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Possible change in Asian dust source suggested by atmospheric anthropogenic radionuclides during the 2000s

机译:大气人为放射性核素表明2000年代亚洲尘埃来源可能发生变化

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Decades-long monitoring of anthropogenic radionuclides in the atmospheric deposition in Tsukuba, Japan suggests not only the substantial impacts of the Asian dust (Kosa) on the deposition but also the possible change of the Kosa source region, especially during springs of the 2000s. In order to know more about such change, 4 single wet deposition events occurred in the spring of 2007 were scrutinized. The largest anthropogenic radionuclides wet deposition was supplied by the April 2-4 event. It brought several tens % of the monthly depositions (April 2007) of the dust (residue) mass (4.5 g M~(-2) and anthropogenic radionulides (~(90)Sr: 16,~(137)Cs: 97 and Pu: 3 mBq m~~(-2)). None of the events observed fulfilled both criteria of the specific activities and ~(90)Sr/~(137)Cs activity ratio to the Tsukuba soil; they did not exhibit local soil dust signature. The Kosa events in fact have extensive impacts on the atmospheric environment over Japan in spring season. Considering the elevated specific activities as well as greater ~(137)Cs/~(90)Sr activity ratio in the deposited dust, it is hypothesized that the dust source areas in Asian continent would be shifting from the arid zone to the desert-steppe zone suffering from desertification during the 2000s. This type of the Kosa may be called as the 'new-regime Kosa'. Chemical observation in the far downwind region of the Kosa dust could allow us to know possible shift in the source regions.
机译:对日本筑波大气沉积中人为放射性核素进行的长达数十年的监测表明,不仅亚洲尘埃(Kosa)对沉积物产生了重大影响,而且还特别是在2000年代春季期间,Kosa源区可能发生变化。为了更多地了解这种变化,我们仔细研究了2007年春季发生的4次单次湿沉降事件。 4月2-4日的事件提供了最大的人为放射性核素湿沉降。它带来了尘埃(残留)质量(4.5 g M〜(-2)和人为放射性核素(〜(90)Sr:16 ~~(137)Cs:97和Pu)的每月沉积量的百分之几十(2007年4月)。 :3 mBq m ~~(-2))。所观察到的事件均未达到筑波土壤的比活和〜(90)Sr /〜(137)Cs活度比的标准,也没有表现出局部土壤尘埃实际上,科萨事件在春季对日本的大气环境产生了广泛影响,考虑到比活度的升高以及沉积尘埃中〜(137)Cs /〜(90)Sr活度比的增加,我们推测在2000年代,亚洲大陆的粉尘源地区将从干旱地区转移到遭受荒漠化的沙漠草原地区,这种类型的科萨可能被称为“新政权科萨”。科萨尘埃的顺风区可能使我们知道源区可能发生的偏移。

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