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| Determining the Leaching Range of In-situ Uranium Mining by Numerical Simulation |
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Received:November 21, 2022
Revised:November 27, 2022
Accepted:November 28, 2022
Published Online:March 17, 2023
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| DOI:doi:10.3969/j.issn.1007-7545.2023.04.005 |
| KeyWord:leaching range; hydrodynamic field; solute transport; path line |
| Author | Institution |
| WU Hui |
东华理工大学水资源与环境工程学院 |
| LUO Yue |
东华理工大学核资源与环境国家重点试验室 |
| LI Xun |
东华理工大学水资源与环境工程学院 |
| LIU Jin-hui |
东华理工大学核资源与环境国家重点试验室 |
| WANG Bing |
东华理工大学水资源与环境工程学院 |
| CHEN Qian-qian |
江西省勘查设计研究院有限公司 |
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| Abstract: |
| The determination of leaching range is an important part of acid in-situ uranium leaching process. Taking a uranium mining area in Inner Mongolia as an example, based on the hydrodynamic model and solute transport model, the leaching range was determined by pH<2, hydraulic gradient tending to natural flow field, and path line cumulative flow contribution rate is more than 97%, respectively. The leaching range determined under the three conditions is compared and analyzed. The following results can be obtained: 1) The solution leaching range determined by the three methods is close to that of uranium ore, which can be used to characterize the solution leaching range. 2) There are some differences between the edge position of the three methods and the dissolution range of uranium ore, among which the pH delineation range is the closest. 3) The operation with pH<2 as the standard is less difficult, and the data processing of the other two methods is more complex. It is considered that pH<2 is the most suitable for characterizing the leaching range. |
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