基于多尺度表征的萤石型微细粒白云鄂博尾矿工艺矿物学研究

Study on Process Mineralogy of Fluorite−Type Fine−Grained Bayan Obo Tailings Based on Multi−scale Characterization

  • 摘要: 选取典型高萤石型白云鄂博尾矿,开展了系统的工艺矿物学研究。综合运用化学成分分析、X射线衍射、自动矿物特征定量分析系统、电子探针扫描电镜、矿物解离分析及激光粒度测试等多种表征技术,首次精准揭示了该微细粒尾矿的矿物组成、元素分布与嵌布特性。结果表明,该尾矿矿样中有价元素以CaF2为主,其次为REO,含量分别为45.24%、1.23%;有用矿物以萤石为主,其次为氟碳铈矿和独居石,质量分数分别为37.55%、3.66%和2.70%。矿样粒度微细特征显著,矿样中−74 μm粒级占99.70%,其中−25 μm粒级占79.20%,CaF2和REO分布率分别为78.92%、83.71%。萤石单体解离度较高,为87.96%,多呈半自形~他形粒状结构,但常与重晶石、磷灰石、白云石等脉石矿物致密共生,并普遍包裹稀土矿物,形成复杂空间构型;稀土矿物氟碳铈矿和独居石单体解离度略低于萤石,分别为69.89%和79.43%,主要与萤石连生,局部与脉石矿物形成复杂连生体。上述微细粒特性及复杂嵌布关系导致常规浮选分离困难,本研究为后续开展白云鄂博微细粒尾矿中萤石资源的综合回收利用研究提供了关键的矿物学依据。

     

    Abstract: This study selected typical fluorite−rich Bayan Obo tailings and conducted systematic process mineralogy investigations. By comprehensively employing various characterization techniques, including chemical composition analysis, X−ray diffraction, Advanced Mineral Identification and Characterization System, electron probe scanning electron microscopy, mineral liberation analysis, and laser particle size testing, the mineral composition, elemental distribution, and dissemination characteristics of this ultrafine−grained tailings system were precisely revealed for the first time. The results indicate that the valuable elements in the tailings sample are mainly CaF2, followed by REO, with contents of 45.24% and 1.23%, respectively; The useful minerals are mainly fluorite, with bastnaesite and monazite as secondary components, with mass fractions of 37.55%, 3.66%, and 2.70%, respectively. The ore sample exhibits significant fine particle characteristics, with the −74 μm fraction accounting for 99.70% of the total, and the −25 μm fraction making up 79.20%. The distribution rates of CaF2 and REO are 78.92% and 83.71%, respectively. The fluorite shows a relatively high single dissociation degree of 87.96%, primarily occurring in semi−automorphic to euhedral granular structures. However, it often forms dense associations with gangue minerals such as barite, apatite, and dolomite, and is frequently enveloped by rare earth minerals, resulting in complex spatial configurations. The rare earth minerals, bastnaesite and monazite, have slightly lower single dissociation degrees compared to fluorite, at 69.89% and 79.43%, respectively. These minerals mainly occur in association with fluorite and, in some cases, form complex intergrowths with gangue minerals. The aforementioned fine particle characteristics and intricate dissemination relationships make conventional flotation separation challenging. This study provides critical mineralogical evidence for the comprehensive recovery and utilization of fluorite resources from the Bayan Obo fine−grained tailings in subsequent stages.

     

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