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大气试验中产生的放射性核素在全球范围内的扩散与沉降。

Worldwide dispersion and deposition of radionuclides produced in atmospheric tests.

作者信息

Bennett Burton G

机构信息

Environmental Measurements Laboratory, U.S. Department of Energy, New York, NY 10014-4811, USA.

出版信息

Health Phys. 2002 May;82(5):644-55. doi: 10.1097/00004032-200205000-00011.

Abstract

Radionuclides produced in atmospheric nuclear tests were widely dispersed in the global environment. From the many measurements of the concentrations in air and the deposition amounts, much was learned of atmospheric circulation and environmental processes. Based on these results and the reported fission and total yields of individual tests, it has been possible to devise an empirical model of the movement and residence times of particles in the various atmospheric regions. This model, applied to all atmospheric weapons tests, allows extensive calculations of air concentrations and deposition amounts for the entire range of radionuclides produced throughout the testing period. Especially for the shorter-lived fission radionuclides, for which measurement results at the time of the tests are less extensive, a more complete picture of levels and isotope ratios can be obtained, forming a basis for improved dose estimations. The contributions to worldwide fallout can be inferred from individual tests, from tests at specific sites, or by specific countries. Progress was also made in understanding the global hydrological and carbon cycles from the tritium and 14C measurements. A review of the global measurements and modeling results is presented in this paper. In the future, if injections of materials into the atmosphere occur, their anticipated motions and fates can be predicted from the knowledge gained from the fallout experience.

摘要

大气层核试验产生的放射性核素在全球环境中广泛扩散。通过对空气中浓度和沉降量的大量测量,人们对大气环流和环境过程有了很多了解。基于这些结果以及所报道的各次试验的裂变产额和总产额,得以设计出一个关于粒子在不同大气区域的运动和停留时间的经验模型。该模型应用于所有大气层武器试验,能够对整个试验期间产生的所有放射性核素的空气浓度和沉降量进行广泛计算。特别是对于寿命较短的裂变放射性核素,在试验时其测量结果较少,由此可以获得更完整的水平和同位素比值情况,为改进剂量估计奠定基础。对全球沉降的贡献可以从个别试验、特定地点的试验或特定国家的试验中推断出来。通过对氚和碳 - 14的测量,在理解全球水文循环和碳循环方面也取得了进展。本文对全球测量和建模结果进行了综述。未来,如果向大气中注入物质,根据从沉降经验中获得的知识可以预测其预期的运动和归宿。

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