The Dimorphos Boulder Swarm

D. Jewitt, Yoonyoung Kim, Jing Li, M. Mutchler
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引用次数: 2

Abstract

We present deep Hubble Space Telescope images taken to examine the ejecta from the DART spacecraft impact into asteroid Dimorphos. The images reveal an extensive population of comoving boulders, the largest of which is ∼7 m in diameter (geometric albedo 0.15 assumed). Measurements of 37 boulders show a mean sky-plane velocity dispersion of 0.30 ± 0.03 m s−1, only slightly larger than the 0.24 m s−1 gravitational escape velocity from the Didymos–Dimorphos binary system. The total boulder mass, M b ∼ 5 × 106 kg (density 2200 kg m−3 assumed), corresponds to about 0.1% of the mass of Dimorphos, and the boulders collectively carry about 3 × 10−5 of the kinetic energy delivered by the DART spacecraft impact. The sky-plane distribution of the boulders is asymmetric, consistent with impact into an inhomogeneous, likely rubble-pile, body. Surface boulder counts on Didymos show that the observed boulder swarm could be ejected from as little as 2% of the surface of Dimorphos (for example, a circular crater at the impact point about 50 m in diameter). The large, slow-moving boulders are potential targets to be investigated in situ by the upcoming ESA HERA mission.
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Dimorphos巨石群
我们展示了深哈勃太空望远镜拍摄的图像,以检查DART航天器撞击小行星Dimorphos的喷出物。图像显示了大量的移动巨石,其中最大的直径约7米(假设几何反照率为0.15)。对37颗巨砾的测量表明,平均天面速度色散为0.30±0.03 m s - 1,仅略大于Didymos-Dimorphos双星系统的引力逃逸速度0.24 m s - 1。巨石的总质量为M b ~ 5 × 106 kg(假设密度为2200 kg M−3),相当于Dimorphos质量的0.1%,这些巨石共同携带了DART航天器撞击所传递的动能的3 × 10−5。这些巨石的平面分布是不对称的,与撞击到一个不均匀的、可能是碎石堆的物体相一致。Didymos上的表面巨石计数显示,观察到的巨石群可以从Dimorphos表面的2%抛射出来(例如,撞击点直径约50米的圆形陨石坑)。这些大而缓慢移动的巨石是即将到来的ESA HERA任务在现场调查的潜在目标。
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