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| 1 | 风沙流中静电力对剪切力的影响显示文摘根据模拟的风沙跃移层中风速廓线分布结果,讨论了电场力对风沙流中气载剪切力和颗粒作用于单位体积气流的体积力的影响.结果表明:沙粒带正电荷时的气载剪切力和颗粒作用于单位体积气流的体积力最大,不带电荷时次之,沙粒带负电荷时的气载剪切力和体积力最小. | 吕萍 黄建平 董治宝 | 2010 | 兰州大学学报(自然科学版)2010，46，5： | 1 |
| 2 | A Wind Tunnel Investigation of the Shear Stress with A Blowing Sand Cloud显示文摘In a blowing sand system,the wind provides the driving forces for the particle movement while the moving particles exert the opposite forces to the wind by extracting its momentum.The wind-sand interaction that can be characterized by shear stress and force exerted on the wind by moving particles results in the modification of wind profiles.Detailed wind pro-files re-adapted to blown sand movement are measured in a wind tunnel for different grain size populations and at differ-ent free-stream wind velocities.The shear stress with a blowing sand cloud and force exerted on the wind by moving par-ticles are calculated from the measured wind velocity profiles.The results suggest that the wind profiles with presence of blowing sand cloud assume convex-upward curves on the u(z)-ln(z) plot compared with the straight lines characterizing the velocity profiles of clean wind,and they can be better fitted by power function than log-linear function.The exponent of the power function ranging from 0.1 to 0.17 tends to increase with an increase in wind velocity but decrease with an increase in particle size.The force per unit volume exerted on the wind by blown sand drift that is calculated based on the empirical power functions for the wind velocity profiles is found to decrease with height.The particle-induced force makes the total shear stress with blowing sand cloud partitioned into air-borne stress that results from the wind velocity gradient and grain-borne stress that results from the upward or downward movement of particles.The air-borne stress in-creases with an increase in height,while the grain-borne stress decreases with an increase in height.The air-borne shear stress at the top of sand cloud layer increases with both wind velocity and grain size,implying that it increases with sand transport rate for a given grain size.The shear stress with a blowing sand cloud is also closely related to the sand transport rate.Both the total shear stress and grain-borne stress on the grain top is directly proportional to the square root of sand transport rate.So,the profound effect of the moving particles on the airflow must be considered in modeling the blown sand movement.With the presence of sand movement,the boundary layer with a blowing sand cloud is no longer a con-stant air shear layer. | Zhibao Dong*,Hongtao Wang,Guangqiang Qian,Wanyin Luo Key Laboratory of Desert and Desertification,Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Lanzhou,China | 2008 | Research in Cold and Arid Regions2008，，1： | 1 |
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