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Fingering convection induced by atomic diffusion in stars: 3D numerical computations and applications to stellar models

机译:星体中原子扩散引起的指法对流:三维数值   计算和应用于恒星模型

摘要

Iron-rich layers are known to form in the stellar subsurface through acombination of gravitational settling and radiative levitation. Their presence,nature and detailed structure can affect the excitation process of variousstellar pulsation modes, and must therefore be modeled carefully in order tobetter interpret Kepler asteroseismic data. In this paper, we study theinterplay between atomic diffusion and fingering convection in A-type stars,and its role in the establishment and evolution of iron accumulation layers. Todo so, we use a combination of three-dimensional idealized numericalsimulations of fingering convection, and one-dimensional realistic stellarmodels. Using the three-dimensional simulations, we first validate the mixingprescription for fingering convection recently proposed by Brown et al. (2013),and identify what system parameters (total mass of iron, iron diffusivity,thermal diffusivity, etc.) play a role in the overall evolution of the layer.We then implement the Brown et al. (2013) prescription in the Toulouse-GenevaEvolution code to study the evolution of the iron abundance profile beneath thestellar surface. We find, as first discussed by Th\'eado et al. (2009), thatwhen the concurrent settling of helium is ignored, this accumulation rapidlycauses an inversion in the mean molecular weight profile, which then drivesfingering convection. The latter mixes iron with the surrounding material veryefficiently, and the resulting iron layer is very weak. However, taking heliumsettling into account partially stabilizes the iron profile against fingeringconvection, and a large iron overabundance can accumulate. The opacity alsoincreases significantly as a result, and in some cases ultimately triggersdynamical convection.
机译:已知通过重力沉降和辐射悬浮的结合在恒星的地下形成富铁层。它们的存在,性质和详细的结构会影响各种星状脉动模式的激发过程,因此必须仔细建模,以更好地解释开普勒卫星地震数据。本文研究了A型恒星中原子扩散与指流对流之间的相互作用,及其在铁累积层建立和演化中的作用。为此,我们将指对流的三维理想化数值模拟与一维逼真的恒星模型结合使用。使用三维模拟,我们首先验证了Brown等人最近提出的用于指流对流的混合处方。 (2013年),并确定哪些系统参数(铁的总质量,铁的扩散率,热扩散率等)在该层的整体演化中起作用。 (2013)在图卢兹-日内瓦进化法中规定研究星表下铁丰度分布的演变。我们发现,正如Th \'eado等人首先讨论的那样。 (2009年),当氦气的同时沉降被忽略时,这种积累迅速导致平均分子量分布的倒置,从而驱动手指对流。后者非常有效地将铁与周围的材料混合,生成的铁层非常薄弱。然而,考虑到氦沉降,部分地稳定了铁的轮廓以防止指状对流,并且可能积累大量的铁过量。结果,不透明度也显着增加,并且在某些情况下最终触发动态对流。

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