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Morphology of craters generated by hypervelocity impacts of micron-sized polypyrrole-coated olivine particles

机译:由微米级聚吡咯涂层橄榄石颗粒的超高速撞击产生的陨石坑的形态

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摘要

To understand the process of cosmic dust particle impacts and translate crater morphology on smoothed metallic surfaces to dust properties, correct calibration of the experimental impact data is needed. This article presents the results of studies of crater morphology generated by impacts using micron-sized polypyrrole (PPy)-coated olivine particles. The particles were accelerated by an electrostatic dust accelerator to high speeds before they impacted onto polished aluminum targets. The projectile diameter and velocity ranges were 0.3-1.2 mu m and 3-7 km s(-1). After impact, stereopair images of the craters were taken using scanning electron microscope and 3-D reconstructions made to provide diameter and depth measurements. In this study, not just the dimensions of crater diameters and depths, but also the shape and dimensions of crater lips were analyzed. The craters created by the coated olivine projectiles are shown to have complicated shapes believed to be due to the nonspherical shape of the projectiles.
机译:为了了解宇宙尘埃粒子撞击的过程并将平滑金属表面上的坑口形态转化为尘埃特性,需要对实验撞击数据进行正确的校准。本文介绍了使用微米级聚吡咯(PPy)涂层橄榄石颗粒通过撞击产生的火山口形态的研究结果。在将粒子撞击到抛光的铝靶上之前,将其通过静电除尘器加速至高速。弹丸直径和速度范围为0.3-1.2微米和3-7公里s(-1)。撞击后,使用扫描电子显微镜拍摄陨石坑的立体对图像,并进行3-D重建以提供直径和深度测量值。在这项研究中,不仅分析了火山口直径和深度的尺寸,而且分析了火山口唇的形状和尺寸。由涂层的橄榄石弹丸产生的弹坑显示出复杂的形状,据信这是由于弹丸的非球形形状所致。

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