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Characterization and radionuclide sorption of suspended particulate matters in freshwater according to their settling kinetics

机译:根据沉降动力学对淡水中悬浮颗粒物进行表征和放射性核素的吸附

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摘要

In freshwater, radionuclide transfers depend both on exchanges between liquid and solid phases and on mass transfers between suspended and bottom sediment. Whereas the former ones depend on chemical processes (sorption/desorption, complexation ...), the latter ones are regulated by hydrological and sedimentary considerations (dispersion, erosion, deposit ...) closely related to the interactions between flow, suspended matter and bed sediment. Previous studies highlight the need to consider the matter heterogeneity and its specific sediment dynamics to correctly report the in homogeneity of fluxes in time and in space. These considerations lead us to develop an experimental method to distinguish the different particle groups present in natural water, mainly according to their settling kinetics. In this context, this paper presents the experimental protocol TALISMEN to characterize a natural bulk suspension according to its main settling kinetics groups. In a first step, this identification is achieved by the use of a settling tank that allows the monitoring of the suspended solid concentrations at various depths, combined to a settling model applying a multi-class approach. In a second step, the particle groups are isolated and characterized. The sorption property of each group toward 137Cs is determined by estimation of its distribution coefficients (kd) and sorption kinetics.
机译:在淡水中,放射性核素的转移既取决于液相和固相之间的交换,也取决于悬浮和底部沉积物之间的质量转移。前者取决于化学过程(吸附/解吸,络合...),而后者则受与流动,悬浮物和水之间的相互作用密切相关的水文和沉积因素(分散,侵蚀,沉积...)的调节。床沉积物。先前的研究强调需要考虑物质的非均质性及其特定的沉积动力学,以正确报告时空中通量的均质性。这些考虑因素促使我们开发一种实验方法,主要根据沉降动力学来区分天然水中存在的不同颗粒组。在这种情况下,本文提出了根据其主要沉降动力学组对天然散装悬浮液进行表征的实验方案TALISMEN。第一步,通过使用一个沉降罐来实现这种识别,该沉降罐可以监测各种深度的悬浮固体浓度,并与采用多类方法的沉降模型相结合。在第二步骤中,分离并表征颗粒群。每一组对137Cs的吸附性能是通过估算其分布系数(kd)和吸附动力学来确定的。

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