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arXiv 0901.4434astro-ph.EP
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分层和湍流原行星盘的全球MHD模拟。II。降尘

Global MHD simulations of stratified and turbulent protoplanetary discs. II. Dust settling

Sebastien Fromang, Richard P. Nelson

摘要:

本文的目的是研究小尘埃粒子在原行星盘的垂直分布,其中角动量传输是由于磁旋转不稳定性驱动的MHD湍流。我们考虑的颗粒尺寸范围从大约1微米到几毫米。我们使用基于网格的MHD代码进行全球性的双流体模拟湍流原行星盘,其中包含各种尺寸的尘埃颗粒。在准稳态下,尘埃粒子的重力沉降由湍流扩散平衡。该过程的简单和标准模型不能准确地描述粉尘密度的垂直分布。对于小的尘埃颗粒(几微米大小),特别是在盘的上层($Z>3H$,其中$H$是刻度高度),差异更大。在这里,简单模型预测和模拟结果之间的差异可能有几个数量级。这是因为MHD湍流在吸积盘中是不均匀的,因为速度波动在强烈磁化的日冕发展的盘上层显着增加。我们提供了一个替代模型,提供了一个更好的适合模拟。在这个模型中,尘埃粒子扩散远离中平面的MHD湍流,但扩散系数垂直变化,并在任何地方都成比例的当地湍流垂直速度波动的平方。尘埃粒子的空间分布可以用来追踪原行星盘中MHD湍流的性质,如速度波动的幅度。在未来,数值模拟和观测之间的详细和直接的比较应该被证明是一个有用的工具,用于约束原行星盘中的湍流特性。

英文摘要:

The aim of this paper is to study the vertical profile of small dust particles in protoplanetary discs in which angular momentum transport is due to MHD turbulence driven by the magnetorotational instability. We consider particle sizes that range from approximately 1 micron up to a few millimeters.We use a grid--based MHD code to perform global two-fluid simulations of turbulent protoplanetary discs which contain dust grains of various sizes. In quasi--steady state, the gravitational settling of dust particles is balanced by turbulent diffusion. Simple and standard models of this process fail to describe accurately the vertical profile of the dust density. The disagreement is larger for small dust particles (of a few microns in size), especially in the disc upper layers ($Z>3H$, where $H$ is the scale-height). Here there can be orders of magnitude in the disagreement between the simple model predictions and the simulation results. This is because MHD turbulence is not homogeneous in accretion discs, since velocity fluctuations increase significantly in the disc upper layer where a strongly magnetized corona develops. We provide an alternative model that gives a better fit to the simulations. In this model, dust particles are diffused away from the midplane by MHD turbulence, but the diffusion coefficient varies vertically and is everywhere proportional to the square of the local turbulent vertical velocity fluctuations. The spatial distribution of dust particles can be used to trace the properties of MHD turbulence in protoplanetary discs, such as the amplitude of the velocity fluctuations. In the future, detailed and direct comparison between numerical simulations and observations should prove a useful tool for constraining the properties of turbulence in protoplanetary discs.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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