Rai, Shivendra Nath ; Singh, Rishi Narain (1981) A mathematical model of water table fluctuation in a semi-infinite aquifer induced by localized transient recharge Water Resources Research, 17 (4). pp. 1028-1032. ISSN 0043-1397
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Official URL: http://www.agu.org/pubs/crossref/1981/WR017i004p01...
Related URL: http://dx.doi.org/10.1029/WR017i004p01028
Abstract
A mathematical model of the water table fluctuation in an unconfined aquifer subjected to a typical localized transient recharge is presented. The aquifer is taken to be homogeneous, isotropic, underlain by a horizontal impermeable base, and linked with a surface reservoir on one side. Sensitivity characteristics of the water table due to variations in the rate of recharge, hydraulic conductivity, and specific yield are illustrated with the help of a numerical example.
| Item Type: | Article |
|---|---|
| Source: | Copyright of this article belongs to American Geophysical Union. |
| ID Code: | 49660 |
| Deposited On: | 20 Jul 2011 14:05 |
| Last Modified: | 20 Jul 2011 14:05 |
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