Global environmental transfer of 129I
详细信息    查看全文
文摘
129I is released to the environment via natural production due to cosmic interaction in the upper atmosphere; past nuclear weapon tests and routine releases from nuclear power plants (NPP) and fuel reprocessing plants (FRP). In this study, a compartmental model is used to estimate the transfer of 129I through various environmental segments like ocean atmosphere, land atmosphere, terrestrial biosphere, ocean mixed layer, surface soil, deep ocean, ocean sediment, shallow subsurface soil and deep subsurface soil due to its release in any one or more compartments. Due to NPP and FRP releases into the land atmosphere for a period of 1000 y, the highest inventory of 129I is observed in the surface soil up to a period of 3000 y; afterwards the deep ocean shows the highest inventory. The lowest inventory is found in the ocean sediment up to a period of 200 y; followed by the ocean atmosphere up to a period of 1250 y; afterwards the land atmosphere shows the lowest inventory. The maximum annual effective dose to the world population due to releases of 129I from NPP and FRP for a period of 100 y is estimated as 4.14 脳 10鈭? mSv/y. If the release period is 1000 y, the annual effective dose increases to 1.05 脳 10鈭? mSv/y and for an infinite period of release, it is estimated as 1.5 脳 10鈭? mSv/y. The model results are verified by comparing the effective dose per TBq release of 129I at different time periods with those reported by different international agencies and good matching is observed among the values.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700