Zhang Junshe, Stanforth Robert
Department of Chemical and Biomolecular Engineering, National University of Singapore, Block E5 No. 02-9, 4 Engineering Drive 4, Singapore 117576.
Langmuir. 2005 Mar 29;21(7):2895-901. doi: 10.1021/la047636e.
The slow stage of phosphate or arsenate adsorption on hydrous metal oxides frequently follows an Elovich equation. The equation can be derived by assuming kinetic control by either a diffusion process (either interparticle or intraparticle) or a heterogeneous surface reaction. The aim of this study is to determine whether the slow stage of arsenic adsorption on goethite is more consistent with diffusion or heterogeneous surface reaction control. Adsorption kinetics of arsenate and dimethylarsinate (DMA) on goethite (alpha-FeOOH) were investigated at different pH values and inert electrolyte concentrations. Their adsorption kinetics was described and compared using Elovich (Gamma vs ln time) plots. Desorption of arsenate and DMA was studied by increasing the pH of the suspension from pH 4.0 to pH 10.0 or 12.0. The effective particle sizes and zeta-potential of goethite were also determined. Effective particle size increased rapidly as the pH approached pH(IEP), both in the absence and presence of arsenic. Inert electrolyte concentrations and pH had no effect on the slow stage of arsenate adsorption on goethite, while the kinetics of DMA adsorption on goethite was influenced by both parameters. The slow stage of arsenate adsorption on goethite follows an Elovich equation. Since effective particle size changes with both pH and inert electrolyte concentrations, and effective particle size influences interparticle diffusion, the arsenate adsorption kinetics indicate that the slow adsorption step is not due to interparticle diffusion. DMA also has complex adsorption kinetics with a slow adsorption stage. DMA desorbed completely and rapidly when the pH was raised, in contrast to the slow adsorption kinetics, indicating that the slow adsorption step is not due to intraparticle diffusion. The slow adsorption is not the result of diffusion, but rather is due either to the heterogeneity of the surface site bonding energy or to other reactions controlling arsenic removal from solution.
磷酸盐或砷酸盐在含水金属氧化物上的缓慢吸附阶段通常遵循埃洛维奇方程。该方程可以通过假设由扩散过程(颗粒间或颗粒内)或非均相表面反应进行动力学控制来推导。本研究的目的是确定砷在针铁矿上的缓慢吸附阶段更符合扩散控制还是非均相表面反应控制。在不同的pH值和惰性电解质浓度下,研究了砷酸盐和二甲基砷酸盐(DMA)在针铁矿(α-FeOOH)上的吸附动力学。使用埃洛维奇图(Γ对ln时间)描述并比较了它们的吸附动力学。通过将悬浮液的pH从4.0提高到10.0或12.0来研究砷酸盐和DMA的解吸。还测定了针铁矿的有效粒径和ζ电位。在不存在和存在砷的情况下,随着pH接近pH(等电点)时有效粒径均迅速增加。惰性电解质浓度和pH对砷酸盐在针铁矿上的缓慢吸附阶段没有影响,而DMA在针铁矿上的吸附动力学受这两个参数的影响。砷酸盐在针铁矿上的缓慢吸附阶段遵循埃洛维奇方程。由于有效粒径随pH和惰性电解质浓度而变化,并且有效粒径影响颗粒间扩散,因此砷酸盐吸附动力学表明缓慢吸附步骤不是由于颗粒间扩散。DMA也具有复杂的吸附动力学,具有缓慢的吸附阶段。与缓慢的吸附动力学相反,当pH升高时,DMA完全且迅速地解吸,这表明缓慢吸附步骤不是由于颗粒内扩散。缓慢吸附不是扩散的结果,而是由于表面位点键能的非均质性或由于控制从溶液中去除砷的其他反应。