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arXiv 0908.2247astro-ph.GA
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热力学在圆盘破碎中的作用

The role of thermodynamics in disc fragmentation

Dimitris Stamatellos, Anthony Whitworth

摘要:

热力学在决定原恒星盘碎片形成行星、棕矮星和低质量恒星的方式方面起着重要作用。我们探讨的效果,不同的处理辐射转移在模拟破碎光盘。辐射转移有三种计算方法:(i)Stamatellos等人的扩散近似,(ii)Goodwin等人的正压状态方程(EOS),和(iii)Bate等人的正压EOS。正压近似捕获了每个原碎片中心的密度和温度的一般演变,但(i)它们没有对在圆盘中形成的原碎片的特定情况进行任何调整,(ii)它们没有考虑对于在圆盘外部区域快速形成原碎片重要的热惯性效应。因此,当使用正压EOS时,在圆盘中形成的碎片的数量和它们的性质是不同的。这不仅对盘的研究很重要,而且对坍缩湍流云的模拟也很重要,因为在许多情况下,在这样的模拟中,恒星形成的盘随后碎裂。我们还使用扩散近似,并在每个原碎片坍缩之后,直到形成第二个核心(~10^{-3} g/cm 3),研究了原碎片在距中心恒星不同距离的圆盘中凝聚出来的方式的差异。我们发现,形成更接近中央恒星的原碎片往往形成更早,从第一个核心到第二个核心的演化速度比形成在外盘区域的原碎片更快。前者在内部盘区域有一个大的物质池,它们可以从中吸积并大量生长。后者的吸积速度更慢,温度更高,因为它们通常形成于一个快速的突发事件中。

英文摘要:

Thermodynamics play an important role in determining the way a protostellar disc fragments to form planets, brown dwarfs and low-mass stars. We explore the effect that different treatments of radiative transfer have in simulations of fragmenting discs. Three prescriptions for the radiative transfer are used, (i) the diffusion approximation of Stamatellos et al., (ii) the barotropic equation of state (EOS) of Goodwin et al., and (iii) the barotropic EOS of Bate et al. The barotropic approximations capture the general evolution of the density and temperature at the centre of each proto-fragment but (i) they do not make any adjustments the particular circumstances of a proto-fragment forming in the disc, and (ii) they do not take into account thermal inertia effects that are important for fast-forming proto-fragments in the outer disc region. As a result, the number of fragments formed in the disc and their properties are different, when a barotropic EOS is used. This is important not only for disc studies but also for simulations of collapsing turbulent clouds, as in many cases in such simulations stars form with discs that subsequently fragment. We also examine the difference in the way proto-fragments condense out in the disc at different distances from the central star using the diffusion approximation and following the collapse of each proto-fragment until the formation of the second core (~10^{-3} g/cm3). We find that proto-fragments forming closer to the central star tend to form earlier and evolve faster from the first to the second core than proto-fragments forming in the outer disc region. The former have a large pool of material in the inner disc region that they can accrete from and grow in mass. The latter accrete more slowly and they are hotter because they generally form in a quick abrupt event.

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