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Adsorption kinetics of chromium(III) removal from aqueous solutions using natural red earth

机译:使用天然红土从水溶液中去除铬(III)的吸附动力学

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Laboratory-scale-simulated experiments were carried out using Cr(Ⅲ) solutions to identify the Cr(Ⅲ) retention behavior of natural red earth (NRE), a natural soil available in the northwestern coastal belt of Sri Lanka. The effects of solution pH, initial Cr(Ⅲ) concentration and the contact time were examined. The NRE showed almost 100 % Cr(Ⅲ) adsorption within the first 90 min. [initial [Cr(Ⅲ)] = 0.0092-0.192 mM; initial pH 4.0-9.0]. At pH 2 (298 K), when particle size ranged from 125 to 180 urn the Cr(Ⅲ) adsorption data were modeled according to Langmuir convention assuming site homogeneity. The pH-dependent Cr(Ⅲ) adsorption data were quantified by diffused layer model assuming following reaction stoichiometries: 2 > AlOH_(s) + Cr (OH)_(2(aq))~→ (>AlO)_2Cr_(s)~+) + 2H_2O log K 15.56 2 >FeOH_(s)+ Cr(OH)_(2(ap))~+→ (>FeO)_2Cr_(s)~+ + 2H_2O log K 5.08. The present data showed that NRE can effectively be used to mitigate Cr(Ⅲ) from aqueous solutions and this method is found to be simple, effective, economical and environmentally benign.
机译:使用Cr(Ⅲ)溶液进行了实验室规模的模拟实验,以鉴定天然红土(NRE)的Cr(Ⅲ)保留行为,NRE是斯里兰卡西北沿海带可获得的天然土壤。研究了溶液pH值,初始Cr(Ⅲ)浓度和接触时间的影响。在最初的90分钟内,NRE表现出几乎100%的Cr(Ⅲ)吸附。 [初始[Cr(Ⅲ)] = 0.0092-0.192 mM;初始pH 4.0-9.0]。在pH为2(298 K)时,当粒径为125至180 um时,根据Langmuir惯例模拟Cr(Ⅲ)的吸附数据,并假设其位置均一。假设以下反应化学计量,通过扩散层模型对pH依赖的Cr(Ⅲ)吸附数据进行定量:2> AlOH_(s)+ Cr(OH)_(2(aq))〜→(> AlO)_2Cr_(s)〜 +)+ 2H_2O log K 15.56 2> FeOH_(s)+ Cr(OH)_(2(ap))〜+→(> FeO)_2Cr_(s)〜+ + 2H_2O log K 5.08。目前的数据表明,NRE可以有效地减轻水溶液中的Cr(Ⅲ),并且该方法简单,有效,经济且对环境无害。

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