混合红土中六价铬Cr (VI)的吸附去除

B. Sunil, Saifiya Faziludeen
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引用次数: 3

摘要

采用批量吸附技术,研究了六价铬(Cr (VI))在红土及与黑棉土、海相粘土和膨润土混合的红土上的吸附性能。在本试验中,天然红土分别与10%、20%和30% BC土、海相粘土和膨润土混合。研究了试验土在线性、Freundlich和Langmuir等温线上的相互作用。通过间歇吸附试验,确定了线性等温线参数、Freundlich和Langmuir等温线参数。采用双光束分光光度计测定了天然红土和混合红土对铬(VI)的吸附量。在红土中掺入10%、20%和30% BC土的分布系数分别为1.251、1.359和2.622 L/kg;与海相粘土混合的红土分别为5.396、12.973和48.641 L/kg,与膨润土混合的红土分别为5.093、8.148和12.179 L/kg。从相关系数较高的角度看,实验数据与Langmuir模型拟合较好。土壤pH值和土壤铁含量对Cr (VI)吸附影响较大。研究结果表明,红土与黏性土混合可吸附去除Cr (VI)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Removal of hexavalent chromium Cr (VI) by adsorption in blended lateritic soil
Hexavalent chromium [Cr (VI)] adsorption on lateritic soil and lateritic soil blended with black cotton (BC) soil, marine clay and bentonite clay were studied in the laboratory using batch adsorption techniques. In the present investigation the natural laterite soil was blended with 10%, 20% and 30% BC soil, marine clay and bentonite clay separately. The interactions on test soils have been studied with respect to the linear, Freundlich and Langmuir isotherms. The linear isotherm parameter, Freundlich and Langmuir isotherm parameters were determined from the from the batch adsorption tests. The adsorption of Cr (VI) on natural laterite soil and blended laterite soil was determined using double beam spectrophotometer. The distribution coefficients obtained were 1.251, 1.359 and 2.622 L/kg for lateritic soil blended with 10%, 20% and 30% BC soil; 5.396, 12.973 and 48.641 L/kg for lateritic soil blended with marine clay and 5.093, 8.148 and 12.179 L/kg for lateritic soil blended with bentonite clay respectively. The experimental data fitted well to the Langmuir model as observed from the higher value of correlation coefficient. Soil pH and iron content in soil(s) has greater influence on Cr (VI) adsorption. From the study it is concluded that laterite soil can be blended with clayey soils for removing Cr (VI) by adsorption.
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