渝东某沉积型铁矿工艺矿物学研究

    Process Mineralogy of a Sedimentary Iron Ore in Eastern Chongqing

    • 摘要: 【目的】探究渝东某沉积型铁矿的工艺矿物学特征,明确矿石铁赋存状态、矿物嵌布规律及热失重特性,判断常规选矿可行性并探索焙烧提质方案。【方法】采用 MLA、光学显微镜、X 射线衍射、化学分析、差热 — 热重分析多种检测手段,系统开展矿石物质组成、矿物嵌布特征、结构构造与热失重性能的工艺矿物学实验研究。【结果】①矿石 TFe 品位 35.68%,铁主要赋存于菱铁矿、赤(褐)铁矿,分布率依次为 71.16%、25.27%;②矿石构造包含块状、浸染状、层状构造,结构含它形粒状、斑状、碎屑、反应边、鲕粒结构;③菱铁矿多为 0.1~2.0 mm 团块/不规则脉状,部分包裹 0.01~0.20 mm 氧化铁环边,团粒间充填方解石;赤铁矿呈团粒、不规则细网脉状,粒间填充方解石集合体;④菱铁矿 FeO 均值 58.093%,伴生镁、锰杂质,矿物团块粒度差异大;⑤矿石焙烧失重率超 20%,焙烧可提升铁理论品位。【结论】该铁矿矿物粒度不均、伴生碳酸盐杂质,常规选矿难以产出合格铁精矿;焙烧工艺可改善矿石可选性,具备制备合格铁精矿的潜力。

       

      Abstract: Objective To investigate the process mineralogical properties of sedimentary iron ore from eastern Chongqing, clarify the iron occurrence state, mineral intercalation characteristics and thermal weight loss performance of the ore, evaluate the feasibility of conventional beneficiation, and explore the potential of roasting for iron grade upgrading. Methods Multiple testing and analytical methods including MLA, optical microscopy, X-ray diffraction, chemical analysis, and simultaneous differential thermal-thermogravimetric analysis (DTA-TG) were adopted to systematically analyze the material composition, mineral embedding features, ore textures and structures, as well as thermal weight loss behaviors of the target iron ore. Results The total iron (TFe) grade of the ore is 35.68%. Iron elements mainly reside in siderite and hematite (limonite), with distribution ratios of 71.16% and 25.27% respectively, which are the primary recoverable iron-bearing phases. The ore develops massive, disseminated and layered structures, along with allomorphic granular, porphyritic, clastic, reaction rim and oolitic textures. Most siderite occurs as lumpy or irregular vein aggregates ranging from 0.1 mm to 2.0 mm in size; partial siderite lumps are wrapped by iron oxide reaction rims with variable thickness of 0.01~0.20 mm, and intergranular spaces are filled with calcite. Hematite exists as granular aggregates with uneven particle sizes cemented by calcite aggregates, and also distributes as irregular fine reticular veins in the ore. The average FeO content of siderite reaches 58.093%, accompanied by minor impurities such as magnesium and manganese. In addition, the granularity of major mineral aggregates varies greatly. The ore achieves a weight loss rate over 20% after roasting, which can significantly raise the theoretical iron grade. Conclusions Due to uneven granularity of valuable minerals and carbonate impurities, qualified iron concentrate cannot be produced via conventional mineral separation. Roasting treatment can modify the ore’s beneficiability and has promising prospects for producing qualified iron concentrate.

       

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