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首页> 外文期刊>Mathematical Problems in Engineering: Theory, Methods and Applications >A Coupled Model for Solution Flow and Bioleaching Reaction Based on the Evolution of Heap Pore Structure
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A Coupled Model for Solution Flow and Bioleaching Reaction Based on the Evolution of Heap Pore Structure

机译:基于堆孔结构演化的溶液流动和生物浸交反应的耦合模型

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摘要

Based on the basic seepage law, equations have been derived to descript the solution flow within the copper ore heap which is treated as anisotropy porous media. The relationship between heap permeability and pore ratio has been revealed. Given the consideration of cover pressure and particle dissolution, pore evolution model has been set up. The pore evolution mechanism, due to the process of dissolution, precipitation, blockage, collapse, and caking, has been investigated. The comprehensive model for pore evolution and solution flow under the effect of solute transport and leaching reaction has been established. A trapezoidal heap was calculated, and the estimated results show that permeability decreases with the decreasing of pore ratio. Therefore, the permeability of the heap with small particles is relatively low because of its low pore ratio. Furthermore, permeability and height are found to be the two main factors influencing the solution flow.
机译:基于基本的渗流法,已经得出了方程来描述铜矿堆内的溶液流,其被视为各向异性多孔介质。 据揭示了堆渗透率与孔隙率之间的关系。 鉴于考虑覆盖压力和粒子溶解,已经建立了孔隙演化模型。 已经研究了孔隙演化机制,由于溶解,沉淀,堵塞,塌陷和结块的过程。 建立了溶质输送和浸出反应效果下孔隙演化和溶液流动的综合模型。 计算梯形堆,估计结果表明渗透率随着孔比的降低而降低。 因此,由于其低孔径,具有小颗粒的堆的渗透率相对较低。 此外,发现渗透性和高度是影响溶液流动的两个主要因素。

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