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REMOVAL OF MULTIPLE-METALS FROM CONTAMINATED CLAY MINERALS

机译:从污染的粘土矿物中去除多种金属

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Clay minerals spiked with multi-component metal ions (Cu~(+2), Cd~(+2), Pb~(+2)) were decontaminated using different soil washing solutions. The desorption characteristics were determined by batch acid leaching with various acids. Removal of Cu~(+2), Cd~(+2)and Pb~(+2) ions from variable charge minerals (e.g. kaolinite) required much less effort than their removal from constant-charge minerals (e.g. illite). The surface charge of a clay mineral had an important influence. When the numbers of H~+ and Na~+ ions available in the soil were increased by adding a buffer solution such as NaOAc-HOAc, heavy metals adsorbed on the clay surface transferred to the pore fluid. When more H~+ or Na~+ ions were available in the pore fluid, more Cu~(+2), Cd~(+2) and Pb~(+2) ions were released into the equilibrium solution. Decreasing the pH led to more removal of heavy metal ions from kaolinite. The presence of Na~+ ions facilitated the removal of heavy metals from contaminated illite. The selectivity for desorption was in the order Cu~(+2) > Cd~(+2) > Pb~(+2) for all washing solutions investigated.
机译:使用不同的土壤洗涤液对掺有多组分金属离子(Cu〜(+2),Cd〜(+2),Pb〜(+2))的粘土矿物进行净化。解吸特性通过用各种酸进行分批酸浸确定。从可变电荷矿物质(例如高岭石)中去除Cu〜(+2),Cd〜(+2)和Pb〜(+2)离子所需的工作量要比从恒电荷矿物质(例如伊利石)中去除要少得多。粘土矿物的表面电荷具有重要影响。当通过添加缓冲溶液(如NaOAc-HOAc)增加土壤中可用的H〜+和Na〜+离子数量时,吸附在粘土表面的重金属会转移到孔隙流体中。当孔隙流体中有更多的H〜+或Na〜+离子时,更多的Cu〜(+2),Cd〜(+2)和Pb〜(+2)离子释放到平衡溶液中。降低pH值导致更多地从高岭石中去除重金属离子。 Na +离子的存在有助于从污染的伊利石中去除重金属。对于所有研究的洗涤溶液,解吸的选择性依次为Cu〜(+2)> Cd〜(+2)> Pb〜(+2)。

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