BACTERIAL LEACHING OF BALANCED ORES OF ALBITITE DEPOSITS OF THE UKRAINIAN SHIELD

IF 0.5 Q4 MINERALOGY
V. Verkhovtsev, O.G. Musich, Yu.O. Fomin, Y. Demikhov
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引用次数: 0

Abstract

Prospects for increasing the raw materials resources of uranium ore deposits of the albite formation of the Ingul megablock of the Ukrainian Shield and the possibility of reducing the impact of harmful waste due to the method of bacterial leaching of metals were considered. Mineral-forming systems of uranium-bearing albitites of the Ukrainian Shield have always been considered as monoelement, exclusively uranium objects. However, their out-of-balance ores and tailings contain elevated, up to industrial, concentrations of other metals, which, under conditions of hypergenic processes, pose a potential threat of environmental pollution. In order to determine the possibility of expanding raw materials resources of albite deposits of the Ukrainian Shield due to the use of the method of bacterial leaching of metals, the composition of industrial ores and host rocks was considered. In particular, our data from their mineralogical and geochemical research showed that uranium and five of its companion elements: thorium, vanadium, beryllium, zirconium and lead reach industrial content. At the same time, cobalt, nickel and zinc are characterized by an increased content close to the minimum industrial values. The most promising for bacterial leaching are rocks that contain sulfides. The rocks of the uranium ore albitite formation contain sulfur-containing compounds and, in particular, pyrite, as well as bi- and trivalent iron. We found the highest content of sulfides in albitized rocks (up to 0.82%), ore-free albitites (up to 0.81%), low-ore albitites (up to 0.61%), that is, in rocks accumulated in industrial waste. It is assumed that the use of bacterial leaching methods with the participation of chemolithotrophic microorganisms can be promising for the processing of off-balance ores and will contribute to the expansion of the raw material base of albite deposits of the Ukrainian Shield, due not only to uranium, but also to nickel, cobalt and zinc.
细菌浸出平衡矿石的乌克兰盾的钠长石矿床
讨论了增加乌克兰地盾英古尔巨型岩钠长石地层铀矿床原料资源的前景,以及减少细菌浸出金属方法造成的有害废物影响的可能性。乌克兰地盾含铀钠长石的矿物形成系统一直被认为是单元素的,完全是铀物体。然而,它们的不平衡矿石和尾矿含有其他金属的高浓度,达到工业浓度,在高成因过程的条件下,构成环境污染的潜在威胁。为了确定利用细菌浸出金属方法扩大乌克兰盾区钠长石矿床原料资源的可能性,考虑了工业矿石和主岩的组成。特别是,我们从他们的矿物学和地球化学研究中获得的数据表明,铀及其五种伴体元素:钍、钒、铍、锆和铅达到工业含量。与此同时,钴、镍和锌的含量增加,接近最低工业值。细菌浸出最有希望的是含有硫化物的岩石。铀矿石钠长岩地层的岩石含有含硫化合物,特别是黄铁矿,以及双价和三价铁。我们发现硫化物含量最高的是钠长岩(高达0.82%)、无矿钠长岩(高达0.81%)、低矿钠长岩(高达0.61%),即在工业废料中堆积的岩石中。据推测,在化学岩石营养微生物的参与下,使用细菌浸出方法处理不平衡的矿石是有希望的,并将有助于扩大乌克兰盾钠长石矿床的原料基础,不仅是铀,而且还有镍、钴和锌。
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CiteScore
0.70
自引率
0.00%
发文量
18
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