首页> 外文会议>International Conference on Rare Earth Research and Application; 20060625-30; Beijing(CN) >Separation and Enrichment of Rare Earth Elements in Phosphorite in Xinhua, Zhijin, Guizhou
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Separation and Enrichment of Rare Earth Elements in Phosphorite in Xinhua, Zhijin, Guizhou

机译:贵州治金新华市磷矿中稀土元素的分离富集

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The phosphorite ores-deposits rich in rare earth elements (REE) in Zhijin, Xinhua, Guizhuo occurs in the early Cambrian Meishucun and at the bottom part of Qiongzhusi stage (the upper layer of phosphorites), belonging to Yangzi stratum section. The living creature scraps was proved existent in dolomitic-phosphorites by experiments, The REE could be extracted to provide the worthy data for the further using. Adopting the HNO_3 to extract REE, through the ion exchange method, the REE recovery rate could be reached 85.44 % , having certain reference value.
机译:芝金,新华,桂卓地区富含稀土元素(REE)的磷矿床,发生在寒武纪梅寿村和and竹寺期末(磷矿的上层)的底部,属于扬子地层。实验证明,该生物碎片存在于白云岩中,可以提取稀土元素,为进一步的利用提供有价值的数据。采用HNO_3萃取稀土元素,通过离子交换法,稀土元素的回收率可达到85.44%,具有一定的参考价值。

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