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arXiv 1503.02723astro-ph.SR
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部分电离效应在色球层中的作用

The Role of Partial Ionization Effects in the Chromosphere

Juan Martinez-Sykora, Bart De Pontieu, Viggo H. Hansteen, Mats Carlsson

AI总结:

本文综述并通过 Bifrost 的 2.5D 辐射 MHD 模拟表明,色球层部分电离导致的离子-中性粒子相互作用会通过 Hall 项和双极扩散改变能量耗散与大气结构。

摘要:

日冕加热所需的能量必须由对流区提供。这种能量向日冕传输的数量和方式取决于低层大气和日冕本身的性质。我们综述:1)能量如何在太阳低层大气中积累;2)这种能量如何通过太阳大气传输;以及3)能量最终如何在色球层和/或日冕中耗散。任何能量传输机制都必须处理低层大气中的各种物理过程。我们将聚焦一个在色球层中似乎极为重要、但直到近期才得到深入研究的物理过程:色球层中的离子-中性粒子相互作用效应(INIE)。我们综述了部分电离在色球层中的相关性和作用,并表明该过程实际上对太阳外层大气有显著影响。我们纳入了对使用 Bifrost 代码(Gudiksen 等人,2011)开展的 2.5 维辐射磁流体力学(MHD)模拟的分析,这些模拟包含色球层和日冕的部分电离效应以及沿磁场线的热传导。光球层、色球层和过渡区处于部分电离状态,电离粒子与中性粒子之间的相互作用对这些层次的磁热力学具有重要影响。INIE 通过广义欧姆定律处理,即我们在感应方程中考虑 Hall 项和双极扩散。不同粒子种类之间的相互作用对模拟大气产生如下影响:1)双极扩散耗散磁能,并提高色球层的最低温度;2)上色球层可能在更大的高度范围内被加热并膨胀。这些过程揭示,在包含与不包含 INIE 的模拟中,模拟大气之间存在明显差异。

英文摘要:

The energy for the coronal heating must be provided from the convection zone. The amount and the method by which this energy is transferred into the corona depends on the properties of the lower atmosphere and the corona itself. We review: 1) how the energy could be built in the lower solar atmosphere; 2) how this energy is transferred through the solar atmosphere; and 3) how the energy is finally dissipated in the chromosphere and/or corona. Any mechanism of energy transport has to deal with the various physical processes in the lower atmosphere. We will focus on a physical process that seems to be highly important in the chromosphere and not deeply studied until recently: the ion-neutral interaction effects (INIE) in the chromosphere. We review the relevance and the role of the partial ionization in the chromosphere and show that this process actually impacts considerably the outer solar atmosphere. We include analysis of our 2.5D radiative MHD simulations with the Bifrost code (Gudiksen et al. 2011) including the partial ionization effects on the chromosphere and corona and thermal conduction along magnetic field lines. The photosphere, chromosphere and transition region are partially ionized and the interaction between ionized particles and neutral particles has important consequences on the magneto-thermodynamics of these layers. The INIE are treated using generalized Ohm's law, i.e., we consider the Hall term and the ambipolar diffusion in the induction equation. The interaction between the different species affects the modeled atmosphere as follows: 1) the ambipolar diffusion dissipates magnetic energy and increases the minimum temperature in the chromosphere; 2) the upper chromosphere may get heated and expanded over a greater range of heights. These processes reveal appreciable differences between the modeled atmospheres of simulations with and without INIE.

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