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Removal of a basic dye from aqueous solution by a natural kaolinitic clay-Adsorption and kinetic studies

机译:天然高岭土从水溶液中去除碱性染料-吸附和动力学研究

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摘要

The < 25 μm fraction of natural clay containing kaolinite, chlorite, illite and illite/smectite mixed layered clay minerals was characterized and used as a potential adsorbent for the removal of Rhodamine B (RB) dye from aqueous solution. Adsorption experiments were carried out in batch mode by varying the following parameters: pH, temperature, initial dye concentration, adsorbent dosage and time of contact. The equilibrium data were well fitted by both the Langmuir and Freundlich adsorption isotherms. The Langmuir monolayer adsorption capacity was found to be 4.77 mg/g, which was better than the value reported for kaolinite (1.95 mg/g). The adsorption process followed pseudo-second-order kinetics. Negative ΔG _0 values indicated that adsorption onto this clay was a spontaneous process. A maximum dye uptake of > 90% was achieved at 313 K employing an initial dye concentration of 4.8 × 10 _(-6) M, a pH value of 2 and an adsorbent dosage of 1 g/l.
机译:表征了含量小于25μm的含有高岭石,绿泥石,伊利石和伊利石/蒙脱石混合层状粘土矿物的天然粘土,并将其用作从水溶液中去除若丹明B(RB)染料的潜在吸附剂。通过改变以下参数以分批方式进行吸附实验:pH,温度,初始染料浓度,吸附剂剂量和接触时间。 Langmuir和Freundlich吸附等温线均很好地拟合了平衡数据。发现Langmuir单层吸附容量为4.77 mg / g,比报道的高岭石(1.95 mg / g)更好。吸附过程遵循伪二级动力学。负ΔG_0值表明吸附在该粘土上是自发过程。初始染料浓度为4.8×10 -6(-6)M,pH值为2,吸附剂量为1 g / l,在313 K下达到最大染料吸收率> 90%。

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