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Factors influencing the release rate of uranium, thorium, yttrium and rare earth elements from a low grade ore

机译:影响低品位矿石中铀,or,钇和稀土元素释放速率的因素

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This paper presents data from laboratory leaching of a mineralogically complex low grade ore containing uranium (U), thorium (Th), yttrium (Y), rare earth elements (REEs) and accessory pyrite. The study examines the influence of varying the leaching protocol on the rate of release of U, Th, Y and REEs. Leaching protocols were designed to simulate a range of heap/in situ stope leaching scenarios. Protocol variants included flushing frequency, leachate recycle, nutrient (9 K salts) addition and ferric sulphate addition to cells. Maximum extractions over 52 weeks were: 58% U, 50% Th, 36% Y and 45% of the REEs; observed in cells flushed fortnightly with a ferric sulphate lixiviant (0.5 g/1, pH 3.5). Flushing with tap water once monthly resulted in second highest observed extractions (57% U, 6% Th, 27% Y, 37% REEs) with the exception of Th, where the lower release was due to insufficiently low pH for Th mobilisation. Pourbaix plots indicate that redox potentials within the leaching system were buffered by coffinite dissolution. The high redox potentials, acidic pH and elevated sulphate concentrations required for metals dissolution were found to be a consequence of (a) direct addition of ferric sulphate as a lixiviant or (b) in situ generation of acidity and ferric sulphate via microbially-mediated oxidation of accessory pyrite. Generation and maintenance of acidic sulphate-rich interstitial water appear to control the dissolution of Th, Y and REEs in addition to U. The presented data highlight that significant U, Th, Y and REEs can be mobilised from rock materials by the addition of a ferric sulphate lixiviant, furthermore periodic flushing with water alone is sufficient to achieve similar release of U, Y and REEs where accessory pyrite is available in the reacting system. These findings have significant implications for recovery of valuable elements from low grade and marginal ores or materials previously considered as wastes.
机译:本文介绍了矿物学上复杂的低品位矿石的实验室浸出数据,该矿石包含铀(U),or(Th),钇(Y),稀土元素(REEs)和黄铁矿。该研究检查了不同的浸出方案对U,Th,Y和REE释放速率的影响。浸出协议旨在模拟一系列堆/原位采场浸出方案。协议的变体包括冲洗频率,浸出液再循环,向细胞中添加营养物(9 K盐)和硫酸铁。在52周内最大提取量为:稀土元素含量分别为58%U,50%Th,36%Y和45%。在每两周用硫酸铁浸液剂(0.5 g / 1,pH 3.5)冲洗的细胞中观察到每月一次用自来水冲洗导致观察到的提取量第二高(57%的U,6%的Th,27%的Y,37%REEs),但Th除外,其中较低的释放是由于Th迁移的pH值不足。 Pourbaix图表明浸出系统内的氧化还原电势被有限溶解所缓冲。发现金属溶解所需的高氧化还原电势,酸性pH和升高的硫酸盐浓度是由于(a)直接添加硫酸铁作为浸出剂或(b)通过微生物介导的氧化原位产生酸度和硫酸铁的结果黄铁矿。富含酸性硫酸盐的间隙水的产生和维持似乎可以控制除U之外的Th,Y和REE的溶出。现有数据突出表明,通过添加岩石,可以从岩石中调集大量的U,Th,Y和REE。硫酸铁浸滤剂,此外仅用水定期冲洗就足以实现U,Y和REE的类似释放,而在反应系统中可以使用辅助黄铁矿。这些发现对于从低品位和边缘矿石或以前被视为废物的材料中回收有价值的元素具有重要意义。

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