稀土元素赋存形态对风化壳淋积型稀土矿提取率的影响

Influence of Rare Earth Occurrence States on Extraction Rate in Weathered Crust Elution-Deposited Rare Earth Ores

  • 摘要: 风化壳淋积型稀土矿中稀土元素的赋存状态十分复杂,目前的工艺仅能提取可交换吸附态的稀土元素,稀土资源未能被有效利用。本文选取中国南方的风化壳淋积型稀土矿样品,采用混合酸消解-电感耦合等离子体质谱法(ICP-MS)对样品中全相稀土量进行分析;采用硫酸铵浸取和顺序提取法对机械研磨前后样品中稀土元素不同赋存状态含量进行研究,探讨了硫酸铵浸出率与稀土元素赋存状态间的关系。研究结果表明:①样品研磨过程会改变稀土元素赋存状态,与未经研磨的样品相比,研磨后的两个样品中稀土元素的硫酸铵浸出率分别降低21.5%和51.6%,离子交换态稀土明显减少,碳酸盐结合态明显增加,铁锰氧化态和腐植酸结合态略有增加;②铈元素(Ce)赋存状态具有特殊的富集-分异特性,主要以铁锰氧化态和残渣态存在,其富集顺序与其他稀土元素明显不同,这也导致了Ce的硫酸铵浸出率以及研磨前后赋存状态变化规律与其他稀土元素存在差异;③除Ce以外,其他稀土元素的浸出率与离子交换态和铁锰氧化态含量之和呈正相关,与碳酸盐结合态和残渣态含量之和呈负相关。离子交换态和铁锰氧化态是可交换吸附稀土的重要来源;碳酸盐结合态和残渣态不贡献可交换吸附稀土,需要考虑采用离子交换之外的方式提取。

     

    Abstract: The occurrence of rare earth elements (REEs) in weathered crust elution-deposited rare earth ore is very complicated, and only the exchangeable adsorption state REEs can be utilized by the current extraction process, demonstrating that the REE resources have not been effectively utilized. Two samples from weathered crust elution rare earth ore in southern China were selected. Total REE contents in samples were analyzed by mixed acid digestion–inductively coupled plasma-mass spectrometry (ICP-MS), occurrence states of REEs were analyzed by ammonium sulfate leaching and sequential extraction, and the relationship between ammonium sulfate leaching rates and REE occurrence states was preliminarily discussed. The results were as follows in three aspects: (1) Grinding altered the occurrence state of REEs; the ammonium sulfate leaching rates of REEs in the two samples after grinding decreased by 21.5% and 51.6%, respectively. The ion-exchange REEs in the samples decreased significantly, while the carbonate-bound state increased significantly. The iron-manganese oxide-bound state and humic acid-bound state increased slightly. (2) The occurrence states of cerium (Ce) exhibit special enrichment-depletion characteristics, mainly existing in iron–manganese oxide-bound and residual states. Its enrichment order is significantly different from that of other REEs, which also leads to differences in the ammonium sulfate leaching rate of Ce and the changes in its occurrence state before and after grinding compared with other REEs. (3) The leaching rate of REEs other than Ce is positively correlated with the sum content of the ion-exchange state and iron–manganese oxide-bound state, and negatively correlated with the sum content of the carbonate-bound state and residual state. The ion-exchange state and iron–manganese oxide-bound state REEs are important sources for exchangeable adsorption of REEs. The carbonate bound state and residual state do not contribute to the exchangeable adsorption of REEs, and extraction methods other than ion exchange should be considered. This study provides technical support for establishing evaluation standards for weathered crust elution-deposited rare earth ores and improving the utilization rate of rare earth resources. The BRIEF REPORT is available for this paper at http://www.ykcs.ac.cn/en/article/doi/10.15898/j.ykcs.202501020002.

     

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