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Mineralogical and geochemical study of rare earth elements from a silicate deposit

机译:硅酸盐沉积物稀土元素的矿物学和地球化学研究

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The leachability of the rare earth elements (REE) from the Kipawa deposit, a Heavy REE (HREE) mine project of Matamec resources, was investigated in order to predict their geochemical behavior and to evaluate the factors controlling the REE mobility in ambient conditions. All lithologies of the deposit, including ore and waste rocks, were sampled, characterized using automated SEM-EDS mineralogy, and submitted to kinetic testing using weathering cells in order to investigate their REE leaching potential. All leachates showed a neutral to alkaline pH (7.0 to 9.5) and alkalinity values between 10 and 173 mg CaCO_3/l. The REE concentrations leached from the materials are all below 15μ.g/L. Works are underway (i.e. thermodynamic equilibrium calculations) to determine the control factors of the REE release in the leachates.
机译:研究了Kipawa矿床稀土元素(REE)的可浸出性,麦克风资源的重型REE(HREE)矿井项目,以预测其地球化学行为,并评估控制环境条件下的REE移动性的因素。对包括矿石和废岩体的沉积物的所有岩性被取样,其特征在于使用自动化的SEM-EDS矿物学,并使用风化细胞提交给动力学测试,以研究其REE浸出潜力。所有渗滤液显示中性至碱性pH(7.0至9.5)和10-173mg Caco_3 / L之间的碱度值。从材料浸出的REE浓度均低于15μ.g/升。作品正在进行(即热力学平衡计算),以确定渗滤液中的REE释放的控制因素。

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