JWST 对露西木星特洛伊飞越目标的近红外光谱分析:羟基吸收、脂肪族有机物和二氧化碳的证据

IF 3.8 Q2 ASTRONOMY & ASTROPHYSICS
Ian Wong, Michael E. Brown, Joshua P. Emery, Richard P. Binzel, William M. Grundy, Simone Marchi, Audrey C. Martin, Keith S. Noll, Jessica M. Sunshine
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引用次数: 0

摘要

我们将介绍利用 JWST 上的近红外摄谱仪对露西号航天器将访问的五颗木星三剑星--帕特洛克罗斯-梅诺埃提乌斯双星、欧里贝茨、奥鲁斯、勒库斯和波里梅勒--进行的观测。测量到的 1.7-5.3 μm 反射光谱的波长覆盖范围、空间分辨率和信噪比都比以前的地基光谱技术有所提高,揭示了几个明显的吸收特征。我们探测到一个以 3 μm 波长为中心的宽泛 OH 波段,该波段在低红色天体 Eurybates、Patroclus-Menoetius 和 Polymele 上最为突出。在红色天体 Orus 和 Leucus 上,3.3-3.6 μm 处有一个额外的吸收特征,表明是脂肪族有机物的吸收。碰撞碎片 Eurybates 的独特之处在于它在 4.25 μm 处显示了一个吸收带,我们将其归因于束缚或捕获的二氧化碳。与太阳系其他小天体的比较显示,在 2.7-3.6 μm 波段上,半人马、柯伊伯带天体(KBOs)和活动小行星 238P 上的类似特征具有广泛的相似性。最近的太阳系演化模型认为三体星最初是在外太阳系形成的,因此三体星上的 2.7-3.6 μm 吸收特征相对于柯伊伯带天体的显著衰减,可能是三体星表面在木星区域较高温度下进行二次热处理的结果。在欧律贝特星表面出现的二氧化碳波段表明,二氧化碳可能是三体星主体成分中的一种主要成分,但它存在于地表下或更深的内部,在很大程度上被三体星向内迁移过程中激活的热物理过程所形成的难熔物质所掩盖。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
JWST Near-infrared Spectroscopy of the Lucy Jupiter Trojan Flyby Targets: Evidence for OH Absorption, Aliphatic Organics, and CO2
We present observations obtained with the Near Infrared Spectrograph on JWST of the five Jupiter Trojans that will be visited by the Lucy spacecraft—the Patroclus–Menoetius binary, Eurybates, Orus, Leucus, and Polymele. The measured 1.7–5.3 μm reflectance spectra, which provide increased wavelength coverage, spatial resolution, and signal-to-noise ratio over previous ground-based spectroscopy, reveal several distinct absorption features. We detect a broad OH band centered at 3 μm that is most prominent on the less-red objects Eurybates, Patroclus–Menoetius, and Polymele. An additional absorption feature at 3.3–3.6 μm, indicative of aliphatic organics, is systematically deeper on the red objects Orus and Leucus. The collisional fragment Eurybates is unique in displaying an absorption band at 4.25 μm that we attribute to bound or trapped CO2. Comparisons with other solar system small bodies reveal broad similarities in the 2.7–3.6 μm bands with analogous features on Centaurs, Kuiper Belt objects (KBOs), and the active asteroid 238P. In the context of recent solar system evolution models, which posit that the Trojans initially formed in the outer solar system, the significant attenuation of the 2.7–3.6 μm absorption features on Trojans relative to KBOs may be the result of secondary thermal processing of the Trojans’ surfaces at the higher temperatures of the Jupiter region. The CO2 band manifested on the surface of Eurybates suggests that CO2 may be a major constituent in the bulk composition of Trojans, but resides in the subsurface or deeper interior and is largely obscured by refractory material that formed from the thermophysical processes that were activated during their inward migration.
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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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