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Takuya Kobayashi Haruyasu Nagai Masamichi Chino Hideyuki Kawamura 《Journal of Nuclear Science and Technology》2013,50(3):255-264
The source term of the atmospheric release of 131I and 137Cs due to the Fukushima Dai-ichi Nuclear Power Plant accident estimated by previous studies was validated and refined by coupling atmospheric and oceanic dispersion simulations with observed 134Cs in seawater collected from the Pacific Ocean. By assuming the same release rate for 134Cs and 137Cs, the sea surface concentration of 134Cs was calculated using the previously estimated source term and was compared with measurement data. The release rate of 137Cs was refined to reduce underestimation of measurements, which resulted in a larger value than that previously estimated. In addition, the release rate of 131I was refined to follow the radioactivity ratio of 137Cs. As a result, the total amounts of 131I and 137Cs discharged into the atmosphere from 5 JST on March 12 to 0 JST on March 20 were estimated to be approximately 2.0 × 1017 and 1.3 × 1016 Bq, respectively. 相似文献
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本文写于日本311大地震、海啸发生后的不同时段.首先,对福岛核事故的趋向进行了初步探讨,提出了发生堆芯熔化的可能性极大;其次,对我国的核安全检查进行了思考,述说了可能危及核电厂安全的外部自然事件和人为事件;最后结合地震后所发生的一些现象,提出了需要对地质、地震研究的问题. 相似文献
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