论文标题
M型小行星在其表面组成的背景下的极化
Polarimetry of M-type asteroids in the context of their surface composition
论文作者
论文摘要
目标。我们旨在调查偏光观测如何改善我们对M/X型小行星的性质和多样性的理解。方法。在夏威夷Haleakala天文台的Tohoku 0.6-m望远镜(同时在BVR过滤器中同时),在Rozhen(R Filtery In 2.15-Mims compenter)和2.15-Mmims compeconem和Teliosecone Mimimemimecope(在BVR过滤器中),在夏威夷的Haleakala天文台(同时在BVR过滤器中同时)在Tohoku 0.6米望远镜(在BVR过滤器中同时)对所选的M/X型小行星进行了极化观察。 leoncito(Casleo),阿根廷(在V滤波器中)。我们分析了M/X型小行星的偏振特性以及其他技术获得的可用数据。结果。 22 m/x型小行星与已发表的观测值结合的新的极化观测值提供了41个小行星的数据集,为负极分支和/或反转角的深度确定了该小行星的深度。我们发现,负极分支的深度倾向于随着近红外光谱的陡度而增加。具有较深的负极分支的小行星倾向于具有较高的雷达圆极化比。我们表明,基于负极分支和反转角的深度的关系,可以在M型小行星之间区分两个主要的子类型。我们建议这些组可能与类似于(1)熨斗和石质 - 艾隆以及(2)enstatite和富含铁的碳质软管相似的不同表面组成有关。
Aims. We aim to investigate how polarimetric observations can improve our understanding of the nature and diversity of M/X-type asteroids. Methods. Polarimetric observations of the selected M/X-type asteroids were carried out at the Tohoku 0.6-m telescope at Haleakala Observatory, Hawaii (simultaneously in BVR filters), the 2-m telescope of the Bulgarian National Astronomical Observatory in Rozhen (in R filter), and the 2.15-m telescope of the Complejo Astronómico El Leoncito (CASLEO), Argentina (in V filter). We analysed the polarimetric characteristics of M/X-type asteroids along with the available data obtained by other techniques. Results. New polarimetric observations of 22 M/X-type asteroids combined with published observations provide a data set of 41 asteroids for which the depth of a negative polarisation branch and/or inversion angle were determined. We found that the depth of the negative polarisation branch tends to increase with decreasing steepness of the near-infrared spectra. Asteroids with a deeper negative polarisation branch tend to have a higher radar circular polarisation ratio. We show that, based on the relationship of the depth of the negative polarisation branch and inversion angle, two main sub-types can be distinguished among M-type asteroids. We suggest that these groups may be related to different surface compositions similar to (1) irons and stony-irons and (2) enstatite and iron-rich carbonaceous chondrites.