反转大气条件下露天矿不同深度自然通风过程的数值模拟

P. Amosov, A.A. Baklanov
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引用次数: 0

摘要

研究目的是评估背景分层参数和露天矿深度对矿井自然通风时间和北方爆破作业下风向矿坑上侧大气污染程度的影响。使用了大气空气热力学模型,其中不可压缩流体近似动力学方程补充了传热方程,并考虑了浮力和背景分层机制。该模型是在通用 COMSOL 软件包中创建的,可以研究各种状态下的大气气动热力学。利用再循环通风过程对露天矿大气的二维 CFD 模型进行了测试。背景分层参数(从 0.0 到 +0.025 °С/m,增量为 0.005 °С/m)和采石场深度(从 300 米到 700 米)均有变化。记录了矿坑上侧 1 m/s 的风速、尘云和气云的初始位置(矿坑中心靠近底板处)以及矿坑壁 45° 的倾斜角。在大气逆转加剧时,露天矿自然通风时间明显增加。随着基坑深度的增加,预测了两种最大污染区的形成类型:(1) 在中性分层时,从基坑中心向基坑左侧移动;(2) 在正背景分层时,位于基坑中心靠近底面的位置。结果表明,基坑深度和背景分层参数的增加会导致基坑上侧达到最大浓度的时间明显增加,而最大浓度值则会减小。对于再循环通风方案,大气中反常现象的加剧增加了自然通风的时间,但降低了地坑上侧下游的大气污染水平。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical modeling of natural ventilation processes in an open pit mine at its various depths in inversion atmospheric conditions
The research objective is to assess the influence of the background stratification parameter and the depth of an open pit mine on the time of natural ventilation of the mine and the level of atmospheric pollution at the upper side of the pit downwind of blasting operations in conditions of the North. An aerothermodynamic model of the atmosphere was used, in which the equations of dynamics in the approximation of incompressible fluid were supplemented with the heat transfer equation, and the buoyancy and background stratification mechanisms were taken into account. The model was created in a general-purpose COMSOL software package and makes it possible to study aerothermogasodynamics of the atmosphere in its various states. A two-dimensional CFD-model of the open pit atmosphere was tested using the recirculation ventilation process. The background stratification parameter (from 0.0 to +0.025 °С/m with the increment of 0.005 °С/m) and the quarry depth from 300 to 700 m were variated. The wind velocity of 1 m/s at the upper side of the pit, the initial location of the dust and gas cloud (in the center of the pit near its floor) and the slope angle of the pit wall of 45° were recorded. A significant increase in the time of natural ventilation of the open pit is demonstrated at intensifying inversion of the atmosphere. Two formation types of the maximum pollution area with the increasing pit depth are predicted: (1) displacement from the center to the lee side of the pit at neutral stratification; and (2) position in the center of the pit near its floor at positive background stratification. It is shown that increasing of both the pit depth and the background stratification parameter leads to a noticeable increase in the time to reach the maximum concentration at the upper side of the pit and a decrease in the value of this maximum. For the recirculation ventilation scheme, intensification of inversion in the atmosphere increases the time of natural ventilation, but reduces the level of atmospheric contamination at the upper side of the pit downstream.
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