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首页> 外文期刊>The Astrophysical journal >EXCITATION OF GRAVITY WAVES BY FINGERING CONVECTION, AND THE FORMATION OF COMPOSITIONAL STAIRCASES IN STELLAR INTERIORS
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EXCITATION OF GRAVITY WAVES BY FINGERING CONVECTION, AND THE FORMATION OF COMPOSITIONAL STAIRCASES IN STELLAR INTERIORS

机译:手指对流激发重力波,并在星状室内形成复合阶梯

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Fingering convection (or thermohaline convection) is a weak yet important kind of mixing that occurs in stably stratified stellar radiation zones in the presence of an inverse mean molecular weight gradient. Brown et al. recently proposed a new model for mixing by fingering convection, which contains no free parameter?and was found to fit the results of direct numerical simulations in almost all cases. Notably, however, they found that mixing was substantially enhanced above their predicted values in the few cases where large-scale gravity waves, followed by thermo-compositional layering, grew spontaneously from the fingering convection. This effect is well?known in the oceanographic context?and is attributed to the excitation of the so-called collective instability.?In this work, we build on the results of Brown et al. and of Traxler et al. to determine the conditions under which the collective instability may be expected. We find that it is only relevant in stellar regions that have a relatively large Prandtl number (the ratio of the kinematic viscosity to the thermal diffusivity), or larger. This implies that the collective instability cannot occur in main-sequence stars, where the Prandtl number is always much smaller than this (except in the outer layers of surface convection zones, where fingering is irrelevant anyway). It could in principle be excited in regions of high electron degeneracy, during He core flash, or in the interiors of white dwarfs. We discuss the implications of our findings for these objects, from both a theoretical and?an observational point of view.
机译:指状对流(或热盐对流)是一种弱而重要的混合方式,在平均分子量反比存在的情况下,在稳定分层的恒星辐射区中发生。布朗等。最近,他提出了一种新的指流对流混合模型,该模型不包含自由参数,并且几乎可以满足所有直接数值模拟的结果。然而,值得注意的是,他们发现在少数情况下,指压对流会自发地产生大规模重力波,随后进行热成分分层,从而大大增强了混合,使其超出了预期值。这种效应在海洋学背景中是众所周知的,并且归因于所谓的集体不稳定性的激发。在这项工作中,我们以布朗等人的结果为基础。和Traxler等人。确定在何种情况下可能会发生集体不稳定。我们发现,仅在具有相对较大的Prandtl数(运动粘度与热扩散率之比)或更大的恒星区域中才有意义。这意味着主序恒星不可能发生集体不稳定性,在主序恒星中,Prandtl数总是比这个小得多(除非在表面对流区的外层中指法无关紧要)。原则上,它可以在高电子简并性区域,He核闪光期间或白矮星内部激发。我们从理论和观察的角度讨论了我们的发现对这些对象的意义。

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