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Deposition of ~(137)Cs in Rokkasho, Japan and its relation to Asian dust

机译:日本六所庄〜(137)Cs的沉积及其与亚洲尘埃的关系

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Biweekly atmospheric depositions of ~(137)Cs were measured in Rokkasho, Aomori, Japan from March 2000 to March 2006 to study recent ~(137)Cs deposition. Although the deposition level was generally lower than the detectable limit, deposition samples collected in spring occasionally had measurable levels of ~(137)Cs. The annual ~(137)Cs deposition from 2001 to 2005 was 0.04-0.69 Bq m~(-2) with a mean value of 0.27 Bq m~(-2). Depositions of insoluble Al, Fe and Ti were strongly correlated with the ~(137)Cs deposition, suggesting that suspension of soil particles was the main source of the recent ~(137)Cs deposition. Asian dust events were coincident with some of the significant ~(137)Cs depositions in spring. It was found that the ratios of ~(137)Cs/Al and Fe/Al could be used as indices for discriminating Asian dust from suspension of the local surface soil. Backward trajectory analysis suggested southern Mongolian and northeastern China regions as sources of the significant ~(137)Cs depositions.
机译:自2000年3月至2006年3月在日本青森县六所町测量了〜(137)Cs的双周大气沉积,以研究最近的〜(137)Cs沉积。尽管沉积水平通常低于可检测的极限,但春季采集的沉积样品偶尔会达到〜(137)Cs的可测量水平。 2001〜2005年〜(137)Cs的年沉积量为0.04-0.69 Bq m〜(-2),平均值为0.27 Bq m〜(-2)。不溶性Al,Fe和Ti的沉积与〜(137)Cs沉积密切相关,表明土壤颗粒的悬浮是最近〜(137)Cs沉积的主要来源。亚洲尘埃事件与春季一些重要的〜(137)Cs沉积相吻合。结果表明,〜(137)Cs / Al和Fe / Al的比值可以作为区分亚洲粉尘和局部表层土壤悬浮的指标。向后的轨迹分析表明,蒙古南部和中国东北地区是〜(137)Cs沉积的重要来源。

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