摘要
安全处置高放废物是一项关系到核工业可持续发展、保护环境和保护人民健康的重要而紧迫的重大课题,同时也是一项世界性难题。本文在北山预选区利用音频大地电测测深,查明及圈定花岗岩岩体的分布范围、空间形态、岩体接触面、向深部延伸以及岩体内部不良地质结构的状况。研究结果表明,该技术在探测预选区花岗岩深部地质构造特征方面具有明显的优势,能够解决高放废物深埋地质处置中所遇到的地质构造问题,为处置库场址的稳定性和完整性评价提供参考。
Safe disposal of high level radioactive waste is a major task facing the sustainable development of nuclear industry,the protection of environment and the health of mankind.It is also a difficult problem in the world.How to dispose of high level radioactive waste safely and effectively is very important.This paper based on the method of using EH4 method in Beishan preselected area,detects and locates the range of distribution of the granitic mass,the spatial patterns,the contact area of rock mass,and the conditions of deep-lying and inner adverse geological mass in rock.The whole research results of detection show that the EH4 method has obvious advantage in detecting deep-lying geological structure of granitic mass in preselected area.It also can solve the problems of geological structure and provide a reference for the high level radioactive waste repository site of stability and integrity.
出处
《工程地球物理学报》
2013年第2期156-160,共5页
Chinese Journal of Engineering Geophysics
基金
国防科学技术工业局(编号:2008-652)项目
东华理工大学放射性地质与勘探技术国防重点学科实验室开放基金项目(编号:2011RGET03)
江西省教育厅青年科学基金项目(编号:GJJ12391)联合资助
关键词
EH4
高放废物处置库
花岗岩
EH4
high-level radioactive waste repository
granite
