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arXiv 2111.06372astro-ph.EP
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类月硅酸盐物质形成地球准卫星(469219)2016 HO3 Kamo`oalewa

Lunar-like silicate material forms the Earth quasisatellite (469219) 2016 HO3 Kamo`oalewa

Benjamin N. L. Sharkey, Vishnu Reddy, Renu Malhotra, Audrey Thirouin, Olga Kuhn, Albert Conrad, Barry Rothberg, Juan A. Sanchez, David Thompson, Christian Veillet

摘要:

人们对地球准卫星知之甚少,这是一类近地小太阳系天体,它们绕太阳运行,但仍然靠近地球,因为它们很微弱,难以观测。在这里,我们使用大型双目望远镜和洛厄尔发现望远镜对准卫星(469219)Kamo`oalewa进行全面的物理表征,并评估其与其他近地天体组的相似性。我们发现(469219)Kamo`oalewa的自转周期为28.3(+1.8/-1.3)分钟,并显示出0.4-2.2微米的变红反射光谱。这一光谱显示了硅酸盐基的成分,但其变红程度超出了太阳系内小行星的典型特征。我们比较光谱的几种材料的类似物,并得出结论,最好的匹配是与月球状硅酸盐。这种解释意味着广泛的空间风化,并提出了Kamo`oalewa可能包含月球物质的前景。

英文摘要:

Little is known about Earth quasi-satellites, a class of near-Earth small solar system bodies that orbit the sun but remain close to the Earth, because they are faint and difficult to observe. Here we use the Large Binocular Telescope (LBT) and the Lowell Discovery Telescope (LDT) to conduct a comprehensive physical characterization of quasi-satellite (469219) Kamo`oalewa and assess its affinity with other groups of near-Earth objects. We find that (469219) Kamo`oalewa rotates with a period of 28.3 (+1.8/-1.3) minutes and displays a reddened reflectance spectrum from 0.4-2.2 microns. This spectrum is indicative of a silicate-based composition, but with reddening beyond what is typically seen amongst asteroids in the inner solar system. We compare the spectrum to those of several material analogs and conclude that the best match is with lunar-like silicates. This interpretation implies extensive space weathering and raises the prospect that Kamo`oalewa could comprise lunar material.

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