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Spin Axes and Shape Models of Asteroid Pairs: Fingerprints of YORP and a Path to the Density of Rubble Piles

机译:小行星对的旋转轴和形状模型:YORp和a的指纹   碎石桩密度的路径

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摘要

An asteroid pair consists of two unbound objects with almost identicalheliocentric orbital elements that were formed when a single "rubble pile"asteroid failed to remain bound against an increasing rotation rate. Modelssuggest that the pairs' progenitors gained the fast rotation due to the YORPeffect. Since it was shown that the spin axis vector can be aligned by the YORPeffect, such a behavior should be seen on asteroid pairs, if they were indeedformed by the described mechanism. Alternatively, if the pairs were formed by acollision, the spin axes should have a random direction and small or youngbodies might have a tumbling rotation. Here I apply the lightcurve inversion method on self-obtained photometricdata, in order to derive the rotation axis vectors and shape models of theasteroid pairs 2110, 3749, 5026, 6070, 7343 and 44612. Three asteroids resultedwith polar-directed spin axes and three objects with ambiguous results. Inaddition, the secondary member 44612 presents the same sense of rotation as itsprimary member 2110, and its spin is not tumbling. Finally, I use a rotationalfission model, based on the assumption of an angular momentum conservation, andmatch it to the measured spin, shape, and mass ratio parameters in order toconstrain the density of the primary members in the pairs. Using this method,low density values that are expected from a "rubble pile" are derived. Allthese results lead to the conclusion that the disruption of these asteroidpairs was most likely the outcome of the YORP effect that spun-up "rubble pile"asteroids.
机译:一对小行星由两个未结合的物体组成,它们具有几乎相同的太阳心轨道元素,这是在单个“碎石堆”小行星未能保持增加的旋转速度时形成的。模型表明,由于YORP效应,两对祖先获得了快速旋转。由于已经证明自旋轴矢量可以通过YORP效应进行对齐,因此,如果它们确实是由所描述的机制形成的,则应该在小行星对上观察到这种行为。或者,如果这些对是通过碰撞形成的,则自旋轴应具有随机方向,小的或年轻的物体可能会旋转。在这里,我对自获取的光度数据应用了光曲线反演方法,以导出小行星对2110、3749、5026、6070、7343和44612的旋转轴矢量和形状模型。产生了三个小行星,它们具有极向旋转轴和三个对象结果不明确。另外,次要构件44612呈现出与其主要构件2110相同的旋转感,并且其自旋不翻滚。最后,基于角动量守恒的假设,我使用了旋转裂变模型,并将其与测得的自旋,形状和质量比参数进行匹配,以约束成对的主要成员的密度。使用此方法,可以得出“碎石堆”所期望的低密度值。所有这些结果得出这样的结论:这些小行星对的破坏很可能是旋转“瓦砾堆”小行星的YORP效应的结果。

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  • 作者

    Polishook, David;

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  • 年度 2014
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  • 原文格式 PDF
  • 正文语种 {"code":"en","name":"English","id":9}
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