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Calculation of Dust Lifting by a Transient Shock Wave

机译:瞬态冲击波扬尘的计算

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摘要

A mathematical model of lifting of dust particles under the action of transient shock waves is proposed, which takes into account a simultaneous action of the Saffman force and aerodynamic interference on the particle. This model provides an adequate description of the initial stage of lifting of single particles of a dusty layer under the action of shock waves of weak and moderate strength. Satisfactory agreement of numerical and experimental data is reached. It is shown that particle lifting is caused by the action of the Saffman force in the case of weak shock waves (the shock-wave Mach number is less than 1.5) and medium-sized particles (the particle diameter is less than 100 mum) and aerodynamic interference between the particle and the surface in the case of shock waves of moderate strength (the shock-wave Mach number is 2.1-3.3) and large particles (the particle diameter is 200-250 mum).
机译:提出了一种在瞬变冲击波作用下扬尘的数学模型,该模型考虑了萨夫曼力和空气动力对微粒的同时作用。该模型充分说明了在强度中等强度的冲击波作用下,尘土层中单个颗粒的抬起的初始阶段。数值和实验数据令人满意。结果表明,在弱冲击波(冲击波马赫数小于1.5)和中型粒子(粒径小于100微米)的情况下,由于Saffman力的作用引起了颗粒的提升。在中等强度的冲击波(冲击波马赫数为2.1-3.3)和大颗粒(粒径为200-250微米)的情况下,颗粒与表面之间存在空气动力干扰。

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