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  4. Approximate discharge for constant head test with recharging boundary: Technical Note
 
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Approximate discharge for constant head test with recharging boundary: Technical Note

Auteur(s)
Renard, Philippe 
Centre d'hydrogéologie et de géothermie 
Date de parution
2005
In
Ground Water, Blackwell, 2005/43/3/439-442
Résumé
The calculation of the discharge to a constant drawdown well or tunnel in the presence of an infinite linear constant head boundary in an ideal confined aquifer usually relies on the numerical inversion of a Laplace transform solution. Such a solution is used to interpret constant head tests in wells or to roughly estimate ground water inflow into tunnels. In this paper, a simple approximate solution is proposed. Its maximum relative error is on the order of 2% as compared to the exact analytical solution. The approximation is a weighted mean between the early-time and late-time asymptotes.
URI
https://libra.unine.ch/handle/123456789/18460
DOI
10.1111/j.1745-6584.2005.0024.x
Autre version
http://dx.doi.org/10.1111/j.1745-6584.2005.0024.x
Type de publication
Resource Types::text::journal::journal article
Dossier(s) à télécharger
 main article: Renard_Philippe_-_Approximate_Discharge_for_Constant_Head_Test_20060929.pdf (346.56 KB)
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