在断裂花岗岩中建立前露天铀矿地下污染物迁移模型(法国 La Ribière):利用地球物理学减少不确定性

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC ACS Applied Electronic Materials Pub Date : 2024-04-01 DOI:10.1016/j.jconhyd.2024.104343
S. Guillon , J.-F. Girard , E. Williard , D. Virlogeux , M. Descostes
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引用次数: 0

摘要

对原铀矿的尾矿进行长期管理需要深入了解水文地质过程和水流路径。在法国,大多数遗留铀矿都位于断裂结晶(深成岩)岩石中,其固有的地下异质性增加了有关前开采和研磨活动以及停产时矿山状况的不确定性。铀矿石主要通过硫酸浸出法处理,因此产生了高硫酸盐含量的选矿厂尾矿,现存于多个尾矿库(TSF)中。La Ribière 矿址位于法国中西部,曾是一个露天和地下铀矿,于 1992 年关闭,用于储存选矿厂尾矿。该矿址被用作建立工作流程的试验案例,以解释和预测水流和地下污染物的迁移。首先根据现有信息和水文地球化学监测结果,在 La Ribière 流域范围内建立水流和硫酸盐迁移的概念模型。最近的地球物理调查使这一模型得以完善。事实证明,电阻率断层扫描(ERT)不仅能有效定位 U 型磨机尾矿遗留的高传导性硫酸盐羽流的范围,还能对风化剖面进行成像。磁共振探测(MRS)尽管由于结晶岩的孔隙度较低而信号强度有限,但仍能对孔隙度值、断裂层深度和低孔隙度矿石加工泥浆的位置有一定的了解。在这一概念模型的基础上,利用 METIS 代码开发并校准了三维流动和非反应迁移模型。该模型可以预测硫酸盐羽流的演变,也可用于未来的调查,为铀和其他活性污染物建立简化水文地质的活性迁移模型。
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Modeling subsurface contaminant transport from a former open-pit uranium mine in fractured granites (La Ribière, France): Reducing uncertainties with geophysics

The long-term management of tailings from former uranium (U) mines requires an in-depth understanding of the hydrogeological processes and water flow paths. In France, most of the legacy U mines are located in fractured crystalline (plutonic) rocks, where the intrinsic subsurface heterogeneity adds to the uncertainties about the former extraction and milling activities and the state of the mine when production was ceased. U ores were mainly processed by sulfuric acid leaching, leading to high-sulfate-content mill tailings now contained in several tailing storage facilities (TSFs). The La Ribière site, located in western central France, is a former open-pit and underground U mine, closed in 1992 and used to store mill tailings. This site is being used as a test case to establish a workflow in order to explain and predict water flow and subsurface contaminant transport. A conceptual model of water flow and sulfate transport, at the scale of the La Ribière watershed, is first developed based on available information and hydrogeochemical monitoring. Recent geophysical investigations allows refining this model. Electrical Resistivity Tomography (ERT) proves to be efficient at localizing the extent of the highly conductive sulfate plume inherited from the U-mill tailings, but also at imaging the weathering profile. Magnetic Resonance Sounding (MRS), despite the limited signal intensity due to the low porosity in crystalline rocks, gives some insight into the porosity values, the depth of the fractured layer and the location of the low-porosity ore-processing muds. Based on this conceptual model, a 3D flow and non-reactive transport model with the METIS code is developed and calibrated. This model allows predicting the evolution of the sulfate plume, but will also be used in future investigations, to build reactive transport models with simplified hydrogeology for U and other reactive contaminants.

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