1975
DOI: 10.1071/sr9750021
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Simulation of the water balance for plants growing on coarse textured soils

Abstract: A computer simulation model* of the water balance for plants growing on coarse soils was developed and tested against field measurements. The inputs for this model are measurable physical parameters. From the close agreement between simulated and observed results, it is suggested that evaporation, soil water storage and deep drainage may be satisfactorily predicted.

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Cited by 9 publications
(2 citation statements)
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“…Empirical and physically based mathematical models describe unsaturated flow in the root zone and both can be used to predict changes on a field scale [Baier et al, 1972;Carbon and Galbraith, 1975;Feddes et al, 1975]. The concept of 'field capacity,' now defined as the 'percentage of water remaining in a soil 2 or 3 days after having been saturated, and after free drainage has practically ceased' [Rich, 1971], is usually incorporated in the empirical models.…”
Section: Introductionmentioning
confidence: 99%
“…Empirical and physically based mathematical models describe unsaturated flow in the root zone and both can be used to predict changes on a field scale [Baier et al, 1972;Carbon and Galbraith, 1975;Feddes et al, 1975]. The concept of 'field capacity,' now defined as the 'percentage of water remaining in a soil 2 or 3 days after having been saturated, and after free drainage has practically ceased' [Rich, 1971], is usually incorporated in the empirical models.…”
Section: Introductionmentioning
confidence: 99%
“…When LAI is less than 1, E is split into transpiration, E t , and evaporation from bare soil E b . Then, E = LAIxE t + (l-LAI)xE b , LAI<1 LAI = GRNMAT/1000 E t and E b are determined by a special soil water sub-routine (Carbon & Galbraith, 1975).…”
Section: The Leyfarm Modelmentioning
confidence: 99%