ABSTRACT TAILWATER runoff from 570-m graded furrows was varied from 0 to 8 hr to determine the vari-ability of grain sorghum yield with length of run. During the first 3 to 4 hr, cumulative infiltration into the Pullman clay loam is 5 to 7 cm. Infiltration into the slowly permeable soil then approaches the steady-state rate of less than 0.25 cm/hr. Continuing to irrigate after the entire furrow reached the steady-state infiltration rate did not significantly increase the field average yield. The root zone at the tail end of the field was not fully wetted, but the soil water was sufficient for normal plant growth, and tailwater run-off was less than 10 percent of the applied water. As a result, the irri-gation water-use efficiency varied inversely as the duration of tailwater runoff. By reducing the duration of tailwater runoff, additional land could be irrigated with the limited groundwater supply. Allowing irrigation tailwater runoff is a method of achieving more uni-form water distribution along graded irrigation runs. Criddle et al. (1956) recommended an irrigation advance time equal to one-fourth of the total application time. With this guideline, they also recom-mended a cutback or reduced furrow stream, after water advances to the end of the irrigation run. Irriga-tion tailwater recovery systems are an alternate method of reducing tailwater runoff losses. Bondurant (1969) presented design criteria for these systems and showed how they can be operated to simulate a cut-back furrow stream. Most irrigation system design criteria have been developed for the alluvial soils of the Western US. Irrigated soils in the Great Plains are often fine-textured with much lower infiltration rates. Pullman and related soils of the Southern Great Plains have a slowly permeable subsoil that determines the steady-state infiltration rate. During the first 4 to 6 hr, the infil-tration rate is relatively high, but deceases rapidly as the topsoil is saturated. Subsequently, the slowly permeable subsoil limits the steady-state infiltration rate to less than 0.25 cm/hr. Musick et al. (1973) showed that the flow rate 540 m down irrigated furrows became steady within 4 hr after the wetting front passed. The unique infiltration char-acteristics of Pullman clay loam allow 800-m-long graded furrows to be irrigated without large, deep-percolation losses (Aronovici and Schneider 1972). Most of the irri-gation run is adequately irrigated, but the lower end usually has a soil water deficit, even after tailwater has run off for several hours. In irrigation water management, the crop must be considered in addi-tion to the soil and irrigation prac-tices. Musick and Dusek (1971) showed that grain sorghum in level borders effectively utilized small irrigations throughout the growing season. During 7 treatment-years, reducing the size of each irrigation from 10 to 5 cm increased the irri-gation water-use efficiency from 148 to 226 kg/ha-cm. Musick et al. (1973) presented water-use and grain sorghum yield data from three equal-length segments of 540-m irrigated furrows. Water-use effi-ciencies for the three segments down the irrigation run were 135, 165, and 211 kg/ha-cm, respectively. The potential for efficient water use throughout an irrigation run exists even if the irrigation water distri-bution is quite nonuniform. The study reported here was con-ducted to determine the feasibility of a graded-furrow irrigation system on Pullman clay loam with limited or no tailwater runoff.
Read full abstract