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arXiv 0908.2432astro-ph.SR
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测量渐近巨分支尖端的质量损失演化

Measuring The Mass Loss Evolution at The Tip of The Asymptotic Giant Branch

C. Sandin, M. M. Roth, D. Schönberner

摘要:

在恒星演化的最后阶段,中低质量恒星在质量越来越大的恒星风中失去了它们的外壳。这种风影响了星际介质和银河系的化学演化,以及行星状星云形成的星周包层。这种质量损失的特征取决于恒星的性质和风形成区的气体和尘埃的性质。在本文中,我们提出了一种方法对使用的观测和模型的质量损失的研究,专注于恒星的信封几乎空的质量的阶段。在最近的一项研究中,我们测量了银河系盘中四个行星状星云的质量损失演化和其他性质。具体来说,我们使用积分场光谱的方法对微弱的晕,这是发现外面的明亮的中心部分的行星状星云。我们首先简要比较我们和其他观测方法来确定质量损失率,以说明它们之间的差异和互补。我们的方法的一个优点是,它直接测量气体成分,不需要假设风中灰尘的性质。此后,我们提出了我们的观察方法,在其有效性和假设方面更详细。在本文的第二部分中,我们讨论了当前恒星风模型的能力和假设。我们提出并讨论了这些模型的改进,这将使我们的观察有意义的比较。目前,物理上最完整的模型包括太少的质量在模型域允许风的形成与我们的观察显示的高质量损失率。

英文摘要:

In the final stages of stellar evolution low- to intermediate-mass stars lose their envelope in increasingly massive stellar winds. Such winds affect the interstellar medium and the galactic chemical evolution as well as the circumstellar envelope where planetary nebulae form subsequently. Characteristics of this mass loss depend on both stellar properties and properties of gas and dust in the wind formation region. In this paper we present an approach towards studies of mass loss using both observations and models, focusing on the stage where the stellar envelope is nearly empty of mass. In a recent study we measure the mass-loss evolution, and other properties, of four planetary nebulae in the Galactic Disk. Specifically we use the method of integral field spectroscopy on faint halos, which are found outside the much brighter central parts of a planetary nebula. We begin with a brief comparison between our and other observational methods to determine mass-loss rates in order to illustrate how they differ and complement each other. An advantage of our method is that it measures the gas component directly requiring no assumptions of properties of dust in the wind. Thereafter we present our observational approach in more detail in terms of its validity and its assumptions. In the second part of this paper we discuss capabilities and assumptions of current models of stellar winds. We propose and discuss improvements to such models that will allow meaningful comparisons with our observations. Currently the physically most complete models include too little mass in the model domain to permit a formation of winds with as high mass-loss rates as our observations show.

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