Evaporation from soil (E-s) was studied in an agroforestry system using soi
l microlysimeters, where the tree and crop components were grown together,
in monocultures where the two components were grown separately, and in bare
soil. All measurements were carried out at an equatorial field site in Ken
ya. E-s varied according to the different shade regimes and as a function o
f proximity to trees and/or crops. Over periods of 3-21 days, the maximum r
eduction in E-s compared to completely bare soil was 40%. This was observed
under a maize canopy when the crop leaf area index (LAI) was 2.0. When the
trees had similar values of LAI (1.9), the reduction in E-s was lower at 2
3%. However, in contrast over an entire rainy season, the presence of trees
over bare soil reduced total seasonal E-s by 24%, compared to an 8% reduct
ion in E-s by the maize crop. The maize crop was less effective in reducing
E-s largely because of its shorter duration. (C) 1999 Elsevier Science B.V
. All rights reserved.