Experimental data are presented demonstrating the influence of boundar
y layer flow conditions on aerodynamic entrainment of grains in the ab
sence of intersaltation collisions. New methods are proposed for (1) t
he unambiguous determination of aerodynamic threshold for any grain po
pulation and (2) approximation of the probability density function (PD
F) distributions of threshold shear velocity for aerodynamic entrainme
nt. In wind tunnel experiments, the orderly spatial development of flo
w conditions within a developing boundary layer over the roughened sur
face of a flat plate constrains the aerodynamic threshold condition in
terms of both mean and fluctuating values. Initial grain dislodgement
s and subsequent erosion from narrow strips of loose, finely fractiona
ted ballotini were recorded photographically as wind speed was increas
ed. Boundary layer parameters, including average threshold shear veloc
ity (Ut), were calculated using the momentum integral method. Direct
observations show that sporadic oscillation of grains preceded dislodg
ement. At slightly higher velocities most grains rolled over their nei
ghbours before entering saltation. Initial entrainment in spatially se
mi-organized flurries of 50 or more grains was followed by quiescent p
eriods at airflow velocities close to threshold. These observations pr
ovide strong circumstantial evidence linking both the nature and spati
al pattern of initial grain motions to sweep events during the fluid b
ursting process. For each grain fraction, values of Ut were found to
span an unexpectedly wide range and to decrease downwind from the lead
ing edge of the plate as turbulence intensity increased. A probabilist
ic entrainment model is applied to the aerodynamic threshold condition
so as to incorporate the effects of changing turbulent flow regimes o
ver the plate. Analysis of strip erosion curves gives both an objectiv
e definition of the threshold condition and usable approximations of t
he PDF for Ut required by the model and for future stochastic treatme
nt of the threshold condition.