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Azimuthal asymmetries in the debris disk around HD?61005 - A massive collision of planetesimals?

机译:HD周围碎片盘中的方位角不对称?61005-行星小行星的巨大碰撞?

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Context. Debris disks offer valuable insights into the latest stages of circumstellar disk evolution, and can possibly help us to trace the outcomes of planetary formation processes. In the age range 10 to 100?Myr, most of the gas is expected to have been removed from the system, giant planets (if any) must have already been formed, and the formation of terrestrial planets may be on-going. Pluto-sized planetesimals, and their debris released in a collisional cascade, are under their mutual gravitational influence, which may result into non-axisymmetric structures in the debris disk. Aims. High angular resolution observations are required to investigate these effects and constrain the dynamical evolution of debris disks. Furthermore, multi-wavelength observations can provide information about the dust dynamics by probing different grain sizes. Methods. Here we present new VLT/SPHERE and ALMA observations of the debris disk around the 40?Myr-old solar-type star HD?61005. We resolve the disk at unprecedented resolution both in the near-infrared (in scattered and polarized light) and at millimeter wavelengths. We perform a detailed modeling of these observations, including the spectral energy distribution. Results. Thanks to the new observations, we propose a solution for both the radial and azimuthal distribution of the dust grains in the debris disk. We find that the disk has a moderate eccentricity ( e ~ 0.1 ) and that the dust density is two times larger at the pericenter compared to the apocenter. Conclusions. With no giant planets detected in our observations, we investigate alternative explanations besides planet-disk interactions to interpret the inferred disk morphology. We postulate that the morphology of the disk could be the consequence of a massive collision between ~ 1000?km-sized bodies at ~ 61?au. If this interpretation holds, it would put stringent constraints on the formation of massive planetesimals at large distances from the star.
机译:上下文。碎片盘为了解星际盘演化的最新阶段提供了宝贵的见识,并可能有助于我们追踪行星形成过程的结果。在10到100?Myr的年龄范围内,预计大部分气体已从系统中去除,巨型行星(如果有)必须已经形成,并且地球行星的形成可能仍在继续。冥王星大小的小行星及其碎片在碰撞级联中释放,处于相互的重力影响下,这可能导致碎片盘中出现非轴对称结构。目的需要高角度分辨率的观察来研究这些影响并限制碎片盘的动态演化。此外,多波长观测可以通过探测不同的粒度来提供有关尘埃动力学的信息。方法。在这里,我们介绍了40迈尔太阳岁的恒星HD?61005周围碎片盘的新的VLT / SPHERE和ALMA观测结果。我们以前所未有的分辨率在近红外(散射和偏振光)和毫米波长下解析磁盘。我们对这些观测值进行了详细的建模,包括光谱能量分布。结果。由于有了新的观测结果,我们提出了一种解决方案,以解决碎片盘中尘粒的径向分布和方位角分布。我们发现圆盘具有适度的偏心率(e〜0.1),尘埃密度在中心点比中心点大两倍。结论。在我们的观测中未发现巨型行星的情况下,我们将研究除行星-盘相互作用之外的其他解释来解释推断的盘形态。我们假设磁盘的形态可能是在约61?au处约1000?km大小的物体之间发生巨大碰撞的结果。如果这种解释成立,它将对离恒星很远的大质量行星的形成施加严格的限制。

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