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Khan Z. Jadoon, Samir Al-Mashharawi, Sherif M. Hanafy, Gerard T. Schuster, Thomas M. Missimer
Pág. 1 - 14
Wadi aquifers in Saudi Arabia historically have been recharged primarily by channel loss (infiltration) during floods. Historically, seasonal groundwater levels fluctuated from land surface to about 3 m below the surface. Agricultural irrigation pumping ...
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Iqra Mughal, Khan Z. Jadoon, P. Martin Mai, Samir Al-Mashharawi and Thomas M. Missimer
A component of designing a managed aquifer recharge system in a dune aquifer is the control of diffusive evaporative loss of water which is governed by the physical properties of the sediments and the position of the water table. A critical water table p...
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Oliver M. Lopez, Khan Z. Jadoon and Thomas M. Missimer
Planning for use of a dune field aquifer for managed aquifer recharge (MAR) requires that hydraulic properties need to be estimated over a large geographic area. Saturated hydraulic conductivity of dune sands is commonly estimated from grain size distrib...
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Authors: A Saeed, Z Khan, M Clark, M Nel and R Smith
Pág. 382
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Sadur Rehman, Shad K. Khalil, Abdur Rehman, Amanullah, Amir Z. Khan, Nazir Hussain Shah
Pág. 82 - 87
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Khan, Z.; Balch, T.; Dellaert, F.
Pág. 1960 - 1972
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H. R. Khan, G. K. McDonald, Z. Rengel
Pág. 271 - 284
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Khan, H. R. McDonald, G. K. Rengel, Z.
Pág. 389 - 400
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