Precipitation, throughfall, stemflow and interception losses were determine
d in Chile on 29 research plots grouped in nine research sites, covering a
wide range of rainfall zones, forest types, species, ages and densities. Al
l the data are presented and analyzed on a 12-month time base. Throughfall
varied between 55 and 86% of precipitation (P) and although it was higher i
n coniferous stands than in broadleaved forests the differences were not st
atistically significant. Stemflow varied from 1 to 13% of P in coniferous s
tands and between 1 and 8% of P in broadleaved forests. Stemflow for indivi
dual trees was higher under high annual rainfall and in low dense forests,
and decreased when annual precipitation reduced and forest density increase
d. In broadleaved stands interception losses (I) ranged from 204 to 1097 mm
/year while in coniferous forests I showed a narrower range of variation fr
om 199 to 579 mm/year. Because the final effect of the replacement of nativ
e forests by plantations upon water yield also depends on transpiration and
other evaporation losses, it was not possible to conclude that this substi
tution will increase water availability. In a Monterey pine stand intercept
ion losses increased with the age of the forest because of the tendency for
the branches of this conifer to become horizontal, thus increasing interce
ption capacity and decreasing stemflow. In a native forest that had reached
its climax state interception losses decreased during nine years of measur
ement associated with the continuous reduction of interception capacity of
the dense bamboo understorey. (C) 2001 Elsevier Science B.V. All rights res
erved.