At the VIL site, the SFH/L runs yielded higher Kfs values than the SFH/H
ones by a significant factor of 1.9. In the passage from hw = 0.03 m
to hw = 1.5 m, CV(Kfs) did not change appreciably at the two sites
established on sandy loam soils (AR, VIL) and it clearly decreased
in the finer textured soils. On the other hand,