New numerical models of atomic diffusion in the atmospheres of cool Ap stars, including ambipolar diffusion of hydrogen

G. Alecian, M. Stift
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Abstract

Ambipolar diffusion of hydrogen gives an additional upward thrust to metals that diffuse in the atmosphere of Ap stars. Its quantitative effect on the build-up of abundance stratification due to atomic diffusion that produces the observed abundance anomalies in Ap stars has not been evaluated so far. The purpose of this work is to quantify this effect throughout the stratification process of metals inside the atmosphere. We used our code caratmotion to compute the time-dependent atomic diffusion of four metals (Mg, Ca, Si, and Fe) in the atmosphere of a main-sequence star with an effective temperature of $8\,500$\,K, which is a typical temperature of Ap stars. The results, including ambipolar diffusion of H, are compared to results obtained without this process. Our main result is that ambipolar diffusion must be included in any calculation of atomic diffusion in Ap star atmospheres, at least for stars with $T_ eff 10\,000$\,K. We show that this concerns all metals, even those that are well supported by the radiation field, such as Fe. The crucial role of the stellar mass-loss rate is confirmed; it remains a determining parameter that is constrained, but still free in our calculations. We also present 3D calculations of Ca distributions in magnetic atmospheres. Questioning the interest of systematic searches for stationary solutions (which can often only be reached after a long evolutionary process), we note that remarkable behaviour can occur during the transient phases of the stratification build-up.
冷 Ap 星大气中原子扩散的新数值模型,包括氢的伏极扩散
氢的常极性扩散为在Ap星大气中扩散的金属提供了额外的向上推力。迄今为止,还没有评估过它对原子扩散导致的丰度分层的定量影响,而原子扩散会在Ap星中产生观测到的丰度异常。这项工作的目的是量化大气层内金属分层过程中的这种影响。我们使用 Caratmotion 代码计算了主序星大气中四种金属(Mg、Ca、Si 和 Fe)随时间变化的原子扩散,主序星的有效温度为 $8,500\$,K,这是 Ap 星的典型温度。我们将包括H的伏极扩散在内的结果与没有这一过程的结果进行了比较。我们的主要结果是,在计算Ap恒星大气中的原子扩散时,必须包括伏极扩散,至少对于T_ eff为10,000美元(K)的恒星是这样。我们的研究表明,这涉及到所有金属,甚至包括那些辐射场支持良好的金属,比如铁。恒星质量损失率的关键作用得到了证实;它仍然是一个决定性参数,在我们的计算中受到约束,但仍然是自由的。我们还介绍了磁性大气中 Ca 分布的三维计算。我们质疑系统搜索静态解(通常要经过漫长的演化过程才能达到)的意义,我们注意到在分层建立的瞬态阶段会出现显著的行为。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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