论文标题

使用Murchison Widefield阵列射电望远镜进行分解事件及其表征引起的轨道碎片云的模拟

Simulations of orbital debris clouds due to breakup events and their characterisation using the Murchison Widefield Array radio telescope

论文作者

Joubert, Wynand, Tingay, Steven

论文摘要

在本文中,我们考虑使用广泛的视野雷达传感器,例如默奇森广场阵列(MWA),这是一种用于天体物理学和宇宙学设计的低频射电望远镜,用于对地球轨道对象之间碰撞产生的碎屑云的快速响应观察。在低地球轨道中的物体密度越来越大,包括数十年来天文学界使用的遗产资产,形成新的碎屑云的风险也在增加。 MWA构成了广泛的磁场,快速响应被动雷达系统,我们探索了其在碎屑云的检测和表征中的可能性能。通常,MWA等天文学设施可以在保护未来的太空环境中发挥作用。为了进行这项工作,我们使用进化输出来生成代表性的动态碎片云,使NASA Evolve 4.0分解模型适应4.0分解模型。我们发现,如果MWA可以接近最佳检测敏感性,则MWA可能会检测出大量的建模碎屑云碎片,用于在LEO下部的100 kg至1000 kg的碰撞块中,用于100 kg至1000 kg。对于更保守的假设,仍然可以实现有用的检测部分。碎片的检测部分随着高度的函数而降低,并且与碰撞质量相反。令人鼓舞的是,我们发现MWA的宽阔田地性质允许在单个观察结果中观察到完整的不断发展的碎屑云,只有$ \ sim2 \%$的碎屑片段,逃脱了100秒后的视野敏感部分,用于所有碰撞群体和高度。这些结果表明,MWA是用于快速表征碎片云的本质上有用的设施,但是需要这项工作才能在适当的时间范围内实现数据处理以提供快速警报。

In this paper we consider the use of wide field of view radar sensors such as the Murchison Widefield Array (MWA), a low frequency radio telescope designed for astrophysics and cosmology, for rapid response observations of the debris clouds produced by collisions between objects in Earth orbit. With an increasing density of objects in Low Earth Orbit, including legacy assets used by the astronomy community over decades, the risk of new debris clouds forming is also increasing. The MWA constitutes a wide field, rapid response passive radar system and we explore its likely performance in the detection and characterisation of debris clouds. In general, astronomy facilities such as the MWA can play a role in protecting the space environment for the future. In order to undertake this work, we adapt the NASA EVOLVE 4.0 breakup model, utilising the EVOLVE outputs to produce representative dynamic debris clouds. We find that the MWA is likely to detect a large fraction (>70%) of modelled debris cloud fragments for collision masses between 100 kg and 1000 kg for orbits in the lower part of LEO, if the MWA can achieve close to optimal detection sensitivity. Useful detection fractions are still achieved for more conservative assumptions. The detection fraction of fragments decreases as a function of altitude and inversely with collision mass. Encouragingly, we find that the wide field nature of the MWA allows the full evolving debris clouds to be observed in a single observation, with only $\sim2\%$ of the debris fragments escaping the sensitive portion of the field of view after 100 seconds, for all collision masses and altitudes. These results show that the MWA is an intrinsically useful facility for the rapid characterisation of debris clouds, but that work is required to achieve the data processing within an appropriate timeframe to provide rapid alerts.

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