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福岛核事故后沙特阿拉伯利雅得放射性沉降物的指示情况。

Indication of the radioactive fallout in Riyadh, Saudi Arabia following the Fukushima nuclear accident.

作者信息

Alkhomashi N, Almasoud Fahad I

机构信息

Nuclear Science Research Institute, King Abdulaziz City for Science and Technology (KACST), P.O. Box 6086, Riyadh 11442, Saudi Arabia.

Nuclear Science Research Institute, King Abdulaziz City for Science and Technology (KACST), P.O. Box 6086, Riyadh 11442, Saudi Arabia.

出版信息

J Environ Radioact. 2016 Feb;152:70-4. doi: 10.1016/j.jenvrad.2015.11.009. Epub 2015 Nov 30.

Abstract

On March 2011, a severe damage has occurred to Fukushima Di-iachi nuclear reactor complex in Japan following the huge earthquake and the resulting Tsunami. Consequently, vast amounts of radioactive fallout were released into the atmosphere and contaminated the environment in Japan. Soon after the accident, traces of anthropogenic radionuclides were detected in environmental samples collected in many parts in the northern hemisphere even very far away from Japan creating a global concern. There is no information about radioactive contamination in the Arabian Peninsula caused by the Japanese Fukushima nuclear accident. The first evidence of Fukushima radioactive fallout in Riyadh (24° 43' N, 46° 38' E), Saudi Arabia has been confirmed in April 8, 2011. The airborne fission products (131)I, (134)Cs and (137)Cs were measured in air samples. The radionuclide concentrations were determined by identifying their characteristic gamma rays using a germanium detector. Their activity concentrations were studied as a function of time over a period of 20 days at the end of which they had mostly fallen below our limit of detection. The maximum activity concentration of (131)I, (134)Cs and (137)Cs in air of, respectively, 323.7 ± 18.5, 17.2 ± 1.0 and 26.0 ± 1.8 μBq m(-3) were observed on April 10-11, 2011. The (131)I/(137)Cs and (134)Cs/(137)Cs activity ratio values in air were presented and discussed. Finally, the effective doses to the public of Riyadh city from inhalation of (131)I, (134)Cs and (137)Cs due to contribution from Fukushima incident was found far below levels of concern.

摘要

2011年3月,日本发生强烈地震并引发海啸,福岛第一核电站遭受严重破坏。结果,大量放射性尘埃被释放到大气中,污染了日本的环境。事故发生后不久,在北半球许多地区采集的环境样本中检测到人为放射性核素痕迹,甚至在距离日本很远的地方,这引起了全球关注。目前尚无关于日本福岛核事故导致阿拉伯半岛放射性污染的信息。2011年4月8日,沙特阿拉伯利雅得(北纬24°43′,东经46°38′)首次确认有来自福岛的放射性尘埃。对空气样本中的空气中裂变产物(131)I、(134)Cs和(137)Cs进行了测量。使用锗探测器通过识别其特征伽马射线来确定放射性核素浓度。在20天的时间里研究了它们的活度浓度随时间的变化,到最后它们大多已降至检测限以下。2011年4月10 - 11日,空气中(131)I、(134)Cs和(137)Cs的最大活度浓度分别为323.7±18.5、17.2±1.0和26.0±1.8 μBq m(-3)。给出并讨论了空气中(131)I/(137)Cs和(134)Cs/(137)Cs的活度比值。最后,发现由于福岛事件,利雅得市公众因吸入(131)I、(134)Cs和(137)Cs而受到的有效剂量远低于关注水平。

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