Technical Abstract: We measured soil hydraulic properties on intact soil cores from wheel track and no-wheel track areas of four soil types, after long-term no-till or reduced-till crop rotations in semiarid eastern Colorado. The soil texture varied from sandy loam to silt loam. The results showed a large variability but no consistent differences in water retention curves and hydraulic conductivity (Ksat) between track and no-track areas. However, all water retention and Ksat data could be quantified by essentially universal models that require only soil bulk density and 33-kPa water content. For water retention data from three field soils in the literature where wheel track effects were significant, we present a simple model to derive retention curves for track areas from curves of the no-track areas. This is presented as a topic for further research. The Ksat data for these soils were consistent with the general Ksat-effective porosity relationship pdeveloped previously.