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Spatial variability of field-measured soil-water properties
1973
Hilgardia
Infiltration and redistribution of water following an irrigation was studied, and the work was replicated at 20 locations on a 150hectare plot of land. Hydraulic conductivity was measured as a function of soil-water content at 30.5 cm depth intervals to a depth of 182.9 in twenty 6.5-meter-square plots randomly established over a 150-hectare field. Tensiometers installed at 30.5, 61.0, 91.4, 121.9, 152.4, and 182.9 cm were used to measure hydraulic gradients. Soil-water contents were
doi:10.3733/hilg.v42n07p215
fatcat:zxmu7undgjetxpmv5pyt35m4uy