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A modeling approach using back-calculated induction times to predict recoveries in flotation

机译:一种使用反向计算的诱导时间来预测浮选回收率的建模方法

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The current modeling flotation approach of the Julius Kruttschnitt Mineral Research Centre (JKMRC) predicts recoveries in a flotation circuit using a lumped parameter called the floatability of mineral particles (P) which has no direct physical meaning and is assumed to be conserved in flotation circuits in the absence of regrinding or change in chemical environment. In this paper, the original definition of P as the efficiency of collection was resurrected. Fundamental models of particle collection by bubbles were applied to an industrial data set from a down-the-bank flotation survey of the first four cells of the galena rougher circuit at BHP Billiton's Cannington operation in Australia. The floatability of mineral particles P was no longer treated as a lumped parameter but described by the physical measurable inputs of the models. Induction time as a model parameter was back-calculated from knowledge of the experimental data and application of the collection model. The assumption that the induction time of a size-by-liberation class at fixed chemistry was conserved allowed prediction of galena recoveries in the circuit. An extensive error analysis was conducted on the new modeling approach and it was found to be very sensitive to the value of the bubble rise velocity. Finally, since the variation in the key flotation variables down the bank at the BHP Billiton Cannington's lead rougher circuit was not significant, the two approaches predicted similar flotation kinetics down the bank.
机译:Julius Kruttschnitt矿物研究中心(JKMRC)当前的模型浮选方法使用称为矿物颗粒浮性(P)的集总参数预测浮选回路中的采收率,该集总参数没有直接的物理意义,并且假定在以下地区的浮选回路中是保守的没有再研磨或化学环境变化。在本文中,将P作为收集效率的最初定义复活了。气泡收集颗粒的基本模型被应用于来自澳大利亚必和必拓公司Cannington工厂方铅矿粗糙电路前四个单元的浮选调查的工业数据集。矿物颗粒P的可浮性不再被视为集总参数,而是由模型的物理可测量输入来描述。归纳时间作为模型参数是根据对实验数据的了解和收集模型的应用而反算的。在固定化学条件下按解放军类别的感应时间被保留的假设可以预测电路中方铅矿的回收率。对新的建模方法进行了广泛的误差分析,发现它对气泡上升速度的值非常敏感。最后,由于必和必拓Cannington的前轮粗选电路沿岸关键浮选变量的变化不显着,因此这两种方法预测了沿岸的相似浮选动力学。

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