论文标题
盖亚太空任务观察到的玄武岩小行星的光谱分析
Spectral analysis of basaltic asteroids observed by the Gaia space mission
论文作者
论文摘要
在表征玄武岩小行星(频谱归类为V型)方面,有很多科学兴趣,因为它们是理解早期太阳系中行星形成和进化的关键。这些长期以来一直被认为是完全分化的行星的地壳的一部分。因此,它们的多样性,分布和物理特征对于为太阳系的理论演化模型提供背景和约束至关重要。在这项工作中,我们通过ESA Gaia任务数据释放3的频谱测量的扩展数据集执行光谱分析,因此与文献相比,分析V型型的样本量增加了三倍以上。使用GAIA提供的数据,我们确定了〜2000可能的V型小行星。其中约有350个成功地通过了我们的数据验证标准。该样本包括2.5 au以上的31种新型V型小行星和凤凰区的6个。我们确认,与典型的丝绸相比,主皮带中部和外部的V型小行星在主皮带的中部和外部表现出不同的光谱特性。在内部主带中,我们发现所有人群中V型中的光谱参数大量多样性。小行星的数量显示出比(1459)Magnya大的带状深度。此外,某些对象呈现为0.9〜 \ textmu {} m带中心,而不是一个标准偏差,远离符号的典型值。但是,由于DR3频段中心通常被高估了,因此要确认这些发现。总体而言,我们的结果表明,内部主带可能包含多个分化行星的残余物,而不仅仅是(4)Vesta。
There is a great deal of scientific interest in characterizing the basaltic asteroids (spectrally classified as V-types), as they are the key to understanding planetesimal formation and evolution in the early Solar System. These have long been recognized as parts of the crusts of fully differentiated planetesimals. Thus, their multiplicity, distribution, and physical characteristics are crucial for providing context for and constraining the theoretical evolution models of the Solar System. In this work, we perform spectral analysis with an extended data set of spectral measurements from the ESA Gaia mission Data Release 3, thus increasing the sample size of the analyzed V-types by more than three times as compared to the literature. Using the data provided by Gaia we identified ~2000 possible V-type asteroids. About 350 of them successfully pass our data validation criteria. This sample includes 31 new V-type asteroids beyond 2.5 au and 6 in the Phocaea region. We confirm that the V-type asteroids in the middle and outer part of the main belt show distinct spectral properties compared to typical vestoids. In the inner main belt, we found a great diversity of spectral parameters among the V-types in all populations. Number of asteroids show band depths even greater than that of (1459) Magnya. Furthermore, some objects present 0.9~\textmu{}m band-centers more than one standard deviation away from the typical value for vestoids. However since the DR3 band centers are often overestimated, those findings are to be confirmed. Overall our results indicate that the inner main belt may contain remnants of multiple differentiated planetesimals, not just (4) Vesta.