1887

Abstract

An exploration method using shallow soil temperature<br>measurements as an exploration tool to find permeable bodies at<br>depth in an impermeable matrix is described. The depth of seasonal<br>soil temperature variation is discussed. A method of measuring<br>soil temperatures below the depth of seasonal variation is<br>described. Simple finite difference modeling techniques to predict<br>thermal anomaly characteristics are presented. Case histories are<br>presented which demonstrate the application of the method for<br>groundwater.

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/content/papers/10.3997/2214-4609-pdb.210.1992_031
1992-04-26
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.210.1992_031
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