摘要
测定了土壤包气层中氚在天然条件和人工喷淋条件下的扩散系数,研究了氚示踪剂在黄土包气层中的迁移规律.实验结果表明,在华北地区黄土高原天然条件下,包气带中氚示踪剂以0.03cm/d速度迁移,纵向扩散系数Dx为0.10cm2/d;在2m2实验坑中,以5mm/h喷淋强度每天喷淋3h的条件下,氚示踪剂以2.27cm/d的速度向下迁移, DX为7.75cm2/d。
Diffusivity of 3H was measured in soil aerated zone on both natural and artificial rainfall conditions, migration of 3H tracer was also studied in loess aerated zone at the same time. The results implied that the migration velocity of 3H tracer in aerated zone was 0.03cm/d on natural condition in loess plateau of Huabei Region, the vertical diffusivity Dx was 0.10cm2/d. In the experiment pit, the migration velocity was 2.27cm/d under an artificial condition of 5mm/h sprinkling intensity for 3 hours each day, the vertical diffusivity Dx was 7.75cm2/d.
出处
《核技术》
CAS
CSCD
北大核心
2000年第10期739-742,共4页
Nuclear Techniques
关键词
包气层
核素迁移
氚
示踪实验
放射性废物处置
Aerated zone, Diffusivity, Nuclides migration, Tritium, Tracing experiment