首页> 外文期刊>Journal of Radioanalytical and Nuclear Chemistry: An International Journal Dealing with All Aspects and Applications of Nuclear Chemistry >Sorption of ~(125)I-, ~(137)Cs~+, ~(85)Sr~(2+) and ~(152,154)Eu~(3+) during their transport in undisturbed vertical and horizontal soil cores under dynamic flow conditions
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Sorption of ~(125)I-, ~(137)Cs~+, ~(85)Sr~(2+) and ~(152,154)Eu~(3+) during their transport in undisturbed vertical and horizontal soil cores under dynamic flow conditions

机译:〜(125)I-,〜(137)Cs〜+,〜(85)Sr〜(2+)和〜(152,154)Eu〜(3+)在动态扰动下在竖直和水平土心中的吸附流动条件

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Transport and sorption of ~(125)I-, ~(137)Cs+, ~(85)Sr~(2+) and ~(152,154)Eu~(3+) in undisturbed soil cores have been studied under dynamic conditions. Radionuclides were dissolved in synthetic groundwater (SGW) of 0.015 mol/dm~3 ionic strength, pH 8.4 and redox potential E_h = 145 mV. The soil samples were taken vertically and horizontally from the river bed at 5-100 cm depths, about 120 m southward of the Dukovany Low and Medium Level Radioactive Waste Repository. The respective water-soluble carriers in the 10~(-6) mol/dm~3 concentration were added into the SGW prior to the experiments. The soil cores of 9 cm height and 3.8 cm in diameter were placed into columns made of 150 cm~3 PE injection syringes of suitable dimensions. The SGW was introduced into columns from the Mariotte's bottle through a glass manifolds to supply the soil columns by gravity flow at a constant flow-rate about 1.2 cm~3/h. Into the water stream, radioactive nuclides were added individually in a form of a short pulse in 0.1 cm~3 of demineralized water. In the case of ~(125)I~- transport, retardation and hydrodynamic dispersion coefficients were determined, using an integral form of a simple advection-dispersion equation. For each radionuclides, sorption and desorption data have been obtained, evaluated and the results were compared mutually. Residual distributions of the sorbed cationic radionuclides along the soil columns were also presented.
机译:在动态条件下研究了〜(125)I-,〜(137)Cs +,〜(85)Sr〜(2+)和〜(152,154)Eu〜(3+)在未扰动土芯中的迁移和吸附。将放射性核素溶解在离子强度为0.015 mol / dm〜3,pH 8.4和氧化还原电势E_h = 145 mV的合成地下水(SGW)中。从Dukovany中低放射性废物处置库以南约120 m处的河床以5-100 cm的深度垂直和水平地采集土壤样品。在实验之前,将浓度分别为10〜(-6)mol / dm〜3的水溶性载体加入SGW。将高度为9 cm,直径为3.8 cm的土壤核心放入由尺寸合适的150 cm〜3 PE注射器制成的柱子中。通过玻璃歧管将SGW从Mariotte的瓶子中引入色谱柱,以重力流的形式以约1.2 cm〜3 / h的恒定流速向土壤柱提供水分。将放射性核素以短脉冲的形式分别添加到水流中,并加入0.1 cm〜3的软化水中。在〜(125)I〜-输运的情况下,使用简单对流扩散方程的积分形式确定了延迟和流体动力扩散系数。对于每种放射性核素,均已获取,评估了吸附和解吸数据,并相互比较了结果。还显示了沿土壤柱吸附的阳离子放射性核素的残留分布。

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