Adsorption of heavy metals in acid to alkaline environments by montmorillonite and Ca-montmorillonite

Adsorption of heavy metals in acid to alkaline environments by montmorillonite and Ca-montmorillonite
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DOI:
10.1016/j.cej.2011.05.055
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发表时间:
2011-07-15
影响因子:
15.1
通讯作者:
Abatal, Mohamed
Abatal, Mohamed
中科院分区:
工程技术1区
文献类型:
--
作者:
de Pablo, Liberto;Lourdes Chavez, M.;Abatal, Mohamed

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Ca-蒙脱石对单阳离子溶液中Hg ~(2+)、Cr ~(3+)、Pb ~(2+)、Cu ~(2+)、Zn ~(2+)、Ba ~(2+)、Ni ~(2+)、Mn ~(2+)、Cd ~(2+)、Ba ~(2+)和Ag ~(2+)的吸附符合二级动力学,对Pb ~(2+)、Hg ~(2+)、Cu ~(2+)、Cd ~(2+)的吸附量分别为6.187 × 10 ~(2)、4.369 × 10 ~(2)、2.045 × 10 ~(2)、Zn ~(2+)1.576 × 10 ~(2+)、Ag ~(2+)1.375 × 10 ~(2+)、Cr ~(3+)7.917 × 10 ~(1+)、Ni ~(2+)7.300 × 10 ~(1+)、Ba ~(2+)6.815 × 10 ~(1+)、Cd ~(2+)2.003 × 10 ~(1+)和Mn ~(2+)1.632 × 10 ~(1+)mg·g ~(-1),大于蒙脱石。蒙脱石对Zn ~(2+)、Ba ~(2+)、Hg ~(2+)、Ni ~(2+)、Mn ~(2+)和Cd ~(2+)的吸附量分别为3.477 × 10 ~(-1)、6.984 × 10 ~(-1)、3.681 × 10 ~(-1)、4.849 × 10 ~(-1)、3.820 × 10 ~(-1)和6.978 × 10 ~(-1)。Ba ~(2+)1.073 × 10 ~(-1)和Ni ~(2+)5.969 mg g ~(-1)。在酸性阳离子溶液和近中性蒙脱石和钙蒙脱石建立的pH范围内,在pH低于5时沉淀Cr 3+的氧化物和氢氧化物。在较高pH值下,Hg-2(2+)、Zn 2+、Ba 2+、Cd 2+、Ni 2+、Mn 2+和Ag+以简单阳离子和羟基阳离子的形式被粘土吸附,吸附选择性顺序为Hg-2(2+)> Zn 2 + > Ba 2 + > Cd 2 + > Ni 2 + > Mn 2+。(C)2011 Elsevier B. V.保留所有权利。
Adsorption of Hg2+, Cr3+, Pb2+, Cu2+, Zn2+, Ba2+, Ni2+, Mn2+, Cd2+, Ba2+ and Ag+ by Ca-montmorillonite from monocationic solutions followed second-order kinetics, attaining removals q(e) of Pb2+ 6.187 x 10(2), Hg2+ 4.369 x 10(2), Cu2+ 2.045 x 10(2), Zn2+ 1.576 x 10(2), Ag+ 1.375 x 10(2), Cr3+ 7.917 x 10(1), Ni2+ 7.300 x 10(1), Ba2+ 6.815 x 10(1), Cd2+ 2.003 x 10(1) and Mn2+ 1.632 x 10(1) mg g(-1), greater than those by montmorillonite. Equilibrium adsorption by montmorillonite from bimodal metal +Ca2+ solutions followed the Langmuir model with adsorptions of Zn2+ 3.477 x 10(1), Ba2+ 6.984, Hg2+ 3.681 x 10(1), Ni2+ 4.849, Mn2+ 3.820 and Cd2+ 6.978 mg g(-1), and by Ca-montmorillonite of Zn2+ 3.523 x 10(1). Ba2+ 1.073 x 10(1) and Ni2+ 5.969 mg g(-1). Within the pH range established by acid cationic solutions and near neutral montmorillonite and Ca-montmorillonite, at pHs below 5 precipitate oxides and hydroxides of Cr3+. Pb2+ and Cu2+ while at higher pHs Hg-2(2+), Zn2+, Ba2+, Cd2+, Ni2+, Mn2+ and Ag+ remain in solution and are adsorbed as simple and hydroxyl cations by the clay, keeping the selectivity sequence Hg-2(2+) > Zn2+ > Ba2+ > Cd2+ > Ni2+ > Mn2+. (C) 2011 Elsevier B.V. All rights reserved.