Structural variations of sand-bearing airflow over dune at southeastern fringe of Tengger Desert |
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Authors: | Email author" target="_blank">Eerdum?HasiEmail author |
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Institution: | Hasi Eerdum China Center of Desert Research at Beijing Normal University, Key Laboratory of Environmental Change and Natural Disaster of the Minis-try of Education of China, Beijing 100875, China |
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Abstract: | From the analytical results of observed data on sand transport rates at different positions of dune surface at southeastern
fringe of Tengger Desert, it has been found that the vertical distribution of blown sand flux exhibits a noticeable variation
when sand grains move upslope and downslope of dune surface under the action of wind force. Within the height of 20 cm above
the sand surface, the vertical distribution of mass flux at different positions from toe to dune crest of stoss slope of sand
dunes coincides with a single exponentially decaying law; while the vertical distribution of mass flux over the lee slope
occurs as two variable zones, with the height of 8–12 cm as the dividing line, the sand transport rate below this height exponentially
decreases with increasing height, but above this height decreases in a power function law. On the stoss slope, the relative
sand transport rate in the upper layer of sand flow tends to decrease with the increasing wind velocity and the total sand
transport rate towards the dune crest due to the shortened trajectory length of saltation sand grains moving upslope. On the
lee slope, the increase in lift-off height and trajectory length of saltation sand grains moving downslope leads to the increase
in relative sand transport rate in the upper layer of sand flow. |
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Keywords: | sand dune vertical distribution of sand flux stoss slope lee slope fitting relation |
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