首页|伊犁盆地蒙其古尔砂岩型铀矿床中性CO2+O2地浸中铀的赋存状态变化特征及其规律

伊犁盆地蒙其古尔砂岩型铀矿床中性CO2+O2地浸中铀的赋存状态变化特征及其规律

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自我国采用CO2+O2中性地浸工艺采铀后,一定程度上解决了高碳酸盐矿床采用酸法和碱法地浸导致的堵塞和浸出率低的问题.新疆蒙其古尔铀矿床是我国采用CO2+O2中性浸出方法的代表性高碳酸盐砂岩型铀矿床之一.本研究以蒙其古尔铀矿床原矿石为研究对象开展室内铀浸出实验,并对浸出前后的样品磨制薄片进行TIMA自动矿物扫面以及扫描电镜分析,以查明矿石浸出前后铀赋存状态以及铀矿物粒度、解离度和连生矿物等工艺参数的变化,为改进采铀工艺提供矿物学参数依据.结果表明蒙其古尔铀矿床原矿石中铀的存在形式主要为独立铀矿物、含铀矿物和吸附态铀.铀矿物主要为铀石,以及少量的沥青铀矿.相比于浸出前,浸出后铀石、沥青铀矿均被大量浸出,大于30 µm的铀石被浸出完全,沥青铀矿仅剩少量8~9μm的未被浸出.铀石的解离度在浸出前后最大的变化是小于10%的占比从49.68%变为84.20%.相比于铀石,原矿石中沥青铀矿的解离度更高,在80%~90%解离度范围内的占比达53.06%,浸出后仅有少量60%~70%解离度的沥青铀矿未被浸出.研究表明解离度较大的铀矿物比解离度较小的更易被浸出,沥青铀矿相对于铀石更易被浸出.浸出过程中需要控制好浸出体系的pH,阻止含铀方解石的二次沉淀.本研究查明了浸出前后铀赋存状态以及铀矿物的工艺参数的变化特征,有助于研究影响矿石地浸效率的各种因素,对推动蒙其古尔以及我国类似铀矿床地浸开采技术的完善与创新具有重要的理论和现实意义.
CHANGES OF URANIUM OCCURRENCE STATE IN NEUTRAL CO2+O2 IN-SITU LEACHING IN THE MENGQIGUER SANDSTONE-TYPE URANIUM DE-POSIT IN YILI BASIN
The implementation of the CO2+O2 neutral leaching process for uranium extraction in our country has,to some extent,mitigated the challenges associated with blockage and low leaching rates that were prevalent with acid and alkali leaching methods in high-carbonate uranium deposits.The Monqiguer Uranium Deposit in Xinjiang is one of the representative high-carbonate sandstone-type uranium deposits in China,employing this leaching method.The focus of this paper is on a laboratory uranium leaching exper-iment to raw ore from the Mengqiguer uranium deposit,utilizing TESCAN Integrated Mineralogy Analy-sis(TIMA)and Scanning Electron Microscope(SEM)to analyses thin slices of samples,to illustrate changes in process parameters like uranium occurrence states,uranium mineral size,dissociation degree,and associated minerals before and after leaching.This comprehensive analysis aims to provide mineralogi-cal parameters as a basis for improving the uranium mining process.The results indicate that uranium pri-marily exists in independent uranium minerals,uranium-bearing minerals,and adsorbed uranium in the raw ore of the Mengqiguer uranium deposit.The predominant uranium minerals are identified as coffinite with a small amount of pitchblende.After the uranium ore leaching experiment,a significant amount of coffinite and pitchblende are successfully leached,with coffinite larger than 30 μm being completely leached,and only a small amount of pitchblende(8-9 μm)remaining unleached.The most notable change in the dissociation degree of coffinite before and after leaching is the proportion of less than 10%,which increases from 49.68%to 84.20%.Pitchblende in the raw ore exhibits a higher dissociation degree,accounting for 53.06%in the range of 80%-90%dissociation degrees.Only a small amount of pitch-blende with a 60%-70%dissociation degree remains unleached after leaching.Generally,uranium miner-als with higher dissociation degrees are more easily leached than those with lower dissociation degrees,and pitchblende is more susceptible to leaching compared to coffinite.Throughout the leaching process,it is crucial to control the pH of the leaching system to prevent the secondary precipitation of uranium-bearing calcite.The findings of this study regarding the occurrence state of uranium and the change characteristics of process parameters for uranium minerals before and after leaching contribute to understanding various factors influencing in-situ ore leaching efficiency.This information holds important theoretical and practi-cal significance for advancing the improvement and innovation of in-situ leaching technology at the Mengqiguer uranium deposit and similar uranium deposits in China.

Sandstone-type uranium depositsCO2+O2 neutral leachingTIMAOccurrence state

于慧杰、宋昊、王泽鑫、范元清、李梅、杜钱敏、张成江、谭亚辉

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成都理工大学,四川成都 610059

地质灾害防治与地质环境保护国家重点实验室,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

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砂岩型铀矿 CO2+O2中性浸出 TIMA 赋存状态

国家自然科学基金国家自然科学基金成都理工大学珠峰科学研究计划

42173072U19672072021ZF11413

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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