Takeda Akira, Tsukada Hirofumi, Takaku Yuichi, Hisamatsu Shun'ichi, Nanzyo Masami
Department of Radioecology, Institute for Environmental Sciences, 1-7 Ienomae, Obuchi, Rokkasho, Aomori, 039-3212, Japan.
Sci Total Environ. 2006 Aug 31;367(2-3):924-31. doi: 10.1016/j.scitotenv.2006.01.006. Epub 2006 Feb 17.
The U concentrations in the soils of experimental fields with continuous fertilizer applications and in neighboring non-agricultural soils were determined. The surface soils in the three experimental fields with fertilizer applications contained higher amounts of U compared with the non-agricultural surface soils. The amount of U elevated in the soil was estimated by the vertical profile of U concentration, and an increase of about 200 mg m-2 of U was found in the soils at 0-35 cm depth during a 61-year cultivation period. The estimated value was almost the same as the amount of U added through the fertilizers as calculated from U concentrations in the applied fertilizers. Therefore, almost all the U from the fertilizers would still remain in the upper part of the soils. Chemical extraction results suggested that organic substances and noncrystalline clay minerals in the surface soil should play an important role for accumulation of U derived from the fertilizers.
测定了连续施肥试验田土壤以及相邻非农业土壤中的铀浓度。与非农业表层土壤相比,三个施肥试验田的表层土壤含有更高含量的铀。通过铀浓度的垂直剖面估算土壤中铀含量的升高情况,发现在61年的耕种期内,0-35厘米深度的土壤中铀含量增加了约200毫克/平方米。该估算值与根据施用肥料中的铀浓度计算得出的通过肥料添加的铀量几乎相同。因此,肥料中的铀几乎都仍留在土壤上部。化学提取结果表明,表层土壤中的有机物质和非晶质粘土矿物对肥料中铀的积累应起重要作用。