Uptake of Cm (III) and Eu (III) by C–S–H phases under saline conditions in presence of EDTA: A batch sorption and TRLFS study

IF 3.1 3区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Applied Geochemistry Pub Date : 2024-06-28 DOI:10.1016/j.apgeochem.2024.106087
Aline K. Thumm, Andrej Skerencak-Frech, Xavier Gaona, Marcus Altmaier, Horst Geckeis
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Abstract

Eu (III) and Cm (III) uptake by calcium silicate hydrate phases (C–S–H) was investigated in presence of EDTA in NaCl and CaCl2 solutions. Different experimental parameters, i.e., ionic strength (0.1 m ≤ I'm ≤ 5.05 m), ligand concentration (10−5 m ≤ [EDTA] ≤ 10−2 m), calcium-to-silicon ratio (0.6 ≤ C/S ≤ 1.3) and sorption time (7 d ≤ t ≤ 365 d) were varied in the frame of batch sorption experiments and Time Resolved Laser Fluorescence spectroscopy (TRLFS) measurements. No effect of EDTA on the retention of Eu(III)/Cm(III) by C–S–H phases in NaCl or CaCl2 systems was observed at ligand concentrations ≤ 10−3 M. In NaCl solutions with [EDTA] = 10−2 M and C/S < 1.3, low retention (log Rd = 2–3, with Rd in L∙kg−1) of Eu(III) was detected after 7 d of sorption time, while strong retention (log Rd = 5–6) was observed after 50 d. This behaviour was explained by the initial stabilization of Eu(III)/Cm(III) in the aqueous phase due to the formation of two aqueous Eu(III)/Cm(III)-(OH)n-EDTA complexes, followed by the slow incorporation of Eu(III)/Cm(III) into the C–S–H structure. In CaCl2 solutions for all C/S ratios, as well as in NaCl solutions for C/S ∼ 1.3, the presence of [EDTA] = 10−2 M led to a significant decrease of the uptake (log Rd = 2–3) after 7 and 50 d of contact time. This effect was explained by the formation of stable aqueous Ca–Eu(III)/Cm(III)-EDTA complexes triggered by the presence of moderate to high Ca concentrations. No evident effect caused by increased ionic strength conditions could be confirmed in our sorption experiments.

Results obtained in batch sorption experiments are underpinned by TRLFS data, with the observation of three main aqueous species, tentatively defined as Cm(OH)(EDTA)2-, Cm(OH)x (EDTA)-(x+1) and Ca–Cm(III)-EDTA, as well as a fourth species corresponding to Cm(III) incorporated in the CaO-layer of the C–S–H phases. In spite of the thermodynamic stability of the CaEDTA2− complex, which reduces the concentration of free EDTA, the formation of ternary Ca–Eu(III)/Cm(III)-EDTA complexes is expected to result in a significant impact of EDTA on the uptake of An (III)/Ln (III) by cement at high ligand concentrations. The assumption that Ca outcompetes actinides for the complexation with EDTA in cementitious systems may need to be revisited under these conditions.

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在 EDTA 存在的盐水条件下,C-S-H 相对 Cm (III) 和 Eu (III) 的吸收:批量吸附和 TRLFS 研究
研究了硅酸钙水合物相(C-S-H)在 NaCl 和 CaCl2 溶液中 EDTA 存在下对 Eu (III) 和 Cm (III) 的吸收。在批量吸附实验和时间分辨激光荧光光谱(TRLFS)测量的框架内,改变了不同的实验参数,即离子强度(0.1 m ≤ I'm ≤ 5.05 m)、配体浓度(10-5 m ≤ [EDTA] ≤ 10-2 m)、钙硅比(0.6 ≤ C/S ≤ 1.3)和吸附时间(7 d ≤ t ≤ 365 d)。在 [EDTA] = 10-2 M 和 C/S < 1.3 的 NaCl 溶液中,吸附 7 d 后检测到 Eu(III) 的低保留率(log Rd = 2-3,Rd 单位为 L∙kg-1),而 50 d 后观察到强保留率(log Rd = 5-6)。这种行为的原因是,由于形成了两种水相 Eu(III)/Cm(III)-(OH)n-EDTA 复合物,Eu(III)/Cm(III)在水相中初步稳定,随后 Eu(III)/Cm(III) 缓慢地融入 C-S-H 结构。在所有 C/S 比率的 CaCl2 溶液中,以及在 C/S ∼ 1.3 的 NaCl 溶液中,[EDTA] = 10-2 M 的存在导致接触时间 7 天和 50 天后吸收量显著下降(log Rd = 2-3)。这种影响的原因是中高浓度的 Ca 引发了稳定的 Ca-Eu(III)/Cm(III)-EDTA 水络合物的形成。在批量吸附实验中获得的结果得到了 TRLFS 数据的支持,观察到三种主要的水溶液物种,初步定义为 Cm(OH)(EDTA)2-、Cm(OH)x (EDTA)-(x+1) 和 Ca-Cm(III)-EDTA 以及第四种与 Cm(III) 结合在 C-S-H 相的 CaO 层中相对应的物种。尽管 CaEDTA2- 复合物的热力学稳定性降低了游离 EDTA 的浓度,但 Ca-Eu(III)/Cm(III)-EDTA 三元复合物的形成预计会导致 EDTA 在高配体浓度下对水泥吸收 An (III)/Ln (III) 产生重大影响。在这些条件下,可能需要重新考虑钙在水泥基体系中与 EDTA 的络合中取代锕系元素的假设。
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来源期刊
Applied Geochemistry
Applied Geochemistry 地学-地球化学与地球物理
CiteScore
6.10
自引率
8.80%
发文量
272
审稿时长
65 days
期刊介绍: Applied Geochemistry is an international journal devoted to publication of original research papers, rapid research communications and selected review papers in geochemistry and urban geochemistry which have some practical application to an aspect of human endeavour, such as the preservation of the environment, health, waste disposal and the search for resources. Papers on applications of inorganic, organic and isotope geochemistry and geochemical processes are therefore welcome provided they meet the main criterion. Spatial and temporal monitoring case studies are only of interest to our international readership if they present new ideas of broad application. Topics covered include: (1) Environmental geochemistry (including natural and anthropogenic aspects, and protection and remediation strategies); (2) Hydrogeochemistry (surface and groundwater); (3) Medical (urban) geochemistry; (4) The search for energy resources (in particular unconventional oil and gas or emerging metal resources); (5) Energy exploitation (in particular geothermal energy and CCS); (6) Upgrading of energy and mineral resources where there is a direct geochemical application; and (7) Waste disposal, including nuclear waste disposal.
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