Physically based mathematical models are capable of portraying the pro
cess of soil water utilization by crop roots. However, there are few d
etailed studies comparing simulated profile water content with those o
bserved experimentally in varying soil moisture status. The purpose of
the present study was to test the accuracy of a diffusion based soil
water simulation model under wet, moderately wet and dry soil water re
gimes in a coarse textured lateritic (Oxic Haplustalf) soil using pean
ut as a test crop. Simulated water content (SWC) usually matched well
with the measured water content (MWC), the matching being very accurat
e when roots penetrated to the maximum depth (1.2 m). During the early
part of the drying cycle simulated values were closer to observed val
ues than they during the middle and later part of the drying cycle. Un
der wet regime simulated values were closer to observed values.