新的与过去的二氧化硅挤压曲线实验:应用于 Dimorphos 基准冲击模拟

Uri Malamud, Christoph M. Schafer, Irina Luciana San Sebastian, Maximilian Timpe, Karl Alexander Essink, Christopher Kreuzig, Gerwin Meier, Jürgen Blum, Hagai B. Perets, Christoph Burger
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引用次数: 0

摘要

挤压曲线对于小型多孔天体物理体的数值建模具有根本性的重要意义。经验文献通常对二氧化硅晶粒进行测量,不同的研究采用了不同的方法、尺寸、质地和压力条件。在此,我们回顾了过去的研究,并对进一步的实验进行了补充,以便对二氧化硅的挤压曲线行为有一个全面和总体的了解。我们提出了一种新的幂律函数,可用于类似于微颗粒二氧化硅的模拟材料的冲击模拟。我们基于 DART 撞击小行星 Dimorphos 的研究案例,开展了一项基准研究,将这种新的挤压曲线与其他研究中经常使用的参数二次挤压曲线进行比较。我们发现,典型的二次挤压曲线参数并不完全符合硅挤压实验的结果,因此它们对距离撞击地点较近(较远)的挤压情况估计不足(过多)。因此,这里提出的适用于几百帕至 1.1 GPa 压力的新挤压曲线可能更加精确。此外,该曲线没有根据具体情况进行校准,可以普遍用于彗星或类似小行星的天体,假定其成分类似于微粒硅石。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New versus past silica crush curve experiments: application to Dimorphos benchmarking impact simulations
Crush curves are of fundamental importance to numerical modeling of small and porous astrophysical bodies. The empirical literature often measures them for silica grains, and different studies have used various methods, sizes, textures, and pressure conditions. Here we review past studies and supplement further experiments in order to develop a full and overarching understanding of the silica crush curve behavior. We suggest a new power-law function that can be used in impact simulations of analog materials similar to micro-granular silica. We perform a benchmarking study to compare this new crush curve to the parametric quadratic crush curve often used in other studies, based on the study case of the DART impact onto the asteroid Dimorphos. We find that the typical quadratic crush curve parameters do not closely follow the silica crushing experiments, and as a consequence they under (over) estimate compression close (far) from the impact site. The new crush curve presented here, applicable to pressures between a few hundred Pa and up to 1.1 GPa, might therefore be more precise. Additionally, it is not calibrated by case-specific parameters, and can be used universally for comet- or asteroid-like bodies, given an assumed composition similar to micro-granular silica.
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