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Actinide Geochemistry: From The Molecular Level To The Real System

机译:in系元素地球化学:从分子水平到真实系统

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Geochemical processes leading to either mobilization or retention of radionuclides in an aquifer system are significantly influenced by their interaction with rock, sediment and colloid surfaces. Therefore, a sound safety assessment of nuclear waste disposal requires the elucidation and quantification of those processes. State-of-the-art analytical techniques as e.g. laser- and X-ray spectroscopy are increasingly applied to study solid-liquid interface reactions to obtain molecular level speciation insight.rnWe have studied the sorption of trivalent lanthanides and actinides onto aluminium oxides, hydroxides and purified clay minerals by the time-resolved laser fluorescence spectroscopy and X-ray-absorption spectroscopy. Chemical constitution and structure of surface bound actinides are proposed based on spectroscopic information. Open questions still remain with regard to the exact nature of mineral surface ligands and the mineral/water interface. Similarities of spectroscopic data obtained for M(Ⅲ) sorbed onto γ-alumina, and clay minerals suggest the formation of very comparable inner-sphere surface complexes such as ≡ S-O-An(Ⅲ)(OH)_x~(2-x)(H_2O)_(5-x) at pH > 5. Those speciation data are found consistent with those predicted by surface complexation modelling. The applicability of data obtained for pure mineral phases to actinide sorption onto heterogeneously composed natural clay rock is examined by experiments and by geochemical modelling. Good agreement of experiment and model calculations is found for U(Ⅵ) and trivalent actinide/lanthanide sorption to natural clay rock. The agreement of spectroscopy, geochemical modelling and batch experiments with natural rock samples and purified minerals increases the reliability in model predictions.rnThe assessment of colloid borne actinide migration observed in various laboratory and field studies calls for detailed information on actinide-colloid interaction. Kinetic stabilization of colloid bound actinides can be due to inclusion into inorganic colloid matrix or by macromolecular rearrangement in case of organic, humic/fulvic like colloids. Only a combination of spectroscopy, microscopy and classical batch sorption experiments can help to elucidate the actinide-colloid interaction mechanisms and thus contribute to the assessment of colloids for radionuclide migration.
机译:地球化学过程导致放射性核素的移动或滞留在含水层系统中,受其与岩石,沉积物和胶体表面的相互作用的影响很大。因此,对核废料处置进行合理的安全评估需要阐明和量化这些过程。最先进的分析技术,例如激光和X射线光谱越来越多地用于研究固液界面反应以获得分子水平的形态学见解.rn我们研究了时间分辨激光荧光对三价镧系元素和act系元素在氧化铝,氢氧化物和纯净粘土矿物上的吸附光谱和X射线吸收光谱。基于光谱信息提出了表面结合的act系元素的化学组成和结构。关于矿物表面配体和矿物/水界面的确切性质,仍然存在悬而未决的问题。吸附在γ-氧化铝上的M(Ⅲ)的光谱数据相似,粘土矿物表明形成了非常相似的内球表面复合物,如≡SO-An(Ⅲ)(OH)_x〜(2-x)( pH值大于5时为H_2O)_(5-x)。发现这些形态数据与通过表面络合建模预测的形态数据一致。通过实验和地球化学模拟研究了纯矿物相获得的数据对act系元素吸附到非均质组成的天然粘土岩石上的适用性。发现U(Ⅵ)和三价act系元素/镧系元素对天然粘土岩石的吸附与实验和模型计算吻合良好。光谱学,地球化学建模以及使用天然岩石样品和纯净矿物进行批处理实验的协议提高了模型预测的可靠性。在各种实验室和现场研究中观察到的胶体传播系元素迁移的评估需要有关detailed系元素-胶体相互作用的详细信息。胶体结合的act系元素的动力学稳定可以归因于包含在无机胶体基质中,或者在有机,腐殖质/富里夫样胶体的情况下由于大分子重排。只有光谱学,显微镜学和经典的分批吸附实验的结合才能帮助阐明the系元素与胶体的相互作用机理,从而有助于评估胶体放射性核素的迁移。

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