云南镇雄羊场磷矿磷块岩工艺矿物学研究(磷矿专辑)
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1.云南省地质调查院;2.自然资源部三江成矿作用及资源勘查利用重点实验室;3.云南省三江成矿作用及资源勘查利用重点实验室

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云南省地质勘查(K202201、K202301、Y202301)资助。第一作者:黄太平(1986-),男,大学本科,资源勘查工程专业。E-mail:523917202@qq.com。通讯作者:周 骞(1989-),男,工程师,主要从事矿产勘查与研究工作。E-mail:525396727@qq.com。 ,2,3,周骞1,2,3,米云川1,2,3,胡清华1,夏建峰1


Study on process mineralogy of the phosphorite in Yangchang phosphate deposit, Zhenxiong, Yunnan Province
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1.Yunnan Geological Survey Institute,Kunming,Yunnan,;2.Key Laboratory of Sanjiang Metallogenic Processes and Resource Exploration and Utilization,Ministry of Natural Resources,Kunming,Yunnan,;3.Key Laboratory of Mineralization and Resource Exploration and Utilization in Sanjiang,Yunnan Province,Kunming,;4.China;5.Yunnan Geological Survey Institute,Kunming,Yunnan

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    摘要:

    云南省镇雄县羊场磷矿是近年来发现的早寒武世超大型沉积磷块岩矿床,具“资源储量大、矿石品质优、资源分布集中”的特点,为目前亚洲最大规模隐伏单体富磷矿床。本文采用矿物参数自动定量分析系统(AMICS)、扫描电子显微镜-能谱仪(SEM-EDS)、X射线荧光光谱仪(XRF)、电感耦合等离子体质谱仪(ICP-MS)和偏光显微镜等分析手段,对该矿床磷块岩矿石的化学成分、矿物组成、嵌布特征、主要矿物的粒度和赋存状态及矿物解离度等进行了系统工艺矿物学研究,并提出了相应的矿石分选流程方法。研究表明:矿石属高硅低镁的混合型-碳酸盐型高品位磷块岩矿石,以碳酸盐型为主,矿石矿物为胶磷矿,脉石矿物主要为石英、方解石、白云石及少量黄铁矿等。胶磷矿嵌布粒度较大,因较多颗粒属于解离度大于75%的高自由度状态,较易解离,但单体解离度较低,随破碎程度增加单体解离程度无明显升高趋势。脉石矿物石英、方解石、白云石、黄铁矿等嵌布粒度较小,单体解离度较低,矿物颗粒随着样品破碎程度增加单体解离程度呈明显升高趋势,若需使用选矿方法剔除脉石矿物,需适当增加磨矿时间,以增加其单体解离程度。胶磷矿与石英、方解石、白云石等矿物以两相及多相连生为主。根据矿物组成、粒度分配及矿物连生关系等综合分析,矿石选别时主要脱硅,其次脱镁,建议采用“正浮选”脱硅,如若“正浮选”不能到达磷精矿指标要求或回收率低,则可采用“正-反浮选”先脱硅后脱镁,可获得较好分选效果。

    Abstract:

    The Yangchang phosphate deposit in Zhenxiong County,Yunnan Province is a super large sedimentary phosphate rock deposit discovered in recent years in the Early Cambrian period. It has the characteristics of "large resource reserves, excellent ore quality, and concentrated resource distribution", and is currently the largest hidden single rich phosphate deposit in Asia. This article uses automatic quantitative analysis system for mineral parameters (AMICS), scanning electron microscopy energy dispersive spectroscopy (SEM-EDS), X-ray fluorescence spectrometer (XRF), inductively coupled plasma mass spectrometry (ICP-MS), and polarizing microscope analysis methods to systematically study the chemical composition, mineral composition, embedding characteristics, particle size and occurrence status of major minerals, and mineral dissociation degree of the phosphate rock ore in the deposit. Research has shown that the ore belongs to a typical mixed carbonate type phosphate rock ore, with carbonate type as the main mineral. The ore mineral is collophane, and the vein mineral is mainly quartz, calcite, dolomite, and a small amount of pyrite. The embedded particle size of phosphate rock is relatively large, and many particles belong to a high degree of freedom state with a dissociation degree greater than 75%, which is easy to dissociate. However, the monomer dissociation degree is low, and there is no significant increase in monomer dissociation degree with the increase of fragmentation degree. Vein minerals such as quartz, calcite, dolomite, and pyrite have smaller particle sizes and lower monomer dissociation. The degree of monomer dissociation of mineral particles increases significantly with the increase of sample fragmentation. If mineral processing methods are needed to remove vein minerals, grinding time should be appropriately increased to increase their monomer dissociation degree. Colloidal phosphate ore is mainly associated with minerals such as quartz, calcite, and dolomite in two or multiple phases.Based on comprehensive analysis of mineral composition, particle size distribution, and mineral association, the main method for ore selection is desilication, followed by magnesium removal. It is recommended to use "positive flotation" for desilication. If "positive flotation" cannot meet the requirements of phosphorus concentrate indicators or the recovery rate is low, "positive reverse flotation" can be used for desilication first and then magnesium removal to achieve better separation results.

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  • 收稿日期:2024-05-19
  • 最后修改日期:2024-07-31
  • 录用日期:2024-08-30
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