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模拟多组分离子交换和扩散过程的反应溶液运输,用富含粘土的岩石进行柱体实验
Marie Hedayati1, Roger Herbert1, Yvonne Tsang2
1Uppsala University, Geocentrum, Villavägen 16, 752 36 Uppsala, Sweden.
粘土石通过离子交换和扩散有效地固定了危险元素,如Cs,Pb和Eu,这对于核废物处理至关重要. 了解这些过程可以确保更安全的制和迁移建模.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 核废物管理 核废物管理
背景情况:
- 粘土是核废弃物处理中的重要自然障碍,因为其透率低,吸附率高.
- 了解富含粘土岩石中的污染物运输和吸附对于经过验证的长期安全模型至关重要.
研究的目的:
- 为了研究伍德福德粘土石中的17种离子化合物的反应运输和吸收.
- 使用反应式运输建模验证实验数据.
主要方法:
- 在柱体实验中,将多标记剂溶液注入到压碎的粘土石中.
- 流中断方法用于研究在扩散主导的质量转移期间的动态行为.
- 使用 TOUGHREACT V4.0 OMP 进行反应式运输建模,采用附带扩散单孔性模型.
主要成果:
- 离子交换,扩散和向导是离子度变化的主要驱动因素.
- 矿氧化和酸盐气候导致Si,Al和Fe的释放和沉.
- 伍德福德粘土石通过离子交换有效吸附Cs,Pb和Eu.
结论:
- 单孔性模型精确模拟了反应性传输,但高估了扩散.
- 考虑静止水的双孔性模型可以提供更精确的模拟.
- 研究结果支持使用粘土石作为核废弃物处理中的障碍物,突出了关键的固定机制.
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