Staff Publications

Staff Publications

  • external user (warningwarning)
  • Log in as
  • language uk
  • About

    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

    We have a manual that explains all the features 

Record number 311434
Title Groundwater Recharge in Irrigated Agriculture: The Theory and Practice of Inverse Modelling
Author(s) Boonstra, J.; Bhutta, M.N.
Source Journal of Hydrology 174 (1996)3/4. - ISSN 0022-1694 - p. 357 - 374.
DOI https://doi.org/10.1016/0022-1694(95)02724-6
Department(s) International Institute for Land Reclamation and Improvement
Publication type Refereed Article in a scientific journal
Publication year 1996
Keyword(s) analogen - grondwateraanvulling - hydrologie - irrigatie - modellen - Pakistan - bodemwaterbalans - analogues - groundwater recharge - hydrology - irrigation - models - Pakistan - soil water balance
Categories Geohydrology, Soil Hydrology
Abstract Quantifying the rate of natural groundwater recharge is a prerequisite for drainage design in waterlogged areas. The present study was aimed at determining the seasonal net recharge in the Schedule I-B area of the Fourth Drainage Project, Faisalabad, Pakistan. A numerical groundwater model was developed for the said area and was run in inverse mode to determine the seasonal net recharge. Net recharge values were determined for the period June 1985–June 1990, resulting in five monsoon and five non-monsoon estimates. The data used by the model were the geometry of the aquifer system, the aquifer parameters, and historical water table elevations. The methodology is unique in that it gives information on temporal and areal recharge variations, and requires fewer data than the traditional water-balance method. The maximum average net recharge to the aquifer was calculated as 0.6 mm day−1 during monsoon 1986; the corresponding monsoon rainfall had a return period of some 2.8 years.
Comments
There are no comments yet. You can post the first one!
Post a comment
 
Please log in to use this service. Login as Wageningen University & Research user or guest user in upper right hand corner of this page.