核素迁移试验现场砂源中核素的淋洗及其形态研究

    STUDY ON THE RADIONUCLIDE ELUTION FROM QUARTZ SAND SOURCE AND THEIR SPECIATION

    • 摘要: 用地下水淋洗了核素迁移试验现场中使用的石英砂源 ,用超过滤法研究了淋洗液中核素的形态 ,用连续浸取法研究了淋洗后石英砂上残留核素的存在形态。结果表明 ,当淋洗液为 1 1 0倍柱体积时 ,地下水可将砂源上 90 %以上的2 37Np淋洗下来 ,且主要以可交换的离子态存在 ;淋洗后残留在石英砂上的2 37Np主要以碳酸盐结合态和铁锰氧化物结合态存在 ,其份额分别约为 5 5 %和 1 3 % ;2 38Pu从石英砂上的淋洗没有2 37Np容易 ,在淋洗液中2 38Pu主要以胶体存在

       

      Abstract: The study of the elution of the radionuclide from quartz sand source and their speciation is carried out by column method. The colloid form of nuclides in the eluted solution is studied by ultra-filtration method. The existing form of the nuclides on the sand after elution is studied with sequential extraction method. When the volume of eluted solution is up to 110 times of the column volume, the nuclide 237Np of more than 90% is eluted, and in the exchangeable form. The nuclide 237Np remained in the sand is mainly in the form of being coincident with the matrix of carbonate(5.5%) and the transition metals, iron and manganese( 1.3%). The elution of 238Pu from sand is more difficult than that of 237Np. 238Pu may exist in colloid form in eluted solution.

       

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