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Proton and Trivalent Metal Cation Binding by Dissolved Organic Matter in the Opalinus Clay and the Callovo-Oxfordian Formation

机译:质子和三价金属阳离子通过溶解的有机质结合在蛋白石粘土和Callovo-Oxfordian组中

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摘要

We investigated the proton and trivalent metal binding of dissolved organic matter (DOM) in in situ pore water and anoxic rock extracts of two potential host rocks for the disposal of radioactive waste, i.e., the Opalinus Clay (OPA) and the Callovo-Oxfordian formation (COx). The proton, curium, and europium binding properties of the OPA pore water and the extracted DOM of both rocks were studied with acid-base titrations, time-resolved laser fluorescence spectroscopy (TRLFS), and voltammetry, respectively. Protons were mostly buffered by inorganic compounds. DOM contributed to the total proton buffering capacity of the samples only to a small extent. Significant complexation of curium by DOM was observed for OPA pore water by TRFLS in contrastto little complexation by DOM detected in the OPA and COx extracts. The data on europium binding in OPA pore water were described by the presence of 14.3 μM organic ligands exhibiting a conditional affinity constant of log β = 6.50. Calculations of europium speciation under in situ conditions indicated that carbonates largely controlled the speciation of europium in OPA and COx. In the OPA formation, the presence of DOM may enhance the solubility of europium by 5 × 10~(-8) M, representing about one-third of total dissolvable europium.
机译:我们研究了原位孔隙水中的溶解有机质(DOM)的质子和三价金属结合以及两种潜在的用于放射性废物处置的宿主岩的缺氧岩提取物,即Opalinus粘土(OPA)和Callovo-Oxfordian地层(COx)。分别通过酸碱滴定,时间分辨激光荧光光谱(TRLFS)和伏安法研究了OPA孔隙水的质子,cur和and的结合特性以及两块岩石的提取DOM。质子大部分被无机化合物缓冲。 DOM仅在很小的程度上影响了样品的总质子缓冲能力。相对于OPA和COx提取物中检测到的DOM,OPA孔隙水通过TRFLS观察到的DOM与water的显着复合。关于OPA孔隙水中euro结合的数据由14.3μM有机配体的存在来描述,这些配体的条件亲和常数为logβ= 6.50。原位条件下of形态的计算表明,碳酸盐在很大程度上控制了OPA和COx中of的形态。在OPA的形成中,DOM的存在可使may的溶解度提高5×10〜(-8)M,约占可溶dis总量的三分之一。

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