14C Entry into the Atmosphere


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

详细

14C enters the atmosphere in amounts equivalent to 1.4 PBq/yr with total accumulation 140 PBq via cosmic radiation. As a result of nuclear explosions (1950–1969), its activity in the atmosphere exceeded 200 PBq. At present, 14C has been completely removed into bottom waters and sedimentary rocks in the ocean. The activity of the 14C entering the atmosphere from all operating nuclear reactors equals ~0.3 PBq/yr and the amount from all spent fuel reprocessing facilities equals ~0.06 PBq/yr. The admissible levels of 14C emissions must not exceed levels corresponding to peroral intake dose 10 μSv/yr. This is can be accomplished by means of a system of measures: reduction of the volume of technogenic gases and their 12CO2 content, combining high-efficiency purification with dispersion through high exhaust-stacks, and developing new technologies and reagents binding 14C in compact forms.

作者简介

O. Ustinov

Bochvar High-Technology Research Institute for Inorganic Materials (VNIINM)

Email: j-atomicenergy@yandex.ru
俄罗斯联邦, Moscow

S. Yakunin

Bochvar High-Technology Research Institute for Inorganic Materials (VNIINM)

Email: j-atomicenergy@yandex.ru
俄罗斯联邦, Moscow

V. Kashcheev

Bochvar High-Technology Research Institute for Inorganic Materials (VNIINM)

Email: j-atomicenergy@yandex.ru
俄罗斯联邦, Moscow

补充文件

附件文件
动作
1. JATS XML

版权所有 © Springer Science+Business Media, LLC, part of Springer Nature, 2017