相关实验视频
Updated: Jul 12, 2026

08:01
The Diffusion of Passive Tracers in Laminar Shear Flow
Published on: May 1, 2018
颗粒内部扩散:一个重要的机制影响溶液的运输在古典的含水层?
概括
含水层沙中的颗粒内孔隙比以前测量的要大,揭示了更多的反应场所. 这一发现需要将扩散表达式纳入放射性和有毒废物模拟的运输模型.
科学领域:
- 地质地质地质地质地质地
- 环境科学 环境科学
- 水文地质学 水文地质学
背景情况:
- 标准实验室测试低估了含水层沙子中的颗粒内多孔性.
- 含水层的特性显著影响溶液运输和污染物的命运.
研究的目的:
- 为了准确量化沙子大小的含水层物质中的微粒孔隙.
- 评估这种多孔性对溶解物运输和反应动力学的影响.
主要方法:
- 扫描电子显微镜 (SEM) 的使用
- 注射孔径测量方法 注射孔径测量方法
- 光显微镜显微镜是一种光显微镜.
- 实验室和现场的追踪器测试.
主要成果:
- 颗粒内部的多孔性和反应部位明显大于标准方法所显示的.
- 标志物测试显示溶液不平衡,与扩散到谷物内部和在谷物内部交换相一致.
- 观察到的现象需要对在多孔介质中溶解物体运输的理解进行修订.
结论:
- 标准测量技术未能捕捉到含水层沙子中孔隙和反应点的全部范围.
- 扩散到谷物内部是影响溶液运输的关键过程,特别是对于反应性污染物.
- 运输模型需要更新的扩散表达式,以准确模拟污染物迁移,特别是放射性和有毒废物.
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