(65803) Didymos 的异常亮度相位曲线

IF 3.8 Q2 ASTRONOMY & ASTROPHYSICS
P. H. Hasselmann, V. Della Corte, P. Pravec, S. Ieva, I. Gai, D. Perna, J. D. P. Deshapriya, E. Mazzotta-Epifani, E. Dotto, A. Zinzi, G. Poggiali, I. Bertini, A. Lucchetti, M. Pajola, J. Beccarelli, M. Dall’Ora, J.-Y. Li, S. L. Ivanovski, A. Rossi, J. R. Brucato, C. A. Thomas, O. Barnouin, J. M. Sunshine, A. S. Rivkin, M. Amoroso, A. Capannolo, S. Caporali, M. Ceresoli, G. Cremonese, R. T. Daly, G. Impresario, R. Lasagni-Manghi, M. Lavagna, D. Modenini, E. E. Palmer, P. Palumbo, S. Pirrotta, P. Tortora, M. Zannoni, G. Zanotti
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引用次数: 0

摘要

2022年9月26日,NASA的双小行星重定向试验(DART)成功撞击了与小行星(65803)Didymos形成的双星系统中较小的伴星Dimorphos。双小行星系统和撞击事件都由意大利小行星成像轻立方体卫星(Light Italian Cubesat for Imaging of Asteroids)进行了成像,该卫星在撞击发生前 15 天脱离了 DART。星载 LUKE 红、绿、蓝照相机拍摄的图像与地面观测数据相结合,重建了狄迪莫斯的亮度相位曲线,相位角从 2.35°到 107.7°不等。利用指数-线性方程、"舍甫琴科 "函数和逐部分线性模型对对冲效应机制进行了研究,同时将国际天文学联合会官方的 HG1G2 星等系统应用于完整的相位曲线。对立效应表明这颗 S 型小行星的表面很不寻常,具有类似于 M 型小行星的特征。而根据全相位曲线得出的 HG1G2 参数,迪迪莫斯在分类学上属于 C 型小行星。与近地小行星相比,迪迪莫斯的相位曲线参数非常接近于 Q 型(1862 年)阿波罗小行星,这表明亚微米级的细小颗粒可能在重铸过程中损耗殆尽。据报道,迪迪莫斯的几何反照率(0.15 ± 0.01)比近地 S 型小行星的平均几何反照率(0.26 ± 0.04)小 30%-45%。我们认为,迪迪莫斯可能是一种低地普通金刚石类似物,其中含有抑制反照率的冲击暗化/撞击熔融矿物,这些矿物在过去经历了重铺过程。与陨石的比较表明,迪迪莫斯也可能含有类似于含碳角砾化 L3 普通软玉的物质,但这种可能性较小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Unusual Brightness Phase Curve of (65803) Didymos
On 2022 September 26, NASA's Double Asteroid Redirection Test (DART) successfully hit Dimorphos, the smaller companion of the binary system formed with the asteroid (65803) Didymos. Both the binary system and the impact event were imaged by the Light Italian Cubesat for Imaging of Asteroids, detached from DART 15 days before the impact. Images from the onboard LUKE red, green, and blue camera together with ground-based observations enabled the reconstruction of Didymos's brightness phase curve, with phase angles ranging from 2.35° to 107.7°. The opposition effect regime was studied using the exponential-linear equation, the “Shevchenko” function and the linear-by-parts model while the IAU-official HG1G2 magnitude system was applied to the full phase curve. The opposition effect indicates an unusual asteroid surface for an S type, with characteristics similar to M-type asteroids. While the HG1G2 parameters from the full phase curve place Didymos well among asteroids of the taxonomic C complex. Didymos’s phase curve parameters when compared to near-Earth asteroids are very close to the Q type (1862) Apollo, indicating possible depletion of fine submicrometric grains through resurfacing. Didymos's geometric albedo (0.15 ± 0.01) is reported to be 30%–45% smaller than the average geometric albedo for near-Earth S types (0.26 ± 0.04). We propose that Didymos might be an LL ordinary chondrite analog containing albedo-suppressing, shock-darkened/impact melt minerals that have undergone resurfacing processes in the past. A comparison with meteorites indicates that, less likely, Didymos could also contain materials analog to carbon-bearing brecciated L3 ordinary chondrites.
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来源期刊
The Planetary Science Journal
The Planetary Science Journal Earth and Planetary Sciences-Geophysics
CiteScore
5.20
自引率
0.00%
发文量
249
审稿时长
15 weeks
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