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Distribution of pre- and post-Chernobyl radiocaesium with particle size fractions of soils

机译:切尔诺贝利前后放射性铯的粒径分布

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The association of radiocaesium with particle size fractions separated by sieving and settling from soils sampled eight years after the Chernobyl accident has been determined. The three size fractions were: < 2 μm, 2-63 μm and > 63 μm. ~(137)Cs in the soil samples was associated essentially with the finer size fractions, which generally showed specific activities 3-5 times higher than the bulk samples. Activity ratios of ~(134)Cs/~(137)Cs in the clay-sized fractions appear to be lower with respect to the corresponding values in bulk soil samples. This result indicates that some differences still exists in the particle size distribution between ~(137)Cs originating from nuclear weapons, which has been in the soil for decades after fallout, and ~(137)Cs coming from the Chernobyl accident, eight years after the deposition event. This behaviour could be related to "ageing" processes of radiocaesium in soils.
机译:切尔诺贝利事故后八年取样的土壤中,放射性铯与通过筛分和沉降分离出的粒度级分之间的关​​系已经确定。三种尺寸分数分别为:<2μm,2-63μm和> 63μm。土壤样品中的〜(137)Cs基本上与更细的颗粒级分有关,通常显示出比活度比散装样品高3-5倍。相对于散装土壤样品中的相应值,粘土级分中的〜(134)Cs /〜(137)Cs活度比似乎更低。该结果表明,在核尘沉降后数十年的核武器中〜(137)Cs与八年后的切尔诺贝利事故造成的〜(137)Cs的粒径分布仍存在一些差异。沉积事件。此行为可能与土壤中放射性铯的“老化”过程有关。

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