Heat storage in a shallow confined aquifer: geophysical tests to detect the resulting anomaly and its evolution with time

A confined aquifer lying between 4 and 7 m depth was subjected to several injections of hot water. A resulting decrease of electrical resistivity was observed. Measurements were carried out at the surface, using a classical electrical technique. A model explaining the anomaly is proposed.

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Veröffentlicht in:Journal of hydrology (Amsterdam) 1982-01, Vol.56 (1), p.85-98
Hauptverfasser: Benderitter, Y., Tabbagh, J.
Format: Artikel
Sprache:eng
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Zusammenfassung:A confined aquifer lying between 4 and 7 m depth was subjected to several injections of hot water. A resulting decrease of electrical resistivity was observed. Measurements were carried out at the surface, using a classical electrical technique. A model explaining the anomaly is proposed.
ISSN:0022-1694
1879-2707
DOI:10.1016/0022-1694(82)90058-0