Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/5662
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dc.contributor.authorSeethapathi, P. V.-
dc.date.accessioned2021-01-22T15:35:29Z-
dc.date.available2021-01-22T15:35:29Z-
dc.date.issued1992-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/5662-
dc.description.abstractThe Use of digital model for simulation of aquifer systems has become a common practice in the recent past. However most of the times, the modeller is faced with a task of calibrating the model with inadequate/ unreliable data which in turn causes lack of confidence over the results thus obtained. An attempt is made in this paper to suggest reasonably viable method for calibration of ground water models for regional modelling provided the behaviour of water table is in a state of dynamic equilibrium. The concept of mean year is introduced and the calibration strategy is indicated. A two level bi-seasonal finite difference. Tyson-Weber model is choosen for indicating the calibration strategy.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.subjectGround Water Qualityen_US
dc.subjectRegional Aquiferen_US
dc.title11-Regional Aquifer Modelling in Areas With Limited Data.en_US
dc.typeTechnical Reporten_US
Appears in Collections:Proceedings of the Seminar on Ground Water Hydrology, 17-18 July 1992 at New Delhi, Vol-I

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