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arXiv 1002.3437astro-ph.SR
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对流、过冲和重力波对M矮星和棕矮星大气尘埃输送的作用

The role of convection, overshoot, and gravity waves for the transport of dust in M dwarf and brown dwarf atmospheres

Bernd Freytag, France Allard, Hans-Guenter Ludwig, Derek Homeier, Matthias Steffen

摘要:

观测上,棕矮星的光谱表明其大气中存在尘埃,但理论上尚不清楚是什么阻止尘埃沉降并从光谱形成区域消失。因此,标准模型不得不依赖于关于使尘埃颗粒在大气中保持高空的机制的特别假设。我们应用流体动力学模拟,以发展一个更好的物理理解的混合特性的宏观流动在M矮星和褐矮星大气,特别是底层对流区的影响。我们进行了二维辐射流体动力学模拟,包括尘埃颗粒的形成和运输的CO5BOLD代码的描述。模拟覆盖了对流区和光球层的顶部,包括有效温度在900 K和2800 K之间的尘埃层,所有的logg=5假设太阳的化学成分。对流过冲以指数下降速度的形式出现,尺度高度很小,因此它只影响几乎绝热对流层上方的区域。从那时起,混合是由重力波提供的,重力波的强度足以在较热的模型中维持薄的尘埃云。随着有效温度的降低,波的振幅变得更小,但云变得更厚,并发展出比重力波更有效地混合物质的内部对流。云的存在导致恒星表面在短时间和小空间尺度上呈现出高度结构化的外观。我们确定对流激发的重力波作为一个重要的混合过程中的M矮星和棕矮星大气。在强云形成的条件下,尘埃对流是主要的自持混合成分。

英文摘要:

Observationally, spectra of brown dwarfs indicate the presence of dust in their atmospheres while theoretically it is not clear what prevents the dust from settling and disappearing from the regions of spectrum formation. Consequently, standard models have to rely on ad hoc assumptions about the mechanism that keeps dust grains aloft in the atmosphere. We apply hydrodynamical simulations to develop an improved physical understanding of the mixing properties of macroscopic flows in M dwarf and brown dwarf atmospheres, in particular of the influence of the underlying convection zone. We performed 2D radiation hydrodynamics simulations including a description of dust grain formation and transport with the CO5BOLD code. The simulations cover the very top of the convection zone and the photosphere including the dust layers for effective temperatures between 900K and 2800K, all with logg=5 assuming solar chemical composition. Convective overshoot occurs in the form of exponentially declining velocities with small scale heights, so that it affects only the region immediately above the almost adiabatic convective layers. From there on, mixing is provided by gravity waves that are strong enough to maintain thin dust clouds in the hotter models. With decreasing effective temperature, the amplitudes of the waves become smaller but the clouds become thicker and develop internal convective flows that are more efficient in mixing material than gravity waves. The presence of clouds leads to a highly structured appearance of the stellar surface on short temporal and small spatial scales. We identify convectively excited gravity waves as an essential mixing process in M dwarf and brown dwarf atmospheres. Under conditions of strong cloud formation, dust convection is the dominant self-sustaining mixing component.

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