一盘散落的冰冷物体和木星家族彗星的起源
1Department of Physics, Queen's University, Kingston, Ontario K7L 3N6, Canada. duncan@astro.queensu.ca
概括
模拟显示了海王星之外的物体的分散盘,由早期太阳系动力学形成. 这个磁盘可能是木星家族彗星的来源,包括新发现的物体,如1996 RQ20.
科学领域:
- 行星科学 行星科学
- 计算天体物理学 计算天体物理学
- 太阳系动力学 太阳系动力学
背景情况:
- 柯伊伯带是一个海王星之外的冰冷天体区域.
- 早期的太阳系经历了显著的动态进化.
- 木星家族彗星的起源仍然是一个活跃的研究领域.
研究的目的:
- 为了研究海王星之外的物体分散盘的形成.
- 为了确定这个磁盘是否可能是木星家族彗星的来源.
- 为了确定这个新形成的磁盘的潜在成员.
主要方法:
- 进行了长期轨道整合 (4亿年).
- 模拟模拟了粒子和海王星之间的相互作用.
- 模拟物体的轨道元素被分析并与观察到的物体进行比较.
主要成果:
- 轨道整合产生了海王星之外分散的物体盘.
- 这些物体比柯伊伯带物体表现出更大的偏心和倾斜.
- 大约1%的模拟粒子在这个磁盘中存活了太阳系的年龄.
- 一个有6×10^8个物体的磁盘可以提供观测到的木星家族彗星.
- 1996年RQ20和1996年TL66的物体显示了与预测的圆盘成员的轨道相似性.
结论:
- 模拟的分散盘是太阳系早期进化的可信结果.
- 这个磁盘是木星家族彗星的可行来源.
- 1996 RQ20和1996 TL66是这个分散盘的第一个已识别的成员.
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