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arXiv 1102.3416cond-mat.softphysics.geo-ph
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液滴撞击和穿透颗粒层的长度和时间尺度

Length and time scales of a liquid drop impact and penetration into a granular layer

Hiroaki Katsuragi

摘要:

采用不同的液体和颗粒材料,研究了液滴对颗粒层的冲击和穿透。我们使用各种尺寸的SiC磨料和玻璃珠作为目标颗粒材料。我们还使用乙醇和甘油水溶液以及蒸馏水来制备液滴。液滴以低速(~ m/s)撞击颗粒层。液滴变形和穿透由高速摄像机捕捉。根据视频数据,测量特征时间尺度。使用激光轮廓测量系统,由此产生的火山口的形态和其特征长度尺度进行测量。还通过慢柱贯入实验测量颗粒层的静态强度,以量化cohesion内聚力效应。我们发现,时间尺度几乎是独立的冲击速度,但它们依赖于液滴粘度。特别地,渗透时间与液滴粘度的平方根成比例。相反,凹坑半径与液滴粘度无关。陨石坑半径的比例与前一篇论文相同(Katsuragi,Phys. Rev. Lett.第104卷,2010,第218001页)。

英文摘要:

Liquid drop impact and penetration into a granular layer are investigated with diverse liquids and granular materials. We use various size of SiC abrasives and glass beads as a target granular material. We also employ ethanol and glycerol aqueous solutions as well as distilled water to make a liquid drop. The liquid drop impacts the granular layer with a low speed (~ m/s). The drop deformation and penetration are captured by a high speed camera. From the video data, characteristic time scales are measured. Using a laser profilometry system, resultant crater morphology and its characteristic length scales are measured. Static strength of the granular layer is also measured by the slow pillar penetration experiment to quantify the cohesive force effect. We find that the time scales are almost independent of impact speed, but they depend on liquid drop viscosity. Particularly, the penetration time is proportional to the square root of the liquid drop viscosity. Contrastively, the crater radius is independent of the liquid drop viscosity. The crater radius is scaled by the same form as the previous paper, (Katsuragi, Phys. Rev. Lett. vol. 104, 2010, p. 218001).

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