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USE OF MAGNETIC SEPARATION TO BENEFICIATE RARE METAL ORES

机译:使用磁分离法提纯稀有金属矿石

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摘要

With respect to their magnetic properties, minerals in the rare metal ores under examination can be basically grouped as weakly-magnetic and nonmagnetic. Fig. 1 shows the spectra of their specific magnetic susceptibility values (x). As is evident, the range of changes in percent of ore minerals fluctuates from -0.35 centre dot 10~(-9) m~3/kg (cryolite) to 68.0 centre dot 10~(-9) m~3/kg (biotite) which confirms the considerable difference in magnetic properties for the components in ore minerals and the possibility of using magnetic separation. Using high-gradient magnetic separation (VGMS) it is possible to effectively separate weakly magnetic minerals-with a specific magnetic susceptibility of (200-100) centre dot 10~(-9) m~3/kg within particle sizes from 0.8-0.6 mm to 30-20 mu m other researchers have reduced this range to 12 centre dot 10~(-9) m~3/kg.
机译:就其磁性而言,所检查的稀有金属矿石中的矿物基本上可以分为弱磁性和非磁性。图1显示了它们的特定磁化率值(x)的光谱。显而易见,矿石矿物百分比变化范围从-0.35中心点10〜(-9)m〜3 / kg(冰晶石)到68.0中心点10〜(-9)m〜3 / kg(黑云母) )证实了矿石中各组分的磁性之间存在相当大的差异,并证实了使用磁选的可能性。使用高梯度磁分离(VGMS)可以有效分离弱磁性矿物-在0.8-0.6的粒径范围内,磁化率的特定磁化率为(200-100)中心点10〜(-9)m〜3 / kg毫米到30-20微米其他研究人员将该范围减小到12个中心点10〜(-9)m〜3 / kg。

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