在乱的环恒星盘中快速形成的小行星
Anders Johansen1, Jeffrey S Oishi, Mordecai-Mark Mac Low
1Max-Planck-Institut für Astronomie, Königstuhl 17, D-69117 Heidelberg, Germany. johansen@mpia.de
Nature
|August 31, 2007
概括
行星的形成是由巨石有效地在环恒星盘内引力崩而解释的. 这一过程克服了巨石粘结和气体阻力所带来的挑战,迅速形成行星状物.
科学领域:
- 行星科学 行星科学
- 天体物理学 天体物理学
- 计算流体动力学的流体动力学.
背景情况:
- 行星的形成涉及环恒星盘中的尘埃粒的积累.
- 从米尺寸的巨石成长为千米尺寸的行星体是一个关键的挑战.
- 岩石面临着糟糕的粘合和由于气体逆风而向内漂移.
研究的目的:
- 研究巨石到行星小转变的机制.
- 确定在乱的原行星盘中是否可能发生引力崩.
- 确定快速行星小行星形成的途径.
主要方法:
- 在流气体盘中模拟了岩石的重力崩.
- 在高压区域分析固体度.
- 研究了流动不稳定性在增强固体密度中的作用.
主要成果:
- 岩石在过密的磁盘区域中有效地经历引力崩.
- 度被气体固体流动的不稳定性放大.
- 形成了具有矮行星质量和不同巨石大小的引力绑定的星团.
- 崩发生的速度比辐射漂移更快.
结论:
- 过密地区的重力崩为小行星形成提供了一个可行的机制.
- 这个过程绕过了巨石粘接和气体阻力所带来的局限性.
- 提供了一个解决方案,以快速形成的行星在增长的磁盘.
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