PSL University/Mines ParisTech, Centre de Géosciences, 35 rue Saint-Honoré, 77305 Fontainebleau, France; ORANO Mining, 125 avenue de Paris, 92320 Châtillon, France.
PSL University/Mines ParisTech, Centre de Géosciences, 35 rue Saint-Honoré, 77305 Fontainebleau, France.
J Contam Hydrol. 2023 Mar;254:104106. doi: 10.1016/j.jconhyd.2022.104106. Epub 2022 Nov 17.
Worldwide, most uranium production relies on the 'in situ recovery' (ISR) extraction technique. This consists of dissolving the ore using a leaching solution (acid or alkaline) directly within the deposit through a series of injection and extraction wells. Due to the nature of the injected ISR solutions, the water quality of the aquifer could be affected. Reactive transport modeling is a powerful tool for predicting fluid flow and geochemical reactions in ISR reservoirs. In this study we present a coupled 3D environmental geochemical model (EGM) (based on the HYTEC reactive transport software), capable of predicting the physico-chemical conditions in an acid-leaching ISR uranium mine and its environmental footprint on the aquifer in the years following the closure of the production block. The model was validated at the KATCO mine (Kazakhstan) on two different and independent production blocks, over 10 years after their closure. The model shows that incorporating two main geochemical processes, (1) cationic sorption on clay surfaces (smectite-beidellite) and (2) precipitation of gypsum (CaSO.2HO), successfully reproduces the measured well data (pH, acidity and SO) over short- and long-term time scales. Clay surface sites remain mostly saturated in protons during the production phase. Simulations show that sorbed protons on the clay surfaces maintains the acid conditions for a longer period of time. The environmental impact model was also compared to a pre-existing model specifically developed for production simulation purposes: differences are observed as expected for the uranium production, but also for the impact distances, due to differences in the considered reactive mineralogical paragenesis. Thus, the choice of geochemical model should be made with due regard for the desired objectives. This work will assist the mine operator by providing a tool capable of assessing both the short- and long-term environmental footprints of the ISR production operation conditions and of identifying the best remediation strategy.
在全球范围内,大多数铀生产都依赖于“原地浸出”(ISR)提取技术。该技术包括通过一系列注入和提取井,直接在矿床中使用浸出溶液(酸或碱)溶解矿石。由于注入的 ISR 溶液的性质,含水层的水质可能会受到影响。反应传输建模是预测 ISR 储层中流体流动和地球化学反应的有力工具。在这项研究中,我们提出了一种耦合的 3D 环境地球化学模型(EGM)(基于 HYTEC 反应传输软件),能够预测酸浸 ISR 铀矿的物理化学条件及其在生产块关闭后的几年内对含水层的环境影响。该模型在 KATCO 矿(哈萨克斯坦)的两个不同且独立的生产区块上进行了验证,这些区块在关闭 10 多年后进行了验证。该模型表明,纳入两个主要的地球化学过程(1)阳离子在粘土表面上的吸附(蒙脱石-贝得石)和(2)石膏(CaSO4·2H2O)的沉淀,成功地再现了短期和长期测量井数据(pH 值、酸度和 SO42-)。在生产阶段,粘土表面上的质子仍然主要被质子占据。模拟表明,粘土表面上吸附的质子在更长的时间内保持酸性条件。环境影响模型还与专门为生产模拟目的而开发的现有模型进行了比较:由于考虑的反应矿物共生体不同,预计会出现铀生产的差异,也会出现影响距离的差异。因此,应该根据预期目标选择地球化学模型。这项工作将为矿山运营商提供一种工具,帮助他们评估 ISR 生产作业条件的短期和长期环境影响,并确定最佳的补救策略。