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首页> 外文期刊>Geochemical Journal >Temporal variation of ~(134)Cs and ~(137)Cs activities in surface water at stations along the coastline near the Fukushima Dai-ichi Nuclear Power Plant accident site, Japan
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Temporal variation of ~(134)Cs and ~(137)Cs activities in surface water at stations along the coastline near the Fukushima Dai-ichi Nuclear Power Plant accident site, Japan

机译:日本福岛第一核电站事故发生地点附近海岸线沿线各站地表水中〜(134)Cs和〜(137)Cs活动的时间变化

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摘要

We present our April to December 2011 observations of ~(134)Cs and ~(137)Cs activities in surface water at Hasaki, a coastal station 180 km south of the Fukushima Dai-ichi Nuclear Power Plant (FNPP1) accident site. We also investigate trends by using published data from several other coastal stations, including the accident site. The maximum in radiocaesium activity at Hasaki was observed in June 2011, representing a delay of two months from the corresponding maximum in April 2011 at FNPP1. Directly discharged ~(134)Cs and ~(137)Cs were transported dominantly southward along the coastline of northeastern Honshu, at least in May and June 2011. The reasons for the two-month delay at Hasaki are not yet clear, but clockwise current associated with a warm water eddy of which center located at 36.5 N, 141.4 E off Iwaki between Onahama and Hasaki in mid of May 2011 might prevent southward transport of ~(134)Cs and ~(137)Cs released from FNPP1 to Hasaki until the end of May 2011.
机译:我们展示了我们在福岛第一核电站(FNPP1)事故地点以南180公里的滨海站Hasaki的地表水中〜(134)Cs和〜(137)Cs活动的观测结果。我们还通过使用其他几个沿海站点(包括事故现场)的已发布数据来调查趋势。 2011年6月在Hasaki观测到放射性铯的最高活动,比FNPP1的2011年4月的最高活动推迟了两个月。至少在2011年5月和2011年6月,直接排放的〜(134)Cs和〜(137)Cs沿本州东北部的海岸线主要向南输送。尚不清楚Hasaki延误两个月的原因,但顺时针与2011年5月中旬位于小名ama和波崎之间的岩城中心36.5 N,离磐石141.4 E的暖水涡相关,可能会阻止从FNPP1释放的〜(134)C和〜(137)C向南运输到Hasaki,直到2011年5月底。

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