摘要
在中国辐射防护研究院（ＣＩＲＰ）试验场用Ｃｏｚ－（ＣｏＣｔ２”６ＨｚＯ）、Ｓｒ’”〔Ｓｒ（ＮＯａ）２」作喷淋液进行了１４４０ｈ的淋滤试验，得到了Ｃｏ、Ｓｒ在包气带土壤中迁移的平均阻滞系数；重点采用水文地球化学理论对试验结果作了解释，指出Ｃｏ、Ｓｒ’”的迁移主要受溶度积规则控制，且与土壤和孔隙水中Ｃｏｌ含量有关。
This experiment was made in China Institute for Radiation protection (CIRP) . In the test field, CoCl2 6H2O and Sr(NO3). aqueous solution is used for spinkling solution, Mean resistance detention coefficient of the Co2+ and Sr2+ migration in the aeration zone soil is estimated by C1 -- and Co2+ - Sr2+ mean migration velocity. The experimental result is emphatically explainedby hydrogeochemical theory , It is indicated that the migration of Co.t - Srz. in the aera- tion zone soil is under the control of solubility product rule and related to the Co - content in the soil and pore water.
出处
《水文地质工程地质》
CAS
CSCD
1997年第6期9-12,共4页
Hydrogeology & Engineering Geology
关键词
包气带
土壤
CO^2+
Sr^2+
阻滞系数
元素迁移
aeration zone soil, Co2+ -Sr2+ resistance detention coefficient , solubility product
