Effect of ore particle size on solution capillary seepage in ore heaps
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摘要: 為探究礦石粒徑對礦堆內溶液毛細滲流的影響特征,利用所構建的溶液毛細上升實驗裝置,針對單一粒徑礦堆和混合粒徑礦堆,分別開展不同礦石粒徑下溶液毛細上升實驗,得到了溶液毛細上升高度與時間的關系曲線及相應的擬合方程,分析了溶液上升速度隨時間變化規律.研究發現:實驗初期礦堆內溶液上升速度較快,隨著實驗時間的增加,溶液上升速度逐漸減小并最終降為零,且溶液最大上升高度及溶液上升速度均與礦石粒徑負相關.礦堆內由毛細作用形成的不可動溶液含量隨礦石平均粒徑的減小而增大,細顆粒礦石含量過多時在礦堆內將形成大范圍的不可動溶液區域,影響礦堆內溶液滲透效果.Abstract: To explore the characteristics of the effect of ore particle size on the capillary flow of solution in an ore heap, solution capillary rise experiments of two groups of ore particles, mono-size and non-uniform, were performed with an established capillary rise experimental device. The relationship of solution capillary rise height with time and the corresponding fitting equations were obtained. The regularity of solution rise velocity with time was analyzed. It is found that at the beginning of the experiment, the ore heap solution rises quickly; with the increase of time, the solution rise velocity decreases and eventually drops to zero; the maximum solution rise height and velocity have negative correlation with ore particle size. Immobile solution content inside the ore heap formed by capillary action increases with the decreasing of average particle size, and a wide range area of immobile solution will form when the content of fine particles in the ore heap is too much, which can influence the solution seepage of the ore heap.
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Key words:
- heap leaching /
- seepage /
- capillary rise method /
- particle size
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