1996
DOI: 10.1016/0378-3774(95)01215-x
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Modeling water balance components in relation to field layout in lowland paddy fields. II: Model application

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Cited by 16 publications
(6 citation statements)
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“…Interaction effect of N2 and submerged water management required higher water use due to higher evapotranspiration rate as a result of its higher leaf area index and evaporation [28]. With regards to water productivity, N2 treated plants under moist water condition gave higher water productivity compared to the rest of the treatment combinations due to its lower water use.…”
Section: Effect Of Water Management On Water Use Percentage Of Watermentioning
confidence: 99%
See 1 more Smart Citation
“…Interaction effect of N2 and submerged water management required higher water use due to higher evapotranspiration rate as a result of its higher leaf area index and evaporation [28]. With regards to water productivity, N2 treated plants under moist water condition gave higher water productivity compared to the rest of the treatment combinations due to its lower water use.…”
Section: Effect Of Water Management On Water Use Percentage Of Watermentioning
confidence: 99%
“…Saved and Water Productivity Submerged water management received higher amount of water use than AWD and moist treatments due to the standing water layer maintained continuously on the plot from crop establishment till ten days to harvest. According to [28] evapotranspiration was intense under continuous submergence. This probably increased the rate of evapotranspiration and percolation in submerged treatments which in turned increased water use.…”
Section: Effect Of Water Management On Water Use Percentage Of Watermentioning
confidence: 99%
“…In the above equations, it is assumed that there is no capillary rise in both freely draining and puddled soils. Capillary rise from puddled (paddy) soils is ignored as the plough layer remains saturated for a considerable length of the crop growth period and is at a higher moisture potential than the capillary fringe at deeper depths (Odhiambo & Murthy, 1996).…”
Section: Proposed Decision Support System (Impasse Ver 10)mentioning
confidence: 99%
“…Quantifying water fluxes over a given soil profile may be achieved either through installing different sensors at appropriate soil depths, or by modeling the movement of water in the porous media, using pedo‐transfer functions and agro‐climatological information. Investigating water balance at the root zone level has several applications, but perhaps the most important one is the improvement of irrigation scheduling (Odhiambo and Murty ; Garcia Prats and Guillem Pico, ). Modeling and/or monitoring water balance at field scale has also a wide variety of applications, such as performing economical and hydrological analysis of on‐farm reservoirs (Panigrahi et al ., ; Roost et al ., ).…”
Section: Introductionmentioning
confidence: 97%