This study was conducted to develop new methods needed to characterize the effects of wheel traffic and tillage on pore structure as measured by water flow through macropores. Unconfined (three-dimensional) saturated and unsaturated infiltration measurements at the soil surface were taken sequentially at field sites to determine the steady-state rate of water flow through different pore-size classes on a Tama silty clay loam. A tension infiltrometer was used to obtain the unsaturated infiltration rates. Wheel traffic reduced infiltration rates in tillages, but caused a greater decrease in infiltration rates in a chisel-plow system than in a no-till. Increasing tension caused proportionately smaller decreases in infiltration rates for wheel-trafficked positions. -from Authors