首页|钱家店砂岩型铀矿床铀矿物嵌布特征及对中性(CO2+O2)地浸采铀效率的影响

钱家店砂岩型铀矿床铀矿物嵌布特征及对中性(CO2+O2)地浸采铀效率的影响

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可地浸砂岩型铀矿中铀矿物的空间嵌布特征直接影响其与溶浸剂的接触反应程度,厘清铀矿物浸出过程中的嵌布变化规律对于综合提高铀的浸出率至关重要.基于此,本研究采集了钱家店砂岩型铀矿床Ⅳ号矿段样品,进行了室内浸出实验并对中性浸出反应前后矿样进行了 SEM-EDS镜下观察、以及TESCAN综合矿物分析等表征手段,定量分析了浸出前后铀矿物嵌布、解离度、连生矿物和粒度变化特征.结果表明:(1)钱家店砂岩型铀矿床独立铀矿物主要以沥青铀矿为主,以及少量铀石,完全被包裹的沥青铀矿和铀石解离度分别由61.06%~68.17%增加至83.45%、由46.88%~58.27%增加至65.22%,指示沥青铀矿的解离度参数变化程度明显大于轴石,说明沥青铀矿更易发生氧化溶解.(2)沥青铀矿和铀石多呈现6~12 µm、4~10μm粒径范围与长石、石英、黄铁矿、云母、黏土矿物连生,而这些连生的矿物多呈现包裹铀矿物的状态使铀矿物难以与溶浸液接触反应.(3)浸出之后,可见石英长石碎屑颗粒内部还残留有大量铀矿物,并且其边缘发现有小颗粒(5 μm)铀石残余,指示CO2+O2浸出条件下完全被包裹的铀矿物很难被浸出,并且呈现出沥青铀矿>铀石的优先浸出规律.本研究成果指示了应重点关注与铀矿物有空间嵌布和连生关系的矿物在CO2+O2地浸采铀过程中的地球化学性质和对地浸的影响,以及为针对性地配置溶浸剂(尝试添加额外绿色无污染的H2O2)以溶解氧化较难溶解的铀矿物(如铀石)提供了新的依据.
THE OCCURRENCE CHARACTERISTICS OF URANIUM MINERALS IN QIANJIADIAN SANDSTONE-TYPE URANIUM DEPOSIT AND ITS EFFECT ON EFFICIENCY OF NEUTRAL(CO2+O2)IN-SITU LEACHING OF URANI-UM
The occurrence characteristics of uranium minerals in leachable sandstone-type uranium ore di-rectly influence their contact chemical reaction with the leaching agent.Therefore,it is crucial to elucidate the variations in the distribution of uranium minerals during the leaching process to comprehensively en-hance the leaching rate of uranium.In this study,samples from the IV ore section of the Qianjiadian sand-stone-type uranium deposit were collected for laboratory leaching experiments.Observations using the SEM-EDS microscope and TESCAN Integrated Mineralogy Analysis were con-ducted to quantitatively analyze the characteristics of uranium mineral distribution,dissociation degree,associated minerals,and particle size changes before and after the leaching reaction.The results indicate that the independent uranium minerals in the Qianjiadian sandstone-type uranium deposit are primarily composed of pitchblende with a small amount of coffinite.The dissociation of completely enveloped pitch-blende and coffinite increases from 61.06%to 68.17%and from 46.88%to 58.27%,respectively.This suggests that the change in the dissociation parameter of pitchblende is significantly greater than that of coffinite,indicating that pitchblende is more prone to oxidation dissolution.The particle sizes of pitch-blende and coffinite are mostly in the range of 6 to 12 μm and 4 to 10 μm,respectively,and are associated with feldspar,quartz,pyrite,mica,clay minerals,etc.,which typically act as coating materials on urani-um minerals,creating difficulties for uranium minerals to contact and react with the leaching solution.Af-ter leaching,a substantial number of uranium minerals remain inside the detrital particles of quartz and feldspar.Only small particles(5 μm)of coffinite remain at the edges of these associated particles,indica-ting that fully coated uranium minerals are challenging to leach under CO2+O2 leaching conditions.Addi-tionally,the leaching experiment shows that the leaching effect of pitchblende is higher than that of coffin-ite.This study's results have revealed the geochemical properties of uranium minerals,and their spatial distribution and co-occurrence relationships to the associated minerals affect the U leaching efficiency dur-ing the CO2+O2 in-situ leaching.It provides a new insight for the targeted allocation of leaching agents,such as the addition of environmentally friendly H2O2,to dissolve and oxidize insoluble uranium minerals,such as coffinite.

Qianjiadian sandstone type uranium depositCO2+O2 leachinguranium mineralsoccur-rence characteristics

范元清、宋昊、张成江、谭亚辉、李圻、梁研

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成都理工大学,四川 成都 610059

地学核技术四川省重点实验室,四川成都 610059

核工业北京化工冶金研究院,北京 101149

钱家店砂岩型铀矿 CO2+O2浸出 铀矿物 嵌布特征

国家自然科学基金

U1967207

2024

矿物岩石
四川省矿物岩石地球化学学会 成都理工大学

矿物岩石

CSTPCD北大核心
影响因子:0.8
ISSN:1001-6872
年,卷(期):2024.44(1)
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