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Zinc adsorption on Na-rectorite and effect of static magnetic field on the adsorption

机译:锌对钠锂蒙脱石的吸附及静磁场对吸附的影响

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摘要

Rectorite is a kind of rare clay minerals. In this work, the sorption of Zn~(2+) on Na-rectorite and the effects of static magnetic field on the sorption have been studied. The result from this study indicated that: (1) apparent equilibrium for the sorption of zinc onto Na-rectorite is attained within the first hour; (2) the maximum of the increment of Zn~(2+) adsorbed by Na-rectorite is obtained between pH 4 and pH 6; (3) magnetic treatment enhances the zeta potential of Na-rectorite dispersions in the absence of Zn~(2+) and reduces that of the dispersions in the presence of Zn~(2+); (4) magnetic treatment promotes the sorption of Zn~(2+) onto Na-rectorite, especially at the low Zn~(2+) concentration; (5) the effects of static magnetic field decrease the pH of Na-rectorite dispersions whether containing zinc or not. The mechanisms of static magnetic field on the sorption of Zn~(2+) on Na-rectorite were discussed.
机译:锂蒙脱石是一种稀有的粘土矿物。本文研究了锂蒙脱石对Zn〜(2+)的吸附作用以及静磁场对吸附的影响。这项研究的结果表明:(1)在第一个小时内就达到了锌在钠锂蒙脱石上的吸附的明显平衡; (2)在pH 4〜6之间获得钠锂蒙脱石吸附的Zn〜(2+)的最大增量。 (3)磁处理提高了锌蒙脱石分散体在没有Zn〜(2+)时的zeta电位,降低了在存在Zn〜(2+)时的分散性。 (4)磁处理促进了Zn〜(2+)在钠锂蒙脱石上的吸附,特别是在低Zn〜(2+)浓度下。 (5)静磁场的影响降低了钠锂蒙脱石分散体的pH,无论是否含有锌。讨论了静磁场对钠锂蒙脱石吸附Zn〜(2+)的机理。

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