首页> 外文会议>International Symposium on Process Mineralogy >APPLICATION OF LA-ICP-MS TO PROCESS MINERALOGY: GA AND GE RECOVERY AT KIPUSHI CU-ZN DEPOSIT
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APPLICATION OF LA-ICP-MS TO PROCESS MINERALOGY: GA AND GE RECOVERY AT KIPUSHI CU-ZN DEPOSIT

机译:La-ICP-MS加工矿物学的应用:Kipushi Cu-Zn沉积物的GA和GE恢复

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In the field of process mineralogy, laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) is a valuable tool that can complement other mineralogical techniques used to characterise orebodies and concentrator performance. Many economic metals are present at ultra-low levels as solid solution or as inclusions within minerals and require complex recovery techniques to separate them from the bulk ore. Understanding metal occurrence is necessary for implementing the proper recovery strategies. LA-ICP-MS is a cost-effective and versatile method of measuring precious-metals and other economic trace-elements in solid solution in various types of mineral phases while achieving low detection limits.To demonstrate the practical uses of LA-ICP-MS to process mineralogy, XPS has collected data from a sulphide-rich heavy liquid separation and shaking table concentrate from the Kipushi Cu-Zn deposit, Katanga, Democratic Republic of Congo. In addition to Cu and Zn, Kipushi Corporation SA (KICO) is currently investigating strategies for concentrating Ge and Ga. A combination of gravity separation and recovery of Ge and Ga through flotation of Zn and other base metal sulphides are being considered. The objective of the LA-ICP-MS analysis was to determine the proportion of Ge and Ga present in solid solution in sulphides and in discrete mineral phases. The results indicate that sphalerite carries significant amounts of Ga (42.5 ppm, representing 54% of the Ga deportment) and chalcopyrite hosts moderate proportions of Ge (2462 ppm, representing 21% of the Ge deportment). Discrete phases host the remaining portions of Ga and Ge. The deportment information can be used to guide flowsheet development in order to optimize recovery.
机译:在过程矿物学领域,激光烧蚀电感耦合等离子体质谱法(LA-ICP-MS)是一种有价值的工具,可以补充用于表征矿体和集中器性能的其他矿物的技术。许多经济金属在超低水平上作为固体溶液或矿物质内的夹杂物存在,并且需要复杂的恢复技术来将它们与散装矿石分离。了解金属发生是实施适当的恢复策略所必需的。 La-ICP-MS是一种经济高效而多功能的方法,可在各种类型的矿泉共阶段测量固体溶液中的珍贵金属和其他经济微量元素,同时实现低检测限值。表明LA-ICP-MS的实际用途为了处理矿物学,XPS从硫化物富液体分离和摇动台浓缩物中收集来自Kipushi Cu-Zn矿床,Katanga,刚果民主共和国的数据。除Cu和Zn外,Kipushi Corporation SA(KICO)目前正在考虑浓缩GE和GA的策略。正在考虑GE和Ge的Ge和Ga通过Zn和其他碱金属硫化物的浮选的组合。 La-ICP-MS分析的目的是测定硫化物中固溶体和离散矿物相中的Ge和Ga的比例。结果表明,斯普利特携带大量的GA(42.5ppm,代表GA DEVOSTMENT的54%)和Chalcystite宿主中等比例的GE(2462ppm,代表GE驱逐21%)。离散阶段托管GA和GE的剩余部分。可驱逐信息可用于指导流程开发以优化恢复。

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