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http://117.252.14.250:8080/jspui/handle/123456789/3318Full metadata record
| DC Field | Value | Language |
|---|---|---|
| dc.contributor.author | Mishra, G. C. | - |
| dc.date.accessioned | 2019-08-07T11:30:39Z | - |
| dc.date.available | 2019-08-07T11:30:39Z | - |
| dc.date.issued | 1987 | - |
| dc.identifier.uri | http://117.252.14.250:8080/jspui/handle/123456789/3318 | - |
| dc.description.abstract | A mathematical model has been developed for finding the exchange flow rate between a river and a multiaquifer system for varying river stages. The solution has been obtained by discretising the time parameter and using unit response function coefficients. The analytical solution is tractable for numerical calculation. It is found that the storage coefficient of the lower aquifer controls the recharge from the upper aquifer, besides the aquitard resistance. | en_US |
| dc.language.iso | en | en_US |
| dc.publisher | National Institute of Hydrology | en_US |
| dc.subject | Determination of aquifer recharge | en_US |
| dc.title | 7-Determination of aquifer recharge for varying river stages. | en_US |
| dc.type | Technical Report | en_US |
| Appears in Collections: | National Symposium on Hydrology, 16-18 December 1987, Vol.- II at Roorkee | |
Files in This Item:
| File | Description | Size | Format | |
|---|---|---|---|---|
| 7-Determination of aquifer recharge for varying river stages..pdf | 3.44 MB | Adobe PDF | View/Open |
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