The motion of wind-blown sand grains was photographed by a high-speed digital imaging camera in a large blow-off type wind-tunnel under realistic conditions. Well-sorted sands taken from a natural beach and sieved with median diameters (
d50) of 0.15, 0.25, 0.52, 0.68 mm were employed. The horizontal component of the flying sand grain velocity,
ūs, was slower than wind speed,
u at the same elevation. Above the certain height from the sand surface, the sand velocity became nearly to the wind velocity with the height. These results yielded the following empirical equation;
ūs/
u=0.168ln(
z/
d50)-0.139 (
z; height from the sand surface). For the sand with a median diameter of 0.68 mm (
U=11.8m/s), the approximate values of 2.0 m/s and 10-20 degrees were obtained for the falling velocity and angle, respectively, and 1.0 m/s and 20-50 degrees for the rebound velocity and angle, respectively.
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