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基于離散元理論的自然崩落法放礦細顆粒滲移過程研究

Discrete element method study on the percolation process of fine particles in ore drawing by the block caving method

  • 摘要: 為探討自然崩落法放礦過程中廢石細顆粒的滲移規律及誘因,利用離散元軟件EDEM分別從粗細顆粒數量比、直徑比及礦巖含水率三個方面對細顆粒的滲移過程進行模擬,并設置標志顆粒對不同區域的相鄰粗細顆粒進行跟蹤.研究結果表明:放礦提前貧化率隨粗細顆粒數量比的增大不斷降低;廢石細顆粒滲移速率隨粗細顆粒直徑比的增大而增大,且受含水率影響顯著;相鄰位置的細顆粒的滲移速度大于粗顆粒的下降速度.研究結果為進一步探討礦石損失貧化、確定采場結構參數及優化放礦管理制度提供理論支持.

     

    Abstract: To explore the percolation regulation and inducement of waste fine particles in ore drawing by the block caving method, a simulation is undertaken by using discrete element method software EDEM. This simulation contains coarse-to-fine particle amount ratio, diameter ratio and moisture content, and sets marker particles in different regions to trace the migration of adjacent coarse and fine particles. The results indicate that the ore-drawing advance dilution rate decreases with increasing coarse-to-fine particle amount ratio. The percolation rate of waste fine particles increases with increasing diameter ratio and is significantly affected by moisture content. Moreover, the percolation rate of fine particles is greater than the decline rate of adjacent coarse particles. The results provide a theoretical support for further studying and discussing the ore loss and dilution, determining the stope structure parameters and optimizing the ore drawing management system.

     

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