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湍流穿透对流中被动标量的非局部输运。

Nonlocal transport of passive scalars in turbulent penetrative convection.

作者信息

Miesch MS, Brandenburg A, Zweibel EG

机构信息

DAMTP, University of Cambridge, Silver Street, Cambridge CB3 9EW, United Kingdom and JILA, University of Colorado, Boulder, Colorado 80309-0440, USA.

出版信息

Phys Rev E Stat Phys Plasmas Fluids Relat Interdiscip Topics. 2000 Jan;61(1):457-67. doi: 10.1103/physreve.61.457.

Abstract

We present a Green's function approach for quantifying the transport of a passive scalar (tracer) field in three-dimensional simulations of turbulent convection. Nonlocal, nondiffusive behavior is described by a transilient matrix (the discretized Green's function), whose elements contain the fractional tracer concentrations moving from one subvolume to another as a function of time. The approach was originally developed for and applied to geophysical flows, but here we extend the formalism and apply it in an astrophysical context to three-dimensional simulations of turbulent compressible convection with overshoot into convectively stable bounding regions. We introduce a novel technique to compute this matrix in a single simulation by advecting labeled particles rather than solving the passive scalar equation for a large number of different initial conditions. The transilient matrices thus computed are used as a diagnostic tool to quantitatively describe nonlocal transport via matrix moments and transport coefficients in a generalized, multiorder diffusion equation. Results indicate that transport in both the vertical and horizontal directions is strongly influenced by the presence of coherent velocity structures, generally resembling ballistic advection more than diffusion. The transport of a small fraction of tracer particles deep into the underlying stable region is reasonably efficient, a result which has possible implications for the problem of light-element depletion in late-type stars.

摘要

我们提出了一种格林函数方法,用于在湍流对流的三维模拟中量化被动标量(示踪剂)场的输运。非局部、非扩散行为由瞬变矩阵(离散化的格林函数)描述,其元素包含作为时间函数从一个子体积移动到另一个子体积的示踪剂分数浓度。该方法最初是为地球物理流动开发并应用的,但在这里我们扩展了形式主义,并将其应用于天体物理背景下的湍流可压缩对流三维模拟,包括过冲到对流稳定的边界区域。我们引入了一种新颖的技术,通过平流标记粒子而不是针对大量不同初始条件求解被动标量方程,在单个模拟中计算该矩阵。如此计算出的瞬变矩阵用作诊断工具,通过广义多阶扩散方程中的矩阵矩和输运系数来定量描述非局部输运。结果表明,垂直和水平方向的输运都受到相干速度结构的强烈影响,总体上更类似于弹道平流而非扩散。一小部分示踪剂粒子深入到下层稳定区域的输运相当有效,这一结果可能对晚型恒星中轻元素耗尽问题有影响。

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