PEAK FLOW REQUIREMENTS FOR SPRINKLER IRRIGATION OF ORCHARDS AS AFFECTED BY SOIL TEXTURE AND PEAK EVAPOTRANSPIRATION
A scheduling procedure was used in 17 orchards, from 1962 to 1965 inclusive, to determine the peak flow of irrigation water required per unit area of land. Irrigation was by the sprinkler method, with portable pipe settings of 12 hours. Peak flow was determined on a steady-flow basis during periods of peak evapotranspiration. Evapotranspiration (ET) was determined by use of evaporimeters. The texture and the water-holding capacity of the soil were also determined. Highly significant coefficients of correlation were obtained between the peak flow required and each of percent sand, average ET per day during the period of peak ET, depth of water applied at each irrigation, length of irrigation interval and various other factors. High correlation coefficients were also obtained among the factors studied. Regression of percent sand and peak ET on peak flow accounted for 90.6% of the variations in peak flow; regression of depth per application and length of irrigation interval accounted for 84.1%. It is suggested that peak flow was affected directly by the depth of water applied at each irrigation and by the length of the "safe" irrigation interval, and indirectly by other factors.