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Role of collisions in erosion of regolith during a lunar landing

机译:碰撞在月球着陆过程中的作用

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The supersonic gas plume of a landing rocket entrains lunar regolith, which is the layer of loose solids coveringnthe lunar surface. This ejection is problematic due to scouring and dust impregnation of surrounding hardware,nreduction in visibility for the crew, and spoofing of the landing sensors. To date, model predictions of erosionnand ejection dynamics have been based largely on single-trajectory models in which the role of interparticlencollisions is ignored. In the present work, the parameters affecting the erosion rate of monodisperse solids areninvestigated using the discrete element method (DEM). The drag and lift forces exerted by the rocket exhaustnare incorporated via one-way coupling. The results demonstrate that interparticle collisions are frequent in thenregion immediately above the regolith surface; as many as 20% of particles are engaged in a collision at angiven time. These collisions play an important role both in the erosion dynamics and in the final trajectories ofnparticles. In addition, a direct assessment of the influence of collisions on the erosion rate is accomplished via ancomparison between a “collisionless” DEM model and the original DEM model. This comparison shows that thenerosion dynamics change drastically when collisions are considered and that the erosion rate is dependent on thencollision parameters (coefficient of restitution and coefficient of friction). Physical explanations for these trendsnare provided.
机译:着陆火箭的超音速气体羽流带走了月球重灰石,这是覆盖月球表面的疏松固体层。由于周围硬件的擦洗和灰尘浸入,对机组人员的可见度降低以及着陆传感器的欺骗,这种弹出是有问题的。迄今为止,腐蚀和喷射动力学的模型预测主要基于单轨迹模型,其中忽略了粒子间碰撞的作用。在目前的工作中,未使用离散元方法(DEM)研究影响单分散固体侵蚀速率的参数。火箭尾气施加的阻力和升力通过单向耦合作用。结果表明,在重碎石表面正上方的区域中,粒子间碰撞频繁发生。在血管生成时,多达20%的粒子参与了碰撞。这些碰撞在腐蚀动力学和粒子的最终轨迹中都起着重要作用。此外,通过“无碰撞” DEM模型与原始DEM模型之间的比较,可以直接评估碰撞对侵蚀速率的影响。这种比较表明,当考虑到碰撞时,腐蚀动力学会急剧变化,并且腐蚀速率取决于碰撞参数(恢复系数和摩擦系数)。提供了这些趋势的物理解释。

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  • 来源
    《PHYSICAL REVIEW E》 |2013年第2期|1-14|共14页
  • 作者单位

    Department of Chemical and Biological Engineering University of Colorado Boulder Colorado 80303 USA;

    Department of Chemical and Biological Engineering University of Colorado Boulder Colorado 80303 USA;

    NASA Kennedy Space Center Granular Mechanics and Regolith Operations Laboratory Kennedy Space Center Florida 32899 USA;

    Department of Chemical and Biological Engineering University of Colorado Boulder Colorado 80303 USA;

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