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Multivariate Geometallurgical Modeling in Potassium Alterations for Sulfide Minerals

机译:硫化钾矿物质钾改变的多变量几何冶金模型

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Modeling of geological attributes is a fundamental step in the mining process where quality resources are defined for mining and metallurgical processing. The metallurgical recovery of sulphide minerals in the flotation stage is a variable that depends not only on geological attributes such as ore type, alteration, etc., it also depends on operational parameters such as pH, quantity and quality of chemicals such as thickeners and collectors, residence time, granulometry, etc. These factors make modeling difficult, since the recovery might depend on factors external to geology.In this research we studied multivariable correlations that allow prediction of metallurgical recovery (Rec30 - percentage recovery of the ore after 30 minutes of flotation) through multivariate geostatistics: for this purpose an estimation of the recovery using co-kriging was performed taking into account variables that have high correlations. In this case study a high correlation between iron grades and recovery in potassium-rich alterations was found, which is attributed mainly to the amount of pyrite that makes the process difficult. Additionally, the incorporation of co-kriging allows increasing the estimated tonnage, when there is little information about the primary variable (but not the secondary variable).The advantage of using classical geostatistics is that recovery models can be obtained with good results in terms of cross-validation (good prediction), which overcomes the problem of non-additivity in the case of the generation of a block model for geometallurgical variables. In addition, the advantage of using co-kriging is that the information of this secondary variable is much denser, hence provides improved model resolution. The metallurgical recovery samples are usually expensive and few, the incorporation of secondary well correlated variable then generate a more robust and reliable recovery model.
机译:地质属性建模是采矿过程中的基本步骤,其中为采矿和冶金加工定义了质量资源。浮选阶段中的硫化物矿物质的冶金恢复是一种可变,其不仅取决于矿石类型,改变等的地质属性,它还取决于操作参数,例如增稠剂和收集器等化学品的pH值,数量和质量,停留时间,粒度测量等。这些因素使模型困难,因为恢复可能取决于地质外部的因素。在本研究中,我们研究了允许预测冶金恢复预测的多变量相关性(30分钟后矿石恢复矿石百分比浮选)通过多变量地质学习学:为此目的,考虑具有高相关的变量进行使用CO-Kriging来估计恢复。在这种情况下,研究铁成绩与富含钾的改变的储存之间的高相关,主要归因于使过程困难的黄铁矿量。另外,当有关主变量(但不是次要变量)的信息很少时,CO-Kriging的结合允许增加估计的吨位。使用经典地稳态的优势是可以获得恢复模型的恢复模型交叉验证(良好的预测),其克服了在生成几何变量的块模型的情况下的非增殖性问题。另外,使用Co-Kriging的优点是该次级变量的信息很多更密集,因此提供了改进的模型分辨率。冶金恢复样品通常昂贵且很少,次级阱相关变量的掺入然后产生更稳健和可靠的恢复模型。

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