Ding Bosong, Gao Li, CHENG Jianjun, et al. Numerical Simulation of Wind-Sand Flow Characteristics of Inclined Inserting-Type Sand Fence Under Influence of Inserting Plate Angle[J]. Bulletin of Soiland Water Conservation, 2021, 41(1): 132-137.
DOI:
Ding Bosong, Gao Li, CHENG Jianjun, et al. Numerical Simulation of Wind-Sand Flow Characteristics of Inclined Inserting-Type Sand Fence Under Influence of Inserting Plate Angle[J]. Bulletin of Soiland Water Conservation, 2021, 41(1): 132-137. DOI: 10.13961/j.cnki.stbctb.2021.01.019.
Numerical Simulation of Wind-Sand Flow Characteristics of Inclined Inserting-Type Sand Fence Under Influence of Inserting Plate Angle
[Objective] The structure form of existing sand barriers was optimized to maximize the sand retention effect
the characteristics of wind and sand flow of inclined inserting-type sand fences along a railway were studied in order to provide a relevant design reference and scientific basis for the prevention and control of wind and sand disasters.[Methods] Based on the Eulerian two-fluid unsteady model
numerical simulations were conducted on inclined inserting-type sand fences with different inclination angles of the insert plate (15°
30°
45°
and 60°) but the same porosity (30%).[Results] ① The inclination angle of the insert plate gradually increased
the range of the windward side deceleration zone did not change significantly
and the range of the upper acceleration zone and the leeward side vortex zone gradually increased. The tendency of the windward side airflow to bend downward gradually increased
and the angle between the airflow moving upward on the leeward side and the horizontal wind direction gradually increased. ② Under different wind speeds
the wind speeds around the inclined inserting-type sand fence were U-shaped curves. For the same wind speed
the minimum wind speed in the leeward vortex area was negatively correlated with the inclination angle of the plate.[Conclusion] As the inclination angle of the inserting plate increased gradually
the sand on the windward side gradually increased
and the sand on the leeward side gradually decreased. However
the sand in the 1 H range on the leeward side gradually increased. The distance between the main sand distribution on the leeward side and the sand barrier gradually increased.
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