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福岛第一核电站事故后日本沿海地区 (90)Sr、(137)Cs 和 (134)Cs 的再评估。

Reassessment of (90)Sr, (137)Cs, and (134)Cs in the Coast off Japan Derived from the Fukushima Dai-ichi Nuclear Accident.

机构信息

Institut de Ciència i Tecnologia Ambientals & Departament de Física, Universitat Autònoma de Barcelona , 08193 Cerdanyola del Vallès, Spain.

Laboratory of Ion Beam Physics, ETH-Zurich , Otto-Stern-Weg 5, 8093 Zurich, Switzerland.

出版信息

Environ Sci Technol. 2016 Jan 5;50(1):173-80. doi: 10.1021/acs.est.5b03903. Epub 2015 Dec 17.

Abstract

The years following the Fukushima Dai-ichi nuclear power plant (FDNPP) accident, the distribution of (90)Sr in seawater in the coast off Japan has received limited attention. However, (90)Sr is a major contaminant in waters accumulated within the nuclear facility and in the storage tanks. Seawater samples collected off the FDNPP in September 2013 showed radioactive levels significantly higher than pre-Fukushima levels within 6 km off the FDNPP. These samples, with up to 8.9 ± 0.4 Bq·m(-3) for (90)Sr, 124 ± 3 Bq·m(-3) for (137)Cs, and 54 ± 1 Bq·m(-3) for (134)Cs, appear to be influenced by ongoing releases from the FDNPP, with a characteristic (137)Cs/(90)Sr activity ratio of 3.5 ± 0.2. Beach surface water and groundwater collected in Sendai Bay had (137)Cs concentrations of up to 43 ± 1 Bq·m(-3), while (90)Sr was close to pre-Fukushima levels (1-2 Bq·m(-3)). These samples appear to be influenced by freshwater inputs carrying a (137)Cs/(90)Sr activity ratio closer to that of the FDNPP fallout deposited on land in the spring of 2011. Ongoing inputs of (90)Sr from FDNPP releases would be on the order of 2.3-8.5 GBq·d(-1) in September 2013, likely exceeding river inputs by 2-3 orders of magnitude. These results strongly suggest that a continuous surveillance of artificial radionuclides in the Pacific Ocean is still required.

摘要

福岛第一核电站(FDNPP)事故发生后的几年里,日本沿海海域海水中的(90)Sr 分布情况受到的关注有限。然而,(90)Sr 是核设施内和储水罐中积水的主要污染物。2013 年 9 月在 FDNPP 外采集的海水样本显示,在距离 FDNPP 6 公里范围内,放射性水平明显高于福岛之前的水平。这些样本中,(90)Sr 的放射性活度高达 8.9±0.4 Bq·m-3,(137)Cs 为 124±3 Bq·m-3,(134)Cs 为 54±1 Bq·m-3,似乎受到了来自 FDNPP 的持续释放的影响,其(137)Cs/(90)Sr 活度比为 3.5±0.2。在宫城县海湾采集的滩面水和地下水的(137)Cs 浓度高达 43±1 Bq·m-3,而(90)Sr 接近福岛之前的水平(1-2 Bq·m-3)。这些样本似乎受到携带更接近 2011 年春季在陆地上沉降的 FDNPP 散落物的(137)Cs/(90)Sr 活度比的淡水输入的影响。2013 年 9 月,来自 FDNPP 释放的(90)Sr 持续输入量约为 2.3-8.5GBq·d-1,可能超过河流输入量 2-3 个数量级。这些结果强烈表明,仍需要对太平洋中的人工放射性核素进行持续监测。

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