A study of the hydrological effects of clearing a catchment covered by nati
ve, dry sclerophyl eucalypt forest, and replanting it with a Pinus radiata
plantation was undertaken. The purpose of this study was to examine the eff
ects of vegetation species change and growth rates on streamflow.
The water balance of the two forests was observed for a 27-year period; 11
years before and 16 years after the forest conversion. Data on precipitatio
n, canopy interception, forest floor interception and water yield, combined
with analysis of the rate of vegetative growth and development of the fore
st floor litter, enabled investigation of the effects of forest conversion
on the water balance components for the whole period (1967-1993). The age o
f a P. radiata plantation during the first 16 years of its growth greatly a
ffected the streamflow and other water balance components. For the first 4
years after forest conversion, the rates of evapotranspiration and streamfl
ow changed completely. Transpiration and the evaporation of intercepted rai
nfall ceased after the forest was cleared. The changes in the first 4 years
were followed by a further transformation of the whole evapotranspiration
process as the pine plantation developed. A trend of increasing evapotransp
iration and canopy and forest floor interception losses as the plantation g
rew, with decreases in runoff, was followed by an equilibrium situation in
which streamflow, and the evapotranspiration from soil water storage were s
maller than for the native forest. (C)2000 Elsevier Science B.V. All rights
reserved.