摘要
某铀矿床中水-岩反应的时间范围和强度,可通过对铀天然衰变系放射性不平衡的研究得到半定量化。该铀矿床在形成51Ma以来,由于水-岩反应较弱,矿石中铀系核素并未发生远距离迁移。铀矿体及近矿岩石至今仍基本处于化学封闭状态。虽然岩石裂隙附近局部发生核素微弱迁移和沉淀,但由于裂隙细小且大多充填粘土等,向上迁移不足35m,且仅发生在于106~104a及至今时段内。类比研究结果表明。
The time scale and intensity of the water rock interaction in a uranium deposit can be semi quantitatively assessed using uranium series disequilibrium. As the water rock interaction has been weak, no large range migration of the uranium series radio nuclides in the ores has occurred during 51 Ma since the deposit formed. Up till now, the uranium ore bodies and the granite around the ore bodies have chemically remained a close system. Although the local and weak removal and deposition of radio nuclides occurred in the granite near the fractures, the migration distance was no more than 35 m and only occurred in the time scale from 106 to 104 a or to present as the cracks in the rock are small and mostly filled with clay. This study shows that disposing high level radwaste in the fracture bearing granite without open faults is safe.
出处
《成都理工学院学报》
CSCD
1997年第2期87-94,共8页
Journal of Chengdu University of Technology
基金
国家自然科学基金
中国高放废物处置计划联合资助
关键词
核废物
处置库
安全评价
地球化学
high level radwaste
geological disposal
radioactive disequilibrium
uranium deposit
granite