Fluvial Transport of Chernobyl Plutonium (Pu) to the Black Sea: Evidence from 240Pu/239Pu Atom Ratios in Danube Delta Sediments

M. Ketterer, S. Gulin, Gary D. MacLellan, W. J. Hartsock
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引用次数: 12

Abstract

Sector field ICP-MS has been used to determine 239+240 Pu activity and 240 Pu/ 239 Pu atom ratio profiles in a sediment core obtained in 1997 from the Danube Delta region of the Black Sea. The 239+240 Pu activity profile reveals the presence of a 1963 stratospheric fallout peak, along with two more recent peaks stemming from fluvial transport of Chernobyl Pu through the Danube watershed into the Black Sea. The two recent peaks occur in the early 1990's and are associated with 240 Pu/ 239 Pu atom ratios as high as 0.307, significantly exceeding the established range of stratospheric fallout ( 240 Pu/ 239 Pu = 0.180 ± 0.014). The Chernobyl-derived 240 Pu/ 239 Pu features in the core are also associated with elevated 238 Pu activities (determined by alpha spectrometry), and 238 Pu/ 239+240 Pu activity ratios of 0.08-0.10 in excess of the stratospheric fallout signature ( 238 Pu/ 239+240 Pu = 0.04).
切尔诺贝利钚(Pu)向黑海的河流输送:多瑙河三角洲沉积物中240Pu/239Pu原子比的证据
用扇形场ICP-MS测定了1997年在黑海多瑙河三角洲地区获得的沉积物岩心中的239+240 Pu活度和240 Pu/ 239 Pu原子比。239+240铀的活动剖面揭示了1963年平流层放射性沉降峰值的存在,以及由于切尔诺贝利铀通过多瑙河流域进入黑海的河流运输而产生的两个最近的峰值。最近的两个峰值出现在20世纪90年代初,与240 Pu/ 239 Pu原子比高达0.307有关,大大超过了平流层沉降的既定范围(240 Pu/ 239 Pu = 0.180±0.014)。切尔诺贝利核心区的240 Pu/ 239 Pu特征也与238 Pu活性升高有关(由α光谱测定),238 Pu/ 239+240 Pu活性比超过平流层沉降特征(238 Pu/ 239+240 Pu = 0.04) 0.08-0.10。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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