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硫酸盐配体对针铁矿表面碳酸铀酰表面物种的影响。

Effects of sulfate ligand on uranyl carbonato surface species on ferrihydrite surfaces.

机构信息

School of Agricultural, Forest and Environmental Sciences, 270 Poole Agricultural Center, Clemson University, Clemson, SC 29634-0315, USA.

出版信息

J Colloid Interface Sci. 2012 Jan 1;365(1):268-74. doi: 10.1016/j.jcis.2011.09.026. Epub 2011 Sep 21.

DOI:10.1016/j.jcis.2011.09.026
PMID:21996008
Abstract

Understanding uranium (U) sorption processes in permeable reactive barriers (PRB) are critical in modeling reactive transport for evaluating PRB performance at the Fry Canyon demonstration site in Utah, USA. To gain insight into the U sequestration mechanism in the amorphous ferric oxyhydroxide (AFO)-coated gravel PRB, U(VI) sorption processes on ferrihydrite surfaces were studied in 0.01 M Na(2)SO(4) solutions to simulate the major chemical composition of U-contaminated groundwater (i.e., [SO(4)(2-)] ~13 mM L(-1)) at the site. Uranyl sorption was greater at pH 7.5 than that at pH 4 in both air- and 2% pCO(2)-equilibrated systems. While there were negligible effects of sulfate ligands on the pH-dependent U(VI) sorption (<24 h) in both systems, X-ray absorption spectroscopy (XAS) analysis showed sulfate ligand associated U(VI) surface species at the ferrihydrite-water interface. In air-equilibrated systems, binary and mono-sulfate U(VI) ternary surface species co-existed at pH 5.43. At pH 6.55-7.83, a mixture of mono-sulfate and bis-carbonato U(VI) ternary surface species became more important. At 2% pCO(2), there was no contribution of sulfate ligands on the U(VI) ternary surface species. Instead, a mixture of bis-carbonato inner-sphere (38%) and tris-carbonato outer-sphere U(VI) ternary surface species (62%) was found at pH 7.62. The study suggests that the competitive ligand (bicarbonate and sulfate) coordination on U(VI) surface species might be important in evaluating the U solid-state speciation in the AFO PRB at the study site where pCO(2) fluctuates between 1 and 2 pCO(2)%.

摘要

了解可渗透反应屏障(PRB)中铀(U)的吸附过程对于在美国犹他州 Fry Canyon 示范场地评估 PRB 性能的反应输运模拟至关重要。为了深入了解非晶态氧化铁水合物(AFO)涂覆砾石 PRB 中 U 的螯合机制,在 0.01 M Na(2)SO(4)溶液中研究了亚铁氢氧化物表面上的 U(VI)吸附过程,以模拟该场地 U 污染地下水的主要化学成分(即[SO(4)(2-)]~13 mM L(-1))。在空气和 2% pCO(2)平衡系统中,pH 7.5 时的铀吸附量大于 pH 4 时的吸附量。虽然在两个系统中,硫酸盐配体对 pH 依赖性 U(VI)吸附(<24 h)的影响可以忽略不计,但 X 射线吸收光谱(XAS)分析表明硫酸盐配体与亚铁氢氧化物-水界面上的 U(VI)表面物种有关。在空气平衡系统中,pH 为 5.43 时,共存二元和单硫酸盐 U(VI)三元表面物种。在 pH 6.55-7.83 时,单硫酸盐和双碳酸盐 U(VI)三元表面物种的混合物变得更为重要。在 2% pCO(2)下,硫酸盐配体对 U(VI)三元表面物种没有贡献。相反,在 pH 7.62 时发现了双碳酸盐内界(38%)和三碳酸盐外界 U(VI)三元表面物种(62%)的混合物。研究表明,在评估研究场地 AFO PRB 中 U 的固相间形态时,竞争配体(碳酸氢盐和硫酸盐)在 U(VI)表面物种上的配位可能很重要,因为该场地的 pCO(2)在 1 和 2 pCO(2)%之间波动。

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