高質量プロトスターの周りの塵と分子ガスの円盤
Nimesh A Patel1, Salvador Curiel, T K Sridharan
1Harvard-Smithsonian Center for Astrophysics, 60 Garden Street, MS78, Cambridge, Massachusetts 02138, USA.
Nature
|September 2, 2005
まとめ
高質量恒星形成は,低質量恒星と同様に,増殖によって起こる可能性があります. 観測により,巨大なプロトスターの周りの円盤が明らかになり,巨大な恒星誕生のためのこの蓄積モデルを支持しています.
科学分野:
- 天体物理学 天体物理学
- 恒星の進化について
背景:
- 低質量恒星形成はよく理解されています.
- 高質量恒星形成のメカニズムは未だに十分に理解されていない.
- 星収縮対星合併は,高質量恒星形成における重要な議論である.
研究 の 目的:
- 高質量星の形成過程を調査する.
- 高質量恒星が周周円盤からの蓄積によって形成されているかどうかを判断する.
- 高質量恒星形成における蓄積モデルに賛成または反対の証拠を提供するため.
主な方法:
- 観測天文学は,連続的な塵の放出に焦点を当てている.
- 分子ガスラインの放射を分析する.
- 双極性のジェットの無線観測.
主要な成果:
- 太陽質量15のプロトスターの周りの平らな円盤のような構造の検出.
- 円盤の半径は約330天文学単位,質量は太陽の1~8倍である.
- ディスクは,観測された双極性無線ジェットに垂直して方向づけられています.
結論:
- 高質量恒星は,蓄積によって形成される.
- 観測された円盤構造は,巨大な恒星の形成メカニズムとしての増殖を支えている.
- この発見は,低質量恒星と高質量恒星の形成過程を一致させています.
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