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金属矿山 ›› 2026, Vol. 55 ›› Issue (9): 182-187.

• 矿物工程 • 上一篇    下一篇

营口大石桥某菱镁矿石工艺矿物学研究

马 琨1,2 ,代淑娟1,3 ,李鹏程3 ,刘子源1 ,刘亦政3 ,张 一3   

  1. 1.辽宁科技大学化学工程学院,辽宁 鞍山 114051;2.辽宁科技学院资源与土木工程学院,辽宁 本溪 117004; 3.辽宁科技大学矿业工程学院,辽宁 鞍山 114051
  • 出版日期:2026-09-15 发布日期:2026-10-15
  • 通讯作者: 代淑娟(1967—),女,教授,博士,博士研究生导师。
  • 作者简介:马 琨(1990—),女,讲师,博士研究生。
  • 基金资助:
    辽宁省重点研发项目(编号:2024JH2/102400013)。

Process Mineralogy Research on a Magnesite Ore in Dashiqiao,Yingkou

MA Kun1,2 ,DAI Shujuan1,3 ,LI Pengcheng3 ,LIU Ziyuan1 ,LIU Yizheng3 ,ZHANG Yi3   

  1. 1.School of Chemical Engineering,University of Science and Technology Liaoning,Anshan 114051,China; 2.School of Resources and Civil Engineering,Liaoning Institute of Science and Technology,Benxi 117004,China; 3.School of Mining Engineering,University of Science and Technology Liaoning,Anshan 114051,China
  • Online:2026-09-15 Published:2026-10-15

摘要: 针对营口大石桥某堆存菱镁矿石高硅高钙的特点,采用X射线衍射(XRD)仪、X射线荧光光谱(XRF) 仪及矿物自动分析系统(AMICS)等测试手段,对矿石进行了系统的工艺矿物学研究,分析了矿石的化学成分、矿物组 成、结构构造、嵌布特征、单体解离度、连生特性及粒度分布,旨在为后续选别提纯提供指导。结果表明:矿石中MgO 含量为95.69%,CaO和SiO2 含量分别为1.89%和1.72%,属高硅高钙型菱镁矿;钙元素主要赋存于白云石中,硅元素 分布于镁铝榴石、石英、角闪石和斜绿泥石中。菱镁矿以单体形式为主,占比95.98%,在解离度≥90%级别内的累计 分布率达97.38%,粒度较粗(+74 μm占73.45%);脉石矿物多呈细粒浸染状包裹体,与菱镁矿连生关系紧密,且易泥 化。含硅脉石矿物种类多、可浮性差异大,给浮选脱硅带来困难;白云石与菱镁矿物理化学性质和晶体结构相似,浮选 分离亦较困难。基于工艺矿物学分析结果,采用粗磨—脱泥—单一反浮选流程进行初步探索试验,可获得MgO含量 97.91%、SiO2 含量0.17%、CaO含量1.54%的菱镁矿精矿。研究结果可为后续浮选条件优化试验提供依据。

关键词: 菱镁矿 , 工艺矿物学 , 矿物自动分析系统 , 脱泥 , 反浮选

Abstract: In view of the high-silicon and high-calcium characteristics of a stockpiled magnesite ore from Dashiqiao, Yingkou,a systematic process mineralogy study was conducted using X-ray diffraction (XRD),X-ray fluorescence (XRF),and Automatic Mineral Identification and Characterization System (AMICS).The chemical composition,mineral composition,tex ture and structure,dissemination characteristics,liberation degree,intergrowth characteristics,and particle size distribution of the ore were analyzed to provide guidance for subsequent beneficiation and purification.The results show that the ore contains 95.69% MgO,1.89% CaO,and 1.72% SiO2 ,indicating a high-silicon and high-calcium magnesite.Calcium predominantly oc curs in dolomite,while silicon is distributed in pyrope,quartz,amphibole,and clinochlore.Magnesite is mainly in liberated form,accounting for 95.98%,with a cumulative liberation degree of 97.38% at the level above 90%,and has a relatively coarse particle size (73.45% above 74 μm).Gangue minerals mostly occur as fine-grained disseminated inclusions,closely in tergrown with magnesite,and are prone to sliming.The diversity and varying floatability of silicon-bearing gangue minerals cause difficulties in desilication by flotation;Moreover,the similar physicochemical properties and crystal structures of dolomite and magnesite make their flotation separation challenging.Based on the process mineralogy results,a preliminary flotation test using a rough grinding,desliming and single reverse flotation flowsheet was carried out,yielding a magnesite concentrate with 97.91% MgO,0.17% SiO2 ,and 1.54% CaO.The findings can provide a basis for the subsequent optimization of flotation con ditions.

Key words: magnesite,process mineralogy,automatic mineral identification and characterization system,desliming,re verse flotation

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