钪
褐铁矿
超镁铁质岩
红土
腐岩
镍
冶金
地质学
背景(考古学)
地球化学
材料科学
矿物学
风化作用
古生物学
赤铁矿
作者
S Onggang,Adi Maulana,Sufriadin Sufriadin,Ulva Ria Irfan
出处
期刊:IOP conference series
[IOP Publishing]
日期:2021-11-01
卷期号:921 (1): 012040-012040
被引量:3
标识
DOI:10.1088/1755-1315/921/1/012040
摘要
Abstract Scandium is one of the rare earth elements which is currently widely used for various needs such as the aerospace industry, solid oxide fuel cells, electronics industry and in metallurgical applications. Generally, Scandium appears in small amounts so its structural role in the host minerals cannot be readily identified. Some studies reported the scandium extraction from lateritic nickel deposit where may contain considerable amount of scandium in addition to nickel and cobalt. Preliminary research of scandium enrichment has been investigated from the ultramafik rock indicates that an enrichment of scandium concentration was found in the red limonite. The aim of this study was to investigate the potentially enrichment of scandium mineral from nickel laterite in Lapaopao Area. There are a total of 38 samples from 1 (one) diamond drill holes which represent the limonite, saprolite and bedrock profiles have been collected and studied to investigate the distribution pattern of Sc grades within the lateritic profile. These samples are being analized by XRF for major and minor element and ICP-OES method for rare earth element assaying. The study has confirmed that scandium is enriched in limonite layer of weathered ultramafic laterite profile. The scandium content from the ultramafic bedrock is 15 ppm and has enriched until 81 ppm of scandium in the limonite layer.
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