Effect of Dissolved Silica on Immobilization of Boron by Magnesium Oxide

被引:11
作者
Nozawa, Shoko [1 ,2 ]
Sato, Tsutomu [3 ]
Otake, Tsubasa [3 ]
机构
[1] Hokkaido Univ, Grad Sch Engn, Sapporo, Hokkaido 0608628, Japan
[2] Kankyo Zairyo Engn Co Ltd, Ota Ku, Tokyo 1440052, Japan
[3] Hokkaido Univ, Fac Engn, Sapporo, Hokkaido 0608628, Japan
来源
MINERALS | 2018年 / 8卷 / 02期
关键词
immobilization; boron; magnesium oxide; magnesium silicate hydrates (M-S-H); M-S-H; BOROSILICATE GLASSES; CRYSTAL-STRUCTURE; B-11; REMOVAL; SPECTROSCOPY; WATER;
D O I
10.3390/min8020076
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The effect of silica on the immobilization reaction of boron by magnesium oxide was investigated by laboratory experiments. In the absence of silica, due to dissolution of the magnesium oxide, boron was removed from solutions by the precipitation of multiple magnesium borates. In the presence of silica, magnesium silica hydrate (M-S-H) was formed as a secondary mineral, which takes up boron. Here B-11 magic-angle spinning nuclear magnetic resonance (MAS-NMR) and Fourier transform infrared spectrometer (FT-IR) data show that a part of the boron would be incorporated into M-S-H structures by isomorphic substitution of silicon. Another experiment where magnesium oxide and amorphous silica were reacted beforehand and boron was added later showed that the shorter the reaction time of the preceding reaction, the higher the sorption ratio of boron. That is, boron was incorporated into the M-S-H mainly by coprecipitation. The experiments in the study here show that the sorption of boron in the presence of silica is mainly due to the incorporation of boron during the formation of the M-S-H structure, which suggests that boron would not readily leach out, and that stable immobilization of boron can be expected.
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页数:13
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