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福岛核电厂的中子泄漏证据来自加利福尼亚放射性 35S 的测量。

Evidence of neutron leakage at the Fukushima nuclear plant from measurements of radioactive 35S in California.

机构信息

University of California, San Diego, La Jolla, CA 92093, USA.

出版信息

Proc Natl Acad Sci U S A. 2011 Aug 30;108(35):14422-5. doi: 10.1073/pnas.1109449108. Epub 2011 Aug 15.

Abstract

A recent earthquake and the subsequent tsunami have extensively damaged the Fukushima nuclear power plant, releasing harmful radiation into the environment. Despite the obvious implication for human health and the surrounding ecology, there are no quantitative estimates of the neutron flux leakage during the weeks following the earthquake. Here, using measurements of radioactive (35)S contained in sulfate aerosols and SO(2) gas at a coastal site in La Jolla, California, we show that nearly 4 × 10(11) neutrons per m(2) leaked at the Fukushima nuclear power plant before March 20, 2011. A significantly higher (35)SO(2-)(4) activity as measured on March 28 is in accord with neutrons escaping the reactor core and being absorbed by the coolant seawater (35)Cl to produce (35)S by a (n, p) reaction. Once produced, (35)S oxidizes to (35)SO(2) and (35)SO(2-)(4) and was then transported to Southern California due to the presence of strong prevailing westerly winds at this time. Based on a moving box model, we show that the observed activity enhancement in (35)SO(2-)(4) is compatible with long-range transport of the radiation plume from Fukushima. Our model predicts that (35)SO(2-)(4), the concentration in the marine boundary layer at Fukushima, was approximately 2 × 10(5) atoms per m(3), which is approximately 365 times above expected natural concentrations. These measurements and model calculations imply that approximately 0.7% of the total radioactive sulfate present at the marine boundary layer at Fukushima reached Southern California as a result of the trans-Pacific transport.

摘要

最近的一次地震和随后的海啸对福岛核电站造成了广泛的破坏,向环境中释放了有害辐射。尽管这对人类健康和周围生态系统有明显的影响,但对于地震发生后的几周内中子通量泄漏,目前还没有定量估计。在这里,我们使用加利福尼亚州拉霍亚沿海地区硫酸盐气溶胶和 SO(2)气体中放射性 (35)S 的测量结果,表明在 2011 年 3 月 20 日之前,福岛核电站泄漏了近 4 × 10(11)个中子/平方米。3 月 28 日测量到的 (35)SO(2-)(4) 活性显著升高,这与从中子逃离反应堆堆芯并被冷却剂海水 (35)Cl 吸收,通过 (n, p)反应产生 (35)S 相符。一旦产生,(35)S 就会氧化为 (35)SO(2)和 (35)SO(2-)(4),由于此时盛行西风较强,随后被运送到南加州。基于移动盒模型,我们表明,观察到的 (35)SO(2-)(4) 活性增强与福岛放射性羽流的长距离传输是一致的。我们的模型预测,(35)SO(2-)(4),即福岛海洋边界层中的浓度,约为 2 × 10(5)个原子/立方米,这大约是预期自然浓度的 365 倍。这些测量结果和模型计算表明,由于跨太平洋传输,大约有 0.7%的放射性硫酸盐总量到达了南加州的海洋边界层。

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