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Numerical simulation of aeolian dusty sand transport in a marginal desert region at the early entrainment stage

机译:夹带初期边缘沙漠地区风沙尘埃运移的数值模拟

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Aeolian dusty sand transport in the marginal region of a desert is described numerically from first suspension motion at the early entrainment stage to the unsteady state within a moderate range (1000 m long × 500 m high). A two-dimensional model is built for wind-blown dust flow, and the calculations are carried out using Fluent software. The simulation results describe an integrated picture of aeolian dusty sand transport including uplift, suspension, diffusion, deposition and its space-time concentration. According to the features of a sand-dust storm near the surface, a volume concentration expression of ejection grains is developed as a boundary condition in the simulation approach. The model is verified by comparing results with both experimental data from a wind tunnel and an analytic solution. Uniform dust sizes and R-R distributions are used in the simulation. Gas-solid two-phase flow patterns with these grains are obtained in the downwind space, including the turbulence intensity, gas phase stream functions and solid volume concentration distributions. The influence of wind velocities and grain sizes is analyzed. From the simulation results, spatial distributions of dust volume concentration in the early entrainment stage are described clearly. Different from coarse sands, there is a clear band of uniformly saturated dust concentration in the region directly above the surface.
机译:用数字描述了沙漠边缘地区的风沙尘埃运输,从早期的夹带运动到中等范围(1000 m长×500 m高)内的不稳定状态。建立了一个用于风吹尘埃流的二维模型,并使用Fluent软件进行了计算。模拟结果描述了风沙尘埃运输的整体情况,包括隆起,悬浮,扩散,沉积及其时空集中。根据地表附近沙尘暴的特点,在模拟方法中建立了喷射颗粒的体积浓度表达式作为边界条件。通过将结果与风洞的实验数据和解析解进行比较,可以验证该模型。模拟中使用统一的粉尘大小和R-R分布。在顺风空间获得了具有这些晶粒的气固两相流型,包括湍流强度,气相流函数和固体体积浓度分布。分析了风速和晶粒尺寸的影响。从模拟结果可以清楚地描述夹带初期粉尘体积浓度的空间分布。与粗砂不同,在表面正上方的区域中存在明显的均匀饱和粉尘浓度带。

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