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首页> 外文期刊>Journal of Colloid and Interface Science >Eu(III) uptake on rectorite in the presence of humic acid: A macroscopic and spectroscopic study
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Eu(III) uptake on rectorite in the presence of humic acid: A macroscopic and spectroscopic study

机译:腐殖酸存在下对累托石的Eu(III)吸收:宏观和光谱学研究

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摘要

This work contributed to the comprehension of humic acid (HA) effect on Eu(III) uptake to Na-rectorite by batch sorption experiments, model fitting, scanning electron microscopy, powder X-ray diffraction, Fourier transform infrared spectroscopy, X-ray photoelectron spectroscopy, and extended X-ray absorption fine structure (EXAFS) spectroscopy. At low pH, the presence of HA enhanced Eu(III) sorption on Na-rectorite, while reduced Eu(III) sorption at high pH. The experimental data of Eu(III) sorption in the absence and presence of HA were simulated by the diffuse-layer model well with the aid of FITEQL 3.2 software. The basal spacing of rectorite became large after Eu(III) and HA sorption on Na-rectorite. Some of Eu(III) ions and HA might be intercalated into the interlayer space of Na-rectorite. EXAFS analysis showed that the R_EuO (the bond distance of Eu and O in the first shell of Eu) and N values (coordination number) of Eu(III)-HA-rectorite system were smaller than those of Eu(III)-rectorite system.
机译:这项工作有助于通过分批吸附实验,模型拟合,扫描电子显微镜,粉末X射线衍射,傅里叶变换红外光谱,X射线光电子来理解腐殖酸(HA)对Eu(III)对钠锂蒙脱石吸收的影响光谱学和扩展X射线吸收精细结构(EXAFS)光谱学。在低pH下,HA的存在增强了钠锂蒙脱石对Eu(III)的吸附,而在高pH下降低了Eu(III)的吸附。借助FITEQL 3.2软件,通过扩散层模型很好地模拟了在不存在和存在HA的情况下Eu(III)吸附的实验数据。 Eu(III)和HA在钠锂蒙脱石上吸附后,累托石的基间距增大。某些Eu(III)离子和HA可能插入到钠锂蒙脱石的层间空间中。 EXAFS分析表明,Eu(III)-HA-锂蒙脱石体系的R_EuO(Eu和O在第一壳中的键间距)和N值(配位数)小于Eu(III)-锂蒙脱石体系。

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