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- W815485798 abstract "The meteorological variables which characterize the different seasons of the year produce large changes in the rate of evaporation from exposed surfaces after irrigation. Erie, French, and Harris (1968) have published information depicting the seasonal evapotranspiration of water by crops in Arizona, and Cooley (1970) has computed seasonal evaporation rates from open water surfaces. For both types of surface, the amount of time elapsed since the last addition of water does not materially affect the rate of water loss (provided the crop has a full canopy and water is not withheld too long, of course). On the other hand, bare soil dries rapidly at the surface, and the evaporation rate from it depends upon both the meteorological variables that characterize the season of the year and the amount of time that has elapsed since the last irrigation or rain. We shall present data which illustrates how the evaporation rate from one soil, bare Adelanto loam in Phoenix, changes with season and with time since the last irrigation. DESCRIPTION OF THE DATA Ten years ago precision weighing lysimeters were installed in a field at the U.S. Water Conservation Laboratory in Phoenix, Arizona [Van Havel and Myers (1962)]. The soil in the field and in the lysimeters is Adelanto loam. Eleven" @default.
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- W815485798 date "1971-04-23" @default.
- W815485798 modified "2023-09-23" @default.
- W815485798 title "Seasonal Effects on Soil Drying After Irrigation" @default.
- W815485798 hasPublicationYear "1971" @default.
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