摘要
本文简要介绍了可能的核废物处置场地水运动的同位素示踪，并以￣（３６）Ｃｌ为例，说明了该方法在示踪非饱和带中降水的入渗作用、了解饱和带水流运动情况、测定地下水年龄及研究溶质迁移速率等方面的应用。
In this paper,isotopic tracing of the water moveements is the potential high-level radioactivewaste disposal repository sites has been briefly reviewed.The application of this method to the tracingof precipitation infiltration into the unsaturated zone and the water movement in the saturated zone,tothe dating of groundwater and the study of solute migration rates have been discussed as examplified bychlorine-36.
出处
《华东地质学院学报》
1995年第3期217-220,共4页
Journal of East China Geological Institute
关键词
核废物处置场
同位素示踪
水运动
地下水
氯
High-level radioactive waste disposal
Isotopic tracing
Chlorine-36
Water movements
