There is little information available about the hydraulic conductivity of c
oarse podzol profiles where the vertical variation of the structure is cons
iderable. The near-saturated conductivity of two coarse podzol profiles was
measured by tension infiltrometer. The extrapolated saturated conductivity
was 106.9 cm h(-1) in the very coarse sand and 16.7 cm h(-1) in the medium
coarse sand parent soil, and decreased steadily upward, being between 0.7
and 1.3 cm h(-1) in the two top horizons of these profiles. The unsaturated
conductivities measured by the instantaneous profile method were in good a
ccordance with the results of the tension infiltrometer, but the measuremen
t range of the instantaneous profile method was rather narrow. The near-sat
urated hydraulic conductivity and water retention changed in both profiles
in a systematic way, which agrees with the differences in matrix scale of s
tructure as reflected in the measured soil textural and pedogenic propertie
s.