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首页> 外文期刊>Water, Air, and Soil Pollution >MIGRATION OF SR, ND AND CE IN UNSATURATED CHINESE LOESS UNDER ARTIFICIAL SPRINKLING CONDITIONS: A FIELD MIGRATION TEST
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MIGRATION OF SR, ND AND CE IN UNSATURATED CHINESE LOESS UNDER ARTIFICIAL SPRINKLING CONDITIONS: A FIELD MIGRATION TEST

机译:人工喷洒条件下非饱和黄土中SR,ND和CE的迁移:野外迁移试验

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摘要

Double concentration peak phenomenon has been observed in nuclide migration tests in unsaturated Chinese loess during the cooperative research between China Institute for Radiation Protection (CIRP) and Japan Energy Atomic Research Institute (JEARI), and was considered conflicting with traditional theory of solute migration. In order to confirm the existence of this phenomenon and better understand its formation mechanism, we conducted a nuclide migration test that lasted 470 days using Sr, Nd and Ce which are analogues of ~(90) Sr and actinides, with loess and fine arenaceous quartz, respectively, as tracer carriers. In addition, we examined the efficacy of capillary barrier which is constructed by placing fine-grained soil on a layer of course-grained material, according to its influence on nuclide migration. When using loess as tracer carrier, a fraction of Sr migrated downward from the source layer to form a migration peak, and the residual Sr formed another concentration peak which corresponds to the source layer; while Nd and Ce hardly migrated during the 470 day test with only one concentration peak in the source layer. When using fine arenaceous quartz as tracer carrier, double concentration peak phenomenon occurs for all the nuclides examined, with the peaks distributing, respectively, on the upper and lower sides of the source layer. This phenomenon was suggested to result from the very low water containment ability and nuclide retentivity of the source layer arenaceous quartz. Thus, the so called double concentration peak phenomenon is formed by the source and subsequent migration of part of the source. The obviously reduced migration of Sr when taking fine arenaceous quartz as tracer carrier demonstrated significant influence of the capillary barrier formed by the fine arenaceous quartz layer and overlying loess on nuclide migration. Considering that the fine arenaceous quartz layer is very small (7 mm) in thickness and horizontally placed and the small dimension of the test pit, capillary barrier could be an effective way to protect the underlying waste from leaching.
机译:在中国辐射防护研究所(CIRP)和日本能源原子研究所(JEARI)的合作研究中,在不饱和黄土的核素迁移测试中观察到了双浓度峰现象,这被认为与传统的溶质迁移理论相冲突。为了确认这种现象的存在并更好地了解其形成机理,我们使用了与〜(90)Sr和act系元素类似的Sr,Nd和Ce以及黄土和细砂质石英进行了长达470天的核素迁移测试。分别作为示踪剂载体。此外,我们根据其对核素迁移的影响,研究了通过将细颗粒的土壤放置在一层粗颗粒材料上而构建的毛细管屏障的功效。当使用黄土作为示踪剂载体时,一部分Sr从源层向下迁移形成迁移峰,而残留的Sr形成另一个与源层相对应的浓度峰。在470天的测试中,Nd和Ce几乎没有迁移,在源层中只有一个浓度峰。当使用细砂质石英作为示踪剂载体时,所有检查的核素都出现双倍浓度峰现象,这些峰分别分布在源层的上侧和下侧。提示该现象是由于源层含砂石英的极低的含水能力和核素保持力所致。因此,所谓的双浓度峰现象是由源和源的一部分随后的迁移形成的。当以细砂石英为示踪剂载体时,Sr的迁移明显减少,这表明细砂石英层和上覆黄土形成的毛细屏障对核素迁移的影响很大。考虑到细砂石英层的厚度非常小(7 mm),并且水平放置并且测试坑的尺寸很小,毛细管屏障可以成为保护下面的废物免于浸出的有效方法。

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