Sorption of Ammonium Ions onto Natural and Modified Egyptian Kaolinites: Kinetic and Equilibrium Studies

O. El-Shafey, N. Fathy, T. El-Nabarawy
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引用次数: 15

Abstract

Thermally activated, acid-activated, and acid-leached of thermally activated kaolinites were prepared from the Egyptian ore. The physical and chemical properties were studied using N2 sorption at −196°C, FTIR, SEM, and the total surface acidity. The sorption of ions on the investigated sorbents was controlled with the solution pH, sorbent dosage, and initial concentration of solution. Kinetic and equilibrium sorption at 30°C were employed. Four kinetic models were applied to the kinetic sorption data; pseudo-second-order, Elovich, and intraparticle diffusion models fitted well the kinetic data whereas pseudo-first-order model was less applicable. Elovich parameters refer to physical sorption type of on nonuniform sites and the intraparticle diffusion controls the sorption of by kaolinites to a small extent. The equilibrium sorption data followed Langmuir and D-R models; the negative value of indicates a spontaneous sorption and the mean sorption energy obtained shows also physical sorption. The sorption capacities of nonactivated and activated Egyptian kaolinites towards sorption (10.87–45.45 mg·g−1) were good sorbents as compared with those uptaken by other clays reported in the literature and proved to be more active besides being less expensive and highly available.
天然和改性埃及高岭石对铵离子的吸附:动力学和平衡研究
从埃及矿石中制备了热活化、酸活化和酸浸高岭石。采用- 196°C N2吸附、FTIR、SEM和表面总酸度研究了热活化高岭石的物理化学性质。所研究的吸附剂对离子的吸附受溶液pH、吸附剂用量和溶液初始浓度的控制。采用30℃下的动力学吸附和平衡吸附。对动力学吸附数据采用了四种动力学模型;伪二阶、Elovich和颗粒内扩散模型对动力学数据拟合较好,而伪一阶模型不太适用。Elovich参数是指在非均匀位置上的物理吸附类型,颗粒内扩散对高岭石的吸附有较小的控制作用。平衡吸附数据符合Langmuir和D-R模型;的负值表示自发吸附,平均吸附能也表示物理吸附。与文献报道的其他粘土相比,未活化和活化的埃及高岭土的吸附能力(10.87 ~ 45.45 mg·g−1)都是较好的吸附剂,而且价格便宜,可利用性高。
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