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3D numerical simulation of the evolutionary process of aeolian downsized crescent-shaped dunes

机译:风沙降新月形沙丘演化过程的3D数值模拟

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A dune constitutive model was coupled with a large eddy simulation (LES) with the Smagorinsky subgrid-scale (SGS) model to accurately describe the evolutionary process of dunes from the macroscopic perspective of morphological dynamics. A 3D numerical simulation of the evolution of aeolian downsized crescent-shaped dunes was then performed. The evolution of the 3D structure of Gaussian-shaped dunes was simulated under the influence of gravity modulation, which was the same with the vertical oscillation of the sand bed to adjust the threshold of sand grain liftoff in wind tunnel experiments under the same wind speed. The influence of gravity modulation intensity on the characteristic scale parameter of the dune was discussed. Results indicated that the crescent shape of the dune was reproduced with the action of gravity during regulation of the saturation of wind-sand flow at specific times. The crescent shape was not dynamically maintained as time passed, and the dunes dwindled until they reached final decomposition because of wind erosion. The height of the dunes decreased over time, and the height time curve converged as the intensity of modulation increased linearly. The results qualitatively agreed with those obtained from wind tunnel experiments. (C) 2016 Elsevier B.V. All rights reserved.
机译:沙丘本构模型与Smagorinsky子网格规模(SGS)模型的大涡模拟(LES)结合使用,可以从宏观形态动力学角度准确描述沙丘的演化过程。然后进行了风沙缩小的新月形沙丘演化的3D数值模拟。在重力调制的影响下,模拟了高斯形沙丘的3D结构的演化,该变化与沙床的垂直振动相同,以在相同风速下调整风洞实验中沙粒抬升的阈值。讨论了重力调制强度对沙丘特征尺度参数的影响。结果表明,沙丘的月牙形是在特定时间调节风沙流饱和度时在重力作用下复制的。随着时间的流逝,新月形的形状并没有得到动态保持,沙丘逐渐缩小,直到由于风蚀而最终分解为止。沙丘的高度随时间下降,并且高度时间曲线随着调制强度线性增加而收敛。该结果在质量上与风洞实验获得的结果一致。 (C)2016 Elsevier B.V.保留所有权利。

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