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Chromate uptake characteristics of the pristine layered double hydroxides of Mg with Al

机译:mg与al的原始层状双氢氧化物的铬酸盐吸收特征

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摘要

The layered double hydroxides (LDHs) of Mg with Al readily scavenge dissolved chromate ions under a wide range of conditions. While the chromate uptake is quantitative in the LDH containing 33 mol% Al, the uptake is only 58% of the stoichiometric value in the LDH containing 25 mol% Al. This indicates that the lower symmetry of the NO3− ions in the LDH with 33 mol% Al facilitates the intercalation of chromate ions even under conditions of equilibration with excess dissolved nitrate ions. The chromate uptake obeys the Langmuir adsorption isotherm suggesting that the entire interlayer region of the LDH behaves like a surface. This surface is structural rather than morphological as the chromate uptake correlates negatively with the BET surface area of the LDHs.
机译:Mg与Al形成的层状双氢氧化物(LDHs)在宽范围的条件下均易于清除溶解的铬酸盐离子。尽管在含33摩尔%Al的LDH中铬酸盐的吸收是定量的,但吸收仅为含25摩尔%Al的LDH中化学计量值的58%。这表明,即使在与过量溶解的硝酸根离子平衡的条件下,具有33 mol%Al的LDH中NO3-离子的较低对称性也有助于铬酸盐离子的嵌入。铬酸盐的吸收符合Langmuir吸附等温线,表明LDH的整个夹层区域的行为都像表面。该表面是结构性的而不是形态的,因为铬酸盐的吸收与LDH的BET表面积呈负相关。

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