2003
DOI: 10.1016/s0378-3774(02)00081-1
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Estimating water table contributions to corn and sorghum water use

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Cited by 55 publications
(25 citation statements)
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“…where ∆W is the difference in soil moisture in the 0-120-cm layer between the beginning and end of experimental period, P and I are precipitation and irrigation respectively, G is groundwater imbibition to the root system (calculated following the method described in Sepaskhah et al [29]), R is the surface runoff (there was no surface runoff, as the plot was flat), F is drainage (assumed to be zero, because drip irrigation and precipitation are too low to cause drainage below 2 m). The water use efficiency (WUE, kg·ha −1 ·mm −1 ) was calculated as the grain yield (Y, kg·ha −1 ) divided by ET:…”
Section: Measurementsmentioning
confidence: 99%
“…where ∆W is the difference in soil moisture in the 0-120-cm layer between the beginning and end of experimental period, P and I are precipitation and irrigation respectively, G is groundwater imbibition to the root system (calculated following the method described in Sepaskhah et al [29]), R is the surface runoff (there was no surface runoff, as the plot was flat), F is drainage (assumed to be zero, because drip irrigation and precipitation are too low to cause drainage below 2 m). The water use efficiency (WUE, kg·ha −1 ·mm −1 ) was calculated as the grain yield (Y, kg·ha −1 ) divided by ET:…”
Section: Measurementsmentioning
confidence: 99%
“…The values of ET o in Bajgah and Kooshkak areas were calculated by Penman-FAO (Doorenbos and Pruitt, 1977) method using the meteorological data obtained from weather stations in the areas. The Penman-FAO method was used as recommended by Sepaskhah (1999) for the local conditions. The amount of water for each irrigation event was considered as cumulative ET c in the respective duration and the water was applied with a flexible hose and measured with a volumetric flow meter.…”
Section: Experimental Designmentioning
confidence: 99%
“…Crop-water use from the water table may be important in arid and semi-arid regions (Sepaskhah et al, 2003). Shallow groundwater should be viewed as a potential water resource for crop use provided that upflow does not contribute to processes of soil deterioration, such as salinization or acidification, nor limits crop growth through water logging (Benz et al, 1984).…”
Section: Introductionmentioning
confidence: 99%