The study of trajectory parameters of saltating sand grains is of great imp
ortance to forming the kinematic theory of wind-sand current. By establishi
ng the simplified theoretical pattern and probing into the relationship bet
ween lift-off angle (alpha) and landing angle (beta), relationship between
the ratio of saltation length (L) to maximum height (H) and lift-off angle
as well as the angular variation laws of any point on the trajectory, it ha
s been demonstrated that the relations among these parameters are nonlinear
. Meanwhile, it has also been proved that the theoretical analysis is basic
ally reliable in accordance with the wind tunnel experiments using high-spe
ed multiflash photography. Generally, the trajectory shapes of saltating sa
nd grains are controlled precisely and the theoretical analysis is closely
combined with the experimental results