
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