Influence of inherent iron and oxygen concentrations on selenite sorption process using bentonite
Influence of inherent iron and oxygen concentrations on selenite sorption process using bentonite
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固有铁和氧浓度对膨润土吸附亚硒酸盐过程的影响
DOI:
10.1007/s11426-017-9091-4
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发表时间:
2017
期刊:
影响因子:
--
通讯作者:
刘春立
中科院分区:
文献类型:
--
作者:
何建刚;乔雪玲;时燕琳;李遥;杨小雨;周万强;刘春立
The oxygen concentration and inherent Fe in bentonite have a significant influence on the Se(IV) sorption process. In this study, the sorption of selenite on natural bentonite was investigated using a batch experiment method, and the distribution coefficient (Kd) values were obtained in the pH range from 2.0 to 10.0 under oxic/anoxic conditions. TheKdvalues always reached a maximum value at a pH of 4 under oxic conditions and at a pH of 8 under anoxic conditions; meanwhile, theKdvalue under anoxic conditions was larger than the value under oxic conditions, especially in regard to the maximumKdvalues. The oxygen conditions have a significant influence on the ratio of redox-sensitive Fe2+/Fe3+, which was closely related to the difference in theKdvalues under both oxic/anoxic conditions. Ferric selenite and green rust could be responsible for the maximumKdvalues under oxic/anoxic conditions. In the leaching experiments, we found that the Fe2+in bentonite could replace Mg2+and Al3+in the octahedral sheet. Spectroscopy methods, such as Fourier transform infrared spectroscopy (FTIR), X-ray diffraction (XRD) and X-ray absorption spectroscopy (XAS) were used to characterize the surface properties of the samples after reaction. Overall, this study shows that the addition of Fe2+-containing materials into backfill/buffer materials under anoxic condition could enhance the sorption of79Se(IV).