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首页> 外文期刊>The Astrophysical journal >TIDAL TAILS OF MINOR MERGERS. II. COMPARING STAR FORMATION IN THE TIDAL TAILS OF NGC?2782*
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TIDAL TAILS OF MINOR MERGERS. II. COMPARING STAR FORMATION IN THE TIDAL TAILS OF NGC?2782*

机译:小合并的潮汐尾巴。二。 NGC?2782潮汐尾中的恒星形成比较*

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摘要

The peculiar spiral NGC?2782 is the result of a minor merger with a mass ratio ~4: 1 occurring ~200?Myr ago. This merger produced a molecular and H I-rich, optically bright eastern tail and an H I-rich, optically faint western tail. Non-detection of CO in the western tail by Braine et al. suggested that star formation had not yet begun. However, deep UBVR and Hα narrowband images show evidence of recent star formation in the western tail, though it lacks massive star clusters and cluster complexes. Using Herschel PACS spectroscopy, we discover 158 μm [C II] emission at the location of the three most luminous Hα sources in the eastern tail, but not at the location of the even brighter Hα source in the western tail. The western tail is found to have a normal star formation efficiency (SFE), but the eastern tail has a low SFE. The lack of CO and [C II] emission suggests that the western tail H II region may have a low carbon abundance and be undergoing its first star formation. The western tail is more efficient at forming stars, but lacks massive clusters. We propose that the low SFE in the eastern tail may be due to its formation as a splash region where gas heating is important even though it has sufficient molecular and neutral gas to make massive star clusters. The western tail, which has lower gas surface density and does not form high-mass star clusters, is a tidally formed region where gravitational compression likely enhances star formation.
机译:奇怪的螺旋状NGC?2782是微小合并的结果,质量比〜4:1发生在200年前。这次合并产生了富含分子和H I的,光学上明亮的东部尾巴,以及富含H I的,光学上模糊的西部尾巴。 Braine等人未在西尾中检测到CO。这表明恒星形成尚未开始。然而,深层UBVR和Hα窄带图像显示出最近在西尾形成恒星的证据,尽管它缺乏大量的恒星团和团簇复合体。使用Herschel PACS光谱法,我们在东部尾部的三个最发光的Hα源位置发现了158μm[C II]发射,而在西部尾部的甚至更亮的Hα源位置没有发现。发现西尾具有正常的恒星形成效率(SFE),但东尾具有较低的恒星形成效率。缺乏CO和[C II]排放表明,西部尾部H II区的碳含量可能较低,并且正在经历首次恒星形成。西尾在形成恒星方面效率更高,但缺乏大量星团。我们认为,东部尾部的低SFE可能是由于其形成了一个飞溅区域,在该飞溅区域中,尽管它具有足够的分子和中性气体以形成庞大的星团,但气体加热仍然很重要。西尾巴具有较低的气体表面密度,并且不形成高质量的星团,是潮汐形成的区域,重力压缩可能会增强恒星的形成。

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