A simple fractal model is proposed for the dispersion of passive scala
rs in an incompressible homogeneous turbulent flow field. The dispersi
on process is based on a three-dimensional velocity field which is ass
umed to be a linear superposition of Taylor-Green vortices with wave n
umbers and amplitudes as those in a Weierstrass function. The chosen v
elocity field satisfies the continuity equation as well as Kolmogorov'
s inertial range power law, and has a fractal dimension D between uppe
r and lower length-scale bounds. A cloud of tracer particles is relase
d into the flow field and dispersed by the fluid motion, the trajector
ies are numerically integrated from the velocity field. The puffs whic
h result from this process are used to examine some aspects of turbule
nt dispersion, through comparisons with integrated concentration wind-
tunnel measurements. The agreement between numerical and experimental
results indicates the significance of the proposed simulation model.