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金属矿山 ›› 2026, Vol. 55 ›› Issue (7): 140-.

• 矿物工程 • 上一篇    下一篇

攀西地区钒钛磁铁精矿的工艺矿物学研究

米宏成1 李丽匣1 胡厚勤2 张 春2 陈家宽1 王嘉琦1 褚 洋1 杨淑贤1 李思佑1   

  1. 1.东北大学资源与土木工程学院,辽宁 沈阳 110819;2.攀钢集团矿业有限公司,四川 攀枝花 617000
  • 出版日期:2026-07-15 发布日期:2026-08-18
  • 通讯作者: 李丽匣(1980—),女,教授,博士,博士研究生导师。
  • 作者简介:米宏成(1996—),男,博士研究生。
  • 基金资助:
    国家自然科学基金项目(编号:52174243);辽宁省重点研发计划项目(编号:2024 JH2/102400026)。

Research on the Process Mineralogy of Vanadium-Titanium Magnetite Concentrate in Panxi Area

MI Hongcheng1 LI Lixia1 HU Houqin2 ZHANG Chun2 CHEN Jiakuan1 WANG Jiaqi1 CHU Yang1 YANG Shuxian1 LI Siyou1   

  1. 1.School of Resources and Civil Engineering,Northeastern University,Shenyang 110819,China; 2.Pangang Group Mining Company,Panzhihua 617000,China
  • Online:2026-07-15 Published:2026-08-18
  • Supported by:

摘要: 为揭示攀西地区钒钛磁铁精矿的工艺矿物学关键特征,指导选矿提质降杂与工艺优化,采用化学分析、 X射线衍射(XRD)、扫描电子显微镜-能量色散谱(SEM-EDS)及工艺矿物学参数自动测试系统(BPMA),系统研究该 原料的化学成分、矿物组成、嵌布粒度、解离连生特征及Fe、Ti赋存规律。结果表明:试样TFe品位53.62%,TiO2 品位 12.49%,S含量1.10%;钛磁铁矿为绝对主导矿物,含量达86.35%,Fe、Ti在其中的分布率分别高达92.36%和 86.49%,是铁钛综合回收的核心载体。钛磁铁矿以细粒、微细粒嵌布为主,单体与富连生体合计占86.35%,整体解离 条件良好;钛铁矿、榍石、磁黄铁矿等矿物含量低、粒度微细、解离度差,多与钛磁铁矿及钛闪石、绿泥石紧密连生。钛 磁铁矿内部广泛发育钛铁矿固溶体分离结构,是铁精矿中TiO2 难以高效脱除的关键矿物学因素。研究明确了该矿石 “铁钛高度富集、微细粒嵌布、固溶体共生、复杂连生”的核心特性,为攀西同类钒钛磁铁精矿的提质降杂、精准分选及 工艺流程优化提供了直接工艺矿物学依据。

关键词: 钒钛磁铁精矿 , 工艺矿物学 , 矿物组成 , 解离特征 , 连生关系

Abstract: To reveal the key process mineralogical characteristics of vanadium-titanium magnetite concentrate from the Panxi area and provide guidance for beneficiation upgrading,impurity reduction and process optimization,chemical analysis,X ray diffraction (XRD),scanning electron microscopy coupled with energy-dispersive spectroscopy (SEM-EDS),and process mineralogical parameter automatic analysis system (BPMA) were used to systematically investigate the chemical composition, mineral composition,dissemination size,liberation and intergrowth characteristics,as well as the occurrence regularity of Fe and Ti in the sample.The results show that the sample has a total Fe (TFe) grade of 53.62%,TiO2 grade of 12.49%,and sulfur content of 1.10%.Titanomagnetite is the dominant mineral with a content of 86.35%,and the distribution rates of Fe and Ti in it reach 92.36% and 86.49%,respectively,making it the principal carrier for the comprehensive recovery of iron and titanium. Titanomagnetite mainly occurs as fine to ultra-fine disseminated grains,and the sum of free particles and rich intergrowths ac counts for 86.35%,indicating favorable liberation conditions. In contrast,ilmenite,titanite,pyrrhotite and other minerals are characterized by low content,fine particle size and poor liberation degree,and are closely intergrown with titanomagnetite,ti tanian amphibole and chlorite.Widespread ilmenite exsolution textures within titanomagnetite are identified as the key minera logical factor restricting the efficient removal of TiO2 from iron concentrate.This study clarifies the core characteristics of the ore,i.e.,high Fe-Ti enrichment,fine dissemination,solid solution symbiosis and complex intergrowth,and provides a direct process mineralogical basis for quality improvement,impurity reduction,precise separation and process flow optimization of sim ilar vanadium-titanium magnetite concentrates in the Panxi region.

Key words:  vanadium-titanium magnetic concentrate,process mineralogy,mineral composition,dissociation characteris tics,interrelationship

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