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热活化层状双氢氧化物对水溶液中亚硒酸根阴离子的吸附

Absorption of the selenite anion from aqueous solutions by thermally activated layered double hydroxide.

作者信息

Liu Rui, Frost Ray L, Martens Wayde N

机构信息

Inorganic Materials Research Program, School of Physical and Chemical Sciences, Queensland University of Technology, 2 George Street, GPO Box 2434, Brisbane, Queensland 4001, Australia.

出版信息

Water Res. 2009 Mar;43(5):1323-9. doi: 10.1016/j.watres.2008.12.030. Epub 2009 Jan 3.

DOI:10.1016/j.watres.2008.12.030
PMID:19157487
Abstract

The presence of selenite or selenate in potable water is a health hazard especially when consumed over a long period of time. Its removal from potable water is of importance. This paper reports technology for the removal of selenite from water through the use of thermally activated layered double hydroxides. Mg/Al hydrotalcites with selenite in the interlayer were prepared at different times from 0.5 to 20 h through ion exchange. X-ray diffraction of the MgAlSeO3 hydrotalcites indicates that the selenite anion entered the interlayer spacing of Mg/Al hydrotalcite and MgAlSeO3 hydrotalcite was formed. Raman spectra proved the presence of selenite anion in the hydrotalcite interlayer as the counter anion. The band intensity and width of MgAlSeO3 hydrotalcite in the region of 3800-3000 cm(-1) increase with the adsorption of selenite by the Mg/Al hydrotalcite. The characteristic bands of free selenite anions in the MgAlSeO3 hydrotalcites are located between the region between 850 and 800 cm(-1). The Raman spectra of the lower wave number region of 550-500 cm(-1) show a shift toward higher wave numbers with adsorption of the selenite. An estimation of the amount of selenite anion removed by the thermally activated layered double hydroxide was obtained through the measurement of the intensity of the selenite Raman bands at 814 and 835 cm(-1) resulting from the amount of selenite anion remaining in solution. Thermally activated LDHs provide a mechanism for removing selenite anions from aqueous solutions.

摘要

饮用水中存在亚硒酸盐或硒酸盐会对健康造成危害,尤其是长期饮用时。从饮用水中去除这些物质至关重要。本文报道了通过使用热活化层状双氢氧化物从水中去除亚硒酸盐的技术。通过离子交换在0.5至20小时的不同时间制备了层间含有亚硒酸盐的Mg/Al水滑石。MgAlSeO3水滑石的X射线衍射表明,亚硒酸根阴离子进入了Mg/Al水滑石的层间间距,形成了MgAlSeO3水滑石。拉曼光谱证明了水滑石层间存在亚硒酸根阴离子作为平衡阴离子。随着Mg/Al水滑石对亚硒酸盐的吸附,MgAlSeO3水滑石在3800 - 3000 cm(-1)区域的谱带强度和宽度增加。MgAlSeO3水滑石中游离亚硒酸根阴离子的特征谱带位于850至800 cm(-1)之间。550 - 500 cm(-1)较低波数区域的拉曼光谱显示随着亚硒酸盐的吸附向更高波数移动。通过测量溶液中剩余亚硒酸根阴离子的量所产生的814和835 cm(-1)处亚硒酸根拉曼谱带的强度,估算了热活化层状双氢氧化物去除亚硒酸根阴离子的量。热活化层状双氢氧化物为从水溶液中去除亚硒酸根阴离子提供了一种机制。

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