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Philip Philip (1957)
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Effect of Irrigation Frequency and Nitrogen Fertilization on Growth and Water Use of a Kikuyugrass Lawn (Pennisetum clandestinum Hochst.) 1Agronomy Journal, 58
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No-tillage as compared to tillage practices in dry-land farming of a semi-arid climate.Netherlands Journal of Agricultural Science, 18
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Determination of withdrawal of water from soil by crop roots as a function of depth and timeSoil Research, 5
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Hydraulic Properties of a Clay Loam Soil and the Field Measurement of Water Uptake by Roots: I. Interpretation of Water Content and Pressure Profiles 1Soil Science Society of America Journal, 32
F. Whisler, A. Klute, R. Millington (1968)
Analysis of Steady-State Evapotranspiration from a Soil Column1Soil Science Society of America Journal, 32
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Relation of Root Distribution to Water Uptake and Availability1Agronomy Journal, 56
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M. Nimah, R. Hanks (1973)
Model for Estimating Soil Water, Plant, and Atmospheric Interrelations: II. Field Test of Model1Soil Science Society of America Journal, 37
F. Whisler, A. Klute, R. Millington (1970)
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L. Stone, M. Horton, T. Olson (1973)
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Patterns of Water Uptake and Root Distribution of Soybeans (Glycine max.) in the Presence of a Water Table1Agronomy Journal, 64
P. Rijtema (1965)
An analysis of actual evapotranspiration
Data obtained from careful water balance studies on water uptake by the roots of red cabbage are compared with results obtained from a modified numerical model of Nimah and Hanks. In the modified model the air dry moisture content at the soil surface may vary with time depending on meteorological conditions. The maximum possible rate of evapotranspiration is calculated by considering both meteorological conditions and crop properties. Data are quoted to suggest that the coefficient of the root sink may sometimes vary exponentially with depth. A period of 7 weeks was simulated, and the calculated weekly moisture profiles did not agree completely with those measured in the field. On the other hand, the calculated cumulative rates of evaporation and transpiration were in excellent agreement with the field data. When the original model was used without the suggested modifications, the agreement of these rates with the field data was not as good, an indication that some of these modifications actually improve the predictive capabilities of the model.
Water Resources Research – Wiley
Published: Dec 1, 1974
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