Whey, the liquid byproduct of cheese production, can improve minesoils by increasing the aggregate stability of soils high in sodium or susceptible to erosion. Whey effects on soil hydraulic properties, however, are not known. In this experiment, we determined whey effects on infiltration rates ( at water potentials of -30 = or less) and unsaturated hydraulic conductivities of surface soil horizons after a winter wheat(1/iticum aestivum L.) growing season. The experimental design was a randomized complete block with three replications of four liquid whey application treatments, totaling either 0, 202, 404, or 808 Mg/ha ( control, low, medium, and high, respectively). In Fall 1992 near Kimberly, ID, a field of Portneuf silt loam (Durixerollic Calciorthid) was leveled, subsoiled, then roller-harrowed twice. After planting Malcolm wheat on September 15, we furrowed all plots and then constructed a berm around each. At 3-week intervals beginning on May 19, 1993, either zero, one, two, or four flood applications of 202 Mg/ha of whey were made to each plot, without subsequent tillage. After August wheat harvest, a tension infiltrometer was used to measure vadose zone, unsaturated flow characteristics in the bottom of undisturbed furrows, where most whey had infiltrated. Infiltration rates at potentials of -60 and -150 mm decreased linearly as whey applications increased from 202 to 808 Mg/ha. At a potential of -60 mm, hydraulic conductivity increased but then decreased with whey additions. In short, soil hydraulic properties were little affected by surface whey additions of 404 Mg/ha or less.Additional