In the rural catchment of the Maurets (Var, France), storm runoff is simula
ted via two different representations. If in the representation, the soil p
rofile is composed of the observed porous medium settled upon an impervious
substratum, then the calculated flow does not fit the observation data. If
a pervious layer of high water conductivity is inserted upon the imperviou
s substratum to represent the observed fractured basement, the simulated fl
ow better fits the observations. Moreover, in this case, simulations show t
he large participation of old water to the stormflow, as do geochemical ana
lyses of the catchment. (C) 2000 Academie des sciences / Editions scientifi
ques et medicales Elsevier SAS.