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Solute migration during acid in-situ leach mining of sandstone hosted uranium deposits

机译:酸性原位浸出过程中砂岩患者宿主铀矿床溶质迁移

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Through experiments of solute migration and geochemical simulation, this paper reveals the characteristics and conditions of uranium transport during acid in-situ leaching process. The species and concentration ofuranium are closely related to such hydrogeochemical conditions as pH and Eh values. The predominant uranium species are UO2SO4 and UO22+ for the leaching solution with pH values ranging from 1.9 to 4.4. The uranium concentration increases gradually until reaching saturation with the extension of leaching flow-path.The leaching site is subdivided into six zones according to uranium concentration and hydrogeochemistry.
机译:通过溶质迁移和地球化学模拟的实验,本文揭示了酸原位浸出过程中铀传输的特点和条件。昆虫的物种和浓度与这种水中的条件密切相关,如pH和欧欧元值。浸出溶液的主要铀物种是UO2SO4和UO 2 2 +,pH值范围为1.9至4.4。铀浓浓度逐渐增加,直到延长浸出流动路径达到饱和。根据铀浓度和水力地质化学,浸出部位被细分为六个区域。

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