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Nickel Adsorption by Variable Charge Soils: Effect of pH and Ionic Strength

机译:可变电荷土壤对镍的吸附:pH和离子强度的影响

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The effects of pH and ionic strength (I) on Ni adsorption in variable charge soils were evaluated by laboratory batch experiments. Experimental results fitted the Langmuir model. Maximum adsorption (Ads_(max)) ranged from 260-2818 mg kg~(-1) (topsoil)to 532-1541 mg kg~(-1) (subsoil). Nickel affinity (KL) was higher in the subsoil samples (0.022-0.236 L kg~(-1)) than in topsoil (0.003-0.049 L kg~(-1)). Adsorption envelopes showed sharp increase in Ni adsorption (20-90%) in the 4.0-6.0 pH range. Nickel adsorption was affected by I and specific adsorption predominated in the 3.0-5.0 pH range, while above pH 5.0, it was adsorbed by electrostatic mechanisms. Negative values of free energy variation (AG) and the separation factor K_R<1 indicated that Niadsorption reaction was favorable and occurred spontaneously, especially when pH increase. Chemical and mineralogical soil attributes should be considered as criteria for selecting the areas for disposal of residues containing Ni to minimize the impact on the environment.
机译:通过实验室分批实验评估了pH和离子强度(I)对可变电荷土壤中Ni吸附的影响。实验结果符合Langmuir模型。最大吸附量(Ads_(max))为260-2818 mg kg〜(-1)(表土)至532-1541 mg kg〜(-1)(底土)。底土样品(0.022-0.236 L kg〜(-1))的镍亲和力(KL)高于表土(0.003-0.049 L kg〜(-1))。吸附包膜显示在4.0-6.0 pH范围内,镍吸附量急剧增加(20-90%)。镍的吸附受I的影响,在3.0-5.0 pH范围内,比吸附占主导地位,而在pH 5.0以上,则通过静电机理吸附镍。自由能变化(AG)和分离因子K_R <1的负值表明Ni吸附反应是有利的并且自发发生,特别是在pH升高时。应将化学和矿物土壤属性作为选择含镍残留物处置区域的标准,以最大程度地减少对环境的影响。

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