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曾广圣, 欧乐明. X射线衍射-扫描电镜等技术研究秘鲁铜硫矿石选矿工艺矿物学特征[J]. 岩矿测试, 2019, 38(2): 160-168. DOI: 10.15898/j.cnki.11-2131/td.201804130042
引用本文: 曾广圣, 欧乐明. X射线衍射-扫描电镜等技术研究秘鲁铜硫矿石选矿工艺矿物学特征[J]. 岩矿测试, 2019, 38(2): 160-168. DOI: 10.15898/j.cnki.11-2131/td.201804130042
Guang-sheng ZENG, Le-ming OU. Study on Mineralogical Characteristics of Peru Copper-Sulphur Ore Dressing Process by X-ray Diffraction and Scanning Electron Microscope[J]. Rock and Mineral Analysis, 2019, 38(2): 160-168. DOI: 10.15898/j.cnki.11-2131/td.201804130042
Citation: Guang-sheng ZENG, Le-ming OU. Study on Mineralogical Characteristics of Peru Copper-Sulphur Ore Dressing Process by X-ray Diffraction and Scanning Electron Microscope[J]. Rock and Mineral Analysis, 2019, 38(2): 160-168. DOI: 10.15898/j.cnki.11-2131/td.201804130042

X射线衍射-扫描电镜等技术研究秘鲁铜硫矿石选矿工艺矿物学特征

Study on Mineralogical Characteristics of Peru Copper-Sulphur Ore Dressing Process by X-ray Diffraction and Scanning Electron Microscope

  • 摘要: 秘鲁铜硫矿石的主要回收对象是铜和硫矿物,由于铜矿物嵌布复杂、粒度过细以及与各种脉石矿物或金属矿物交生关系紧密,利用传统工艺矿物学研究方法如化学分析、光学显微镜检测等较难准确定量其工艺矿物学参数。本文采用化学分析、X射线衍射、扫描电镜、偏光显微镜及矿物参数自动分析系统(MLA)等技术手段,研究秘鲁铜硫矿石的化学成分、矿物组成和主要矿物的嵌布特征、粒度分布及单体解离特性等,并对影响选矿指标的主要矿物学因素进行分析。结果表明:矿石中主要元素为Cu(0.65%)和S(9.53%)。矿石中黄铁矿(16.57%)含量较高,形态较为规则,与其他矿物之间的交生关系相对简单,粒度普遍偏粗,其中粒径大于0.30mm的黄铁矿占95.06%。铜矿物主要以不规则粒状、皮壳状、网脉状、纤维状、尘粒状、斑点状分布于脉石中或与黄铁矿、闪锌矿、磁铁矿等金属矿物交生紧密,粒度极不均匀,使得铜矿物解离难度加大,且矿石中云母(12.51%)、绿泥石(3.74%)、滑石(3.34%)、高岭石、蒙脱石(3.59%)等黏土质矿物含量较高,在磨矿过程中易发生泥化从而恶化分选环境。根据该类型矿石的工艺矿物学特性,本文建议采用"粗磨-部分优先浮铜-铜硫混浮-混合精矿再磨再选分离"的工艺流程,可得到质量高的铜、硫精矿。

     

    Abstract:
    BACKGROUNDThe main recovered minerals of copper sulfur ores in Peru were copper minerals and sulfur minerals. Due to the complexity of the embedded copper minerals, the superfine granularity of copper minerals and their close relationship with various gangue or metal minerals, the traditional process mineralogy research methods, such as chemical analysis and optical microscope detection, were difficult to quantify their process mineralogical parameters accurately.
    OBJECTIVESTo systematically investigate the process mineralogy of copper-sulfur ore in Peru.
    METHODSBy means of chemical analysis, X-ray Diffraction, Scanning Electron Microscope, Polarizing Microscope and Mineral Liberation Analysis, the systematic process mineralogy of copper-sulfur ores including chemical composition, mineral composition, occurrences of main minerals, particle size distribution and monomer dissociation characteristics were investigated, and the main mineralogical factors affecting the mineral dressing index were analyzed.
    RESULTSThe main elements in the ore were Cu (0.65%) and S (9.53%). The content of pyrite (16.57%) in the ore was relatively high, and its morphology was regular. The relationship between pyrite and other minerals was relatively simple, and the particle size was generally coarse. Pyrite particle size larger than 0.30mm accounted for 95.06%. However, the copper minerals were mainly irregular granular, shell shaped, reticulated, fibrous, dust-like, and speckled in gangue minerals or intersected with pyrite, sphalerite, magnetite and other metal minerals. The uneven particle size of copper minerals makes the dissociation of copper minerals more difficult. Moreover, the contents of clay minerals such as mica (12.51%), chlorite (3.74%), talc (3.34%), kaolinite and montmorillonite (3.59%) were abundant in the ore. During grinding, mudding occurred easily, which worsened the separation environment.
    CONCLUSIONSThe mineral processing flowsheet of coarse grinding-partially preferred floating copper-copper sulfur mixed flotation-mixed concentrate regrinding and separation can be used in copper-sulfur ore of Peru.

     

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