TECHNICAL PAPERS
Apr 15, 2002

Discharge-Drawdown Relationship of Eccentric Wells

Publication: Journal of Hydrologic Engineering
Volume 7, Issue 3

Abstract

In the literature approximate and exact theoretical equations are presented for steady-state flow toward a discharging well, which is located eccentrically in a circular aquifer along whose outer cylindrical boundary either the drawdown or the flux is zero. This paper presents the results of using a physical model to test the validity of an analytical solution that describes drawdown for a well, which is placed eccentrically in a circular island aquifer. It is constructed in a sandbox model with several wells to conduct numerous steady-state tests. This study shows that the analytical equations are valid for small drawdowns. However, the equations do not represent higher drawdowns in the wells that are eccentrically located in the circular island model under steady-state flow in an unconfined aquifer.

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References

Babbit, H. E., and Caldwell, D. H. (1948). “The free surface around and interference between gravity wells.” Engineering Experiment Station Bull. Series No. 371, 45(48), Univ. of Illinois, Urbana, Ill.
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Hantush, M. S., and Jacop, C. E.(1960). “Flow to an eccentric well in a leaky circular aquifer.” J. Geophys. Res., 65, 3425–3431.
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Information & Authors

Information

Published In

Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 7Issue 3May 2002
Pages: 260 - 264

History

Received: Sep 12, 2001
Accepted: Sep 12, 2001
Published online: Apr 15, 2002
Published in print: May 2002

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Authors

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Mehmet Emin Bı˙rpinar
PhD, Yildiz Technical Univ., Hydraulic and Civil Engineering, 80750 Yildiz, İstanbul, Turkey.
Şükrü Ayhan Gazı˙oğlu
PhD, Yildiz Technical Univ., Hydraulic and Civil Engineering, 80750 Yildiz, İstanbul, Turkey.

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