Wind can be regarded as the most important vector for seed dispersal in ope
n grassland vegetation. Experimental estimates of seed dispersal distances
in this environment are complex because of low arrival probabilities at lar
ge distances. Therefore, a proper mathematical generalization would be esse
ntial to give insight in dispersal probability distributions. Hence a promi
sing individual-based model for seed dispersal presented by Andersen was te
sted for different wind velocities and seeds. Simulation results from the s
eed dispersal model were compared with observations in a horizontal wind tu
nnel. Considering the large variation in seed morphology and mass, the simu
lation results fitted wind tunnel results reasonably well, indicating the g
eneral applicability of the tested model for herbaceous species. Model sens
itivity was evaluated with respect to wind speed and vegetation height. Dif
ferences in wind speed had a larger impact on the tail of the seed shadow t
han on median dispersal. However, vegetation height had little impact on th
e tail of the seed shadow compared to the median.
Terminal velocity (V-t) is the crucial species specific parameter in wind d
ispersal models. There are two frequently used methods to determine V-t: a
dropping method and a method to float seeds in an upward air stream. Howeve
r, these methods have never been compared directly. This paper presents V-t
values determined with both methods. In general results were in the same o
rder. Only for high values of V-t the results of the floating method were f
ound to be lower than the results of the dropping method. Simulation result
s showed that the intraspecific differences in V-t values were an important
factor in determining the seed shadow.