颗粒大小变化的对吸附到异质含水层沉积物的影响
Georgia R Barker1, Landis Jared West1, James T Graham2
1University of Leeds, UK.
Journal of environmental radioactivity
|June 8, 2024
概括
-90 (Sr-90) 在沉积物中的流动性是由吸附控制的. 这项研究发现,即使在异质的含水层材料中,也可以使用离子交换和表面复合模型准确预测Sr-90吸附.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 核科学 核科学 核科学
背景情况:
- -90 (Sr-90) 是核遗留现场的重要污染物.
- 它在地下水中的流动性在很大程度上取决于它对粘土和氧化铁等沉积物成分的吸附.
- 了解SR-90吸附对于管理受污染的场所至关重要.
研究的目的:
- 为了研究-2+ (Sr2+) 在异质含水层沉积物中的吸附.
- 评估不同沉积物颗粒大小的吸附模型 (Kd,Langmuir) 的适用性.
- 开发准确的方法来预测在复杂的地质环境中Sr-90吸收.
主要方法:
- 批量吸附测试是在从石到粘土的含水层沉积物上进行的.
- 确定了吸附系数 (Kd) 和朗慕尔参数 (qmax).
- 电子显微镜被用来描述沉积物的组成和表面特性.
- 离子交换和表面复合模型应用于pH依赖和离子强度依赖的吸附数据.
主要成果:
- 一个线性Kd模型准确地描述了Sr2+吸附,直到特定的平衡度.
- Sr2+吸附与沉积物的特性相关,如阴离子交换能力和表面积.
- 不同质的沉积物,包括砂岩石块和粘土矿物质,对吸附有显著的贡献.
- 一个取决于表面积的石校正改进了批量Kd值的估计.
- 取决于pH的吸附被解释为离子交换 (pH 2-7) 和合离子交换/表面复合 (pH > 7).
结论:
- 假设较大的分量的惰性,进行石校正对于准确的Sr-90吸附估计是不合适的.
- 在异质沉积物中的Sr-90吸附可以从Kd (<2毫米) 数据中可靠地估计,并进行适当的石校正.
- 结合的离子交换和表面复合模型有效地预测了Sr-90吸附行为在各种条件下.
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