研究论文
郭敏丽,王金生,李书绅.饱和黄土中3H和Br-迁移的延迟特征[J].环境科学学报,2004,24(5):878-882
饱和黄土中3H和Br-迁移的延迟特征
- Retardation characters of 3H and Br- migration in saturated loess
- 基金项目:国家重点基础研究发展规划(G1999043606);国家自然科学基金委员会;水利部黄河水利委员会黄河联合资助项目(50239010)
- 郭敏丽
- 北京师范大学环境学院, 地下水环境安全研究所, 环境模拟与污染控制国家重点联合实验室, 北京 100875
- 王金生
- 北京师范大学环境学院, 地下水环境安全研究所, 环境模拟与污染控制国家重点联合实验室, 北京 100875
- 摘要:饱和黄土核素迁移实验表明, Br-的迁移速度比3H快, 这种现象对核素的迁移研究具有重要意义, 但常用的模拟方法显然无法模拟出这种现象.利用实验参数并以水流流速为已知参数, 对实验数据进行了流速反推模拟, 结果显示, 3H和Br-在饱和黄土的迁移中均存在延迟现象, 且3H的延迟大于Br-, 模拟获得3H的延迟因子为195~205, Br-为160~190.对常用模拟法和流速反推法计算结果进行了比较, 结果显示, 采用常用模拟法获得的水流流速存在较大误差.延迟因子的灵敏度分析结果显示, 延迟因子对3H和Br-在饱和黄土中的迁移具有较大影响.
- Abstract:Tests of radionuclide migration in saturated loess soil showed that Br- migrated faster than 3H, this phenomenon has significant implications in the study of radionuclide migration, but has not been determined by numerical models. In this paper we proposed a new method to determine the breakthrough curves of 3H and Br- by obtaining the flow velocity from the tests. The results showed that the migration of both 3H and Br- are retarded in saturated loess, and retardation factors of 3H range from 1.95 to 2.05, and Br- from 1.60 to 1.90, respectively. Comparison of the common method and the proposed method showed that the former gives a larger error for the identification of groundwater velocity. In addition, sensitivity analysis of retardation factor indicated that retardation factor has important influence on 3H and Br- migration in saturated loess soil.
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