YORP Effect on Asteroid 162173 Ryugu: Implications for the Dynamical History

YORP Effect on Asteroid 162173 Ryugu: Implications for the Dynamical History
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YORP 对小行星 162173 Ryugu 的影响:对动力学历史的影响

DOI:
10.1029/2021je006863
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发表时间:
2021
期刊:
Journal of Geophysical Research: Planets
影响因子:
--
通讯作者:
Watanabe Sei‐ichiro
Watanabe Sei‐ichiro
中科院分区:
--
文献类型:
--
作者:
Kanamaru Masanori;Sasaki Sho;Morota Tomokatsu;Cho Yuichiro;Tatsumi Eri;Hirabayashi Masatoshi;Hirata Naru;Senshu Hiroki;Shimaki Yuri;Sakatani Naoya;Tanaka Satoshi;Okada Tatsuaki;Usui Tomohiro;Sugita Seiji;Watanabe Sei‐ichiro

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小行星162173 Ryugu是一颗碳质小行星,日本的Hayabusa 2航天器于2018年访问了它。Ryugu“旋转陀螺”形状的形成机制是近地小行星动力学历史的重要线索。在这项研究中,我们解决了由Yarkovsky-O 'Keefe-Radzievskii-Paddack(YORP)效应引起的其自旋状态的长期演化,即改变旋转周期和自旋极方向的热反冲力矩。考虑到Hayabusa 2观测到的Ryugu的当前轨道,自旋状态和三维形状,我们使用假设零热导率的简化热模型计算了施加在Ryugu上的YORP扭矩。尽管米级地形变化,我们检查的所有20个形状模型都表明,Ryugu的自旋速度目前正在以度/天2的速度下降。我们的研究结果还表明,热扭矩是负责保持自旋极垂直相对于轨道平面。因此,YORP效应可以解释从早期的3.5小时到目前的7.6小时的显著旋转下降。根据输入形状模型,自旋下降的相应时间尺度估计为58 - 870万年。这个时间尺度与最大的陨石坑浦岛(5-12 Ma)或西部隆起(2-9 Ma)的形成时间相当,这是根据先前对龙谷陨石坑统计的研究得出的。因此,它的旋转可能已经开始减速,作为一个重大的重铺事件的结果。
Asteroid 162173 Ryugu is a carbonaceous asteroid that was visited by Japan's Hayabusa2 spacecraft in 2018. The formation mechanism of the “spinning‐top” shape of Ryugu is a vital clue to the dynamical history of the near‐Earth asteroid. In this study, we address the long‐term evolution of its spin state induced by the Yarkovsky‐O’Keefe‐Radzievskii‐Paddack (YORP) effect, that is, the thermal recoil torque that changes the rotation period and spin‐pole direction. Given the current orbit, spin state, and three‐dimensional shape of Ryugu observed by Hayabusa2, we computed the YORP torque exerted on Ryugu using a simplified thermal model assuming zero thermal conductivity. Despite variations in the meter‐scaled topography, all 20 shape models that we examined indicate that the spin velocity of Ryugu is currently decreasing at a rate of deg/day2. Our findings also suggest that the thermal torque is responsible for maintaining the spin pole upright with respect to the orbital plane. Therefore, the YORP effect may explain the significant spin‐down from an earlier period of 3.5 hr to the present period of 7.6 hr. The corresponding time scale of the spin‐down is estimated to be 0.58–8.7 million years, depending on the input shape models. This time scale is comparable to the formation period of the largest crater,Urashima(5–12 Ma), or the western bulge (2–9 Ma) as derived from previous studies on crater statistics in Ryugu. Thus, its rotation may have started to decelerate as a consequence of major resurfacing events.
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影响因子: 6.5
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发表时间: 2019-03-01
影响因子: 5.3
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