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使用尺寸排阻色谱法(SEC)测定 Rh(III)与腐殖酸相互作用的动力学效应。

Kinetic effects on the interactions of Rh(III) with humic acids as determined using size-exclusion chromatography (SEC).

机构信息

Marine Biogeochemistry Research Group, Instituto de Investigacións Mariñas (CSIC), 36208 Vigo, Spain.

出版信息

Environ Sci Pollut Res Int. 2013 Apr;20(4):2330-9. doi: 10.1007/s11356-012-1113-8. Epub 2012 Aug 9.

Abstract

The anthropogenic inputs of Rh in the environment-together with other platinum group elements-have increased considerably during the last 20-30 years. However, thermodynamics and kinetics on the interaction of Rh with natural organic and inorganic ligands are still poorly characterized. Here, we report the time-dependent speciation of rhodium chlorides spiked to model freshwater with and without the presence of humic substances. Rhodium species were determined using size-exclusion chromatography-inductively coupled plasma mass spectrometry (SEC-ICP-MS). Results indicate that organic matter can effectively bind rhodium, but the extremely slow reaction kinetics of Rh plays a significant role on its speciation in natural waters. Accordingly, formation of Rh-organic complexes from spiked rhodium chlorides required around 15 days to reach equilibrium; this should be taken into account in those laboratory experiments where the biological interactions of Rh, using spiked samples, are studied. Regarding Rh inorganic speciation in freshwater, the available thermodynamic constants predict the dominance of the neutral trihydroxo and negatively charged tetrahydroxo rhodium complexes over typical pHs (6-8); our results, however, indicate only the presence of negatively charged hydroxocomplexes at pH 7. Reexamination of the Rh stability constants suggest that these hydroxylated rhodium complexes may also dominate its inorganic speciation in seawater.

摘要

在过去的 20-30 年中,人为向环境中输入的铑-以及其他铂族元素-大大增加了。然而,铑与天然有机和无机配体相互作用的热力学和动力学仍未得到充分描述。在这里,我们报告了添加到有和没有腐殖质存在的模型淡水中的氯化铑的时变形态。使用尺寸排阻色谱-电感耦合等离子体质谱(SEC-ICP-MS)来确定铑的形态。结果表明,有机物可以有效地结合铑,但铑的极其缓慢的反应动力学对其在天然水中的形态分布起着重要作用。因此,从添加的氯化铑中形成的 Rh-有机络合物需要大约 15 天才能达到平衡;在使用添加样品研究 Rh 的生物学相互作用的那些实验室实验中,应考虑到这一点。关于淡水中的 Rh 无机形态分布,可用的热力学常数预测中性三羟基和带负电荷的四羟基铑络合物在典型 pH 值(6-8)下占主导地位;然而,我们的结果仅表明在 pH 值为 7 时存在带负电荷的氢氧化物络合物。对 Rh 稳定常数的重新检查表明,这些羟基化的铑络合物也可能主导其在海水中的无机形态分布。

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