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Groundwater recharge estimation from ephemeral streams. Case study: Wadi Tabalah, Saudi Arabia
Author(s) -
Sorman Ali U.,
Abdulrazzak Mohamed J.,
MorelSeytoux H. J.
Publication year - 1997
Publication title -
hydrological processes
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.222
H-Index - 161
eISSN - 1099-1085
pISSN - 0885-6087
DOI - 10.1002/(sici)1099-1085(19971015)11:12<1607::aid-hyp490>3.0.co;2-q
Subject(s) - groundwater recharge , wadi , hydrology (agriculture) , depression focused recharge , vadose zone , geology , aquifer , groundwater , water table , surface runoff , hydrogeology , groundwater flow , arid , groundwater model , environmental science , geotechnical engineering , geography , ecology , paleontology , cartography , biology
Abstract Estimation of groundwater recharge to an unconfined aquifer is studied using analytical and numerical techniques and results are compared with field observations. There is an acute need for such estimation in water balance studies in arid climates, and the case study in this paper is for such a region. The wetting front movement in the unsaturated zone depends on antecedent soil moisture, the ponded water depth and its duration, and on the position of the water table and the hydraulic properties of the unsaturated zone. A hydraulic connection between the recharge basin and the aquifer is not immediately established because the wetting front is unsaturated. A numerical model is applied to estimate recharge in an arid‐zone wadi, and its validity is tested by comparing it with an analytical solution of the equations. The calculated recharge values matched the piezometric levels observed at a well site at the edge of the wadi channel. The total recharge depths found by integration in the time domain provided a good estimate of the transmitted volume of water per unit length of wadi channel. The findings were confirmed by runoff volume measurements at gauging stations located in the basin. © 1997 John Wiley & Sons, Ltd.