利用COMSOL软件开发了用于尾矿堆场除尘过程研究的大气空气热力学模型

P. Amosov, A. Baklanov
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引用次数: 0

摘要

本文概述了利用计算流体动力学软件系统(CFD建模)研究采矿设施空气热力学和大气污染的概况。专业软件和非专业软件都有标记。本文重点介绍了使用FLOWVISION、ANSYS FLUENT和COMSOL软件代码进行的研究。本文描述了一个大气的空气热力学模型,其中用传热方程和科里奥利、对流(浮力)、本底分层和辐射通量等参数补充了不可压缩流体近似中的动力学方程。本文描述了COMSOL软件中必要的修改,这使得在各种大气条件下进行大气空气热力学研究成为可能。建立了一个二维CFD大气模型,并在尾矿库的简化表示上进行了试验。在固定风速5 m/s和背景分层参数变化(-0.05 ~ +0.05℃/m)条件下,进行了数值实验,并对计算结果进行了分析。注意到不同大气条件下气流气动参数和温度空间分布的差异。利用粉尘强度的经验依赖性估计了粉尘高度处的动态速度和垂直质量通量。讨论了垂直质量通量随分层参数的解析依赖关系。与不稳定状态和逆温状态相比,显示了垂直质量通量量级的不对称性(相对于大气中性状态)。在稳定的大气条件下,沙尘团垂直通量的大小,以及由此产生的下游大气污染,将明显高于不稳定状态。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Development of a model of atmospheric aerothermodynamics for the study of dusting processes at tailings dumps using COMSOL software
An overview of studies of aerothermodynamics and atmospheric pollution at mining facilities using computational fluid dynamics software systems (CFD modeling) has been presented. Both specialized and non-specialized software are marked. The review focuses on the studies performed using the FLOWVISION, ANSYS FLUENT and COMSOL software codes. An aerothermodynamic model of the atmosphere is described in which the equations of dynamics in the incompressible fluid approximation are supplemented by the heat transfer equation and the parameters of Coriolis, convection (buoyancy), background stratification and radiation flux. The necessary modifications in the COMSOL software are described, which make it possible to carry out studies of atmospheric aerothermodynamics under various atmospheric conditions. A two-dimensional CFD model of the atmosphere has been built and tested on a simplified representation of the tailings dump. At a fixed wind flow velocity of 5 m/s and variations in the background stratification parameter (from –0.05 to +0.05 °C/m), numerical experiments have been performed and the calculation results have been analyzed. Differences in the aerodynamic parameters of the flows and the spatial distribution of temperature under different atmospheric conditions are noted. Estimates of the dynamic velocity at the dusting height and the vertical mass flux using the empirical dependence of the dusting intensity are performed. The analytical dependence of the vertical mass flux as a function of the stratification parameter is discussed. The asymmetry (relative to the neutral state of the atmosphere) of the magnitude of the vertical mass flux in comparison with the unstable and inversion states is shown. In stable atmospheric conditions, the magnitude of the vertical flux of the dust mass, and hence the pollution of the atmosphere downstream, will be noticeably higher than in unstable states.
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