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首页> 外文期刊>The Science of the Total Environment >Modeling packed bed sorbent systems with the Pore Surface Diffusion Model: Evidence of facilitated surface diffusion of arsenate in nano-metal (hydr)oxide hybrid ion exchange media
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Modeling packed bed sorbent systems with the Pore Surface Diffusion Model: Evidence of facilitated surface diffusion of arsenate in nano-metal (hydr)oxide hybrid ion exchange media

机译:用孔表面扩散模型对填充床吸附剂系统进行建模:砷酸盐在纳米金属(氢)氧化物混合离子交换介质中促进表面扩散的证据

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This study explores the possibility of employing the Pore Surface Diffusion Model (PSDM) to predict the arsenic breakthrough curve of a packed bed system operated under continuous flow conditions with realistic groundwa-ter, and consequently minimize the need to conduct pilot scale tests. To provide the nano-metal (hydr)oxide hybrid ion exchange media's performance in realistic water matrices without engaging in taxing pilot scale testing, the multi-point equilibrium batch sorption tests under pseudo-equilibrium conditions were performed; arsenate breakthrough curve of short bed column (SBC) was predicted by the PSDM in the continuous flow experiments; SBC tests were conducted under the same conditions to validate the model. The overlapping Freundlich isotherms suggested that the water matrix and competing ions did not have any denoting effect on sorption capacity of the media when the matrix was changed from arsenic-only model water to real groundwater. As expected, the PSDM provided a relatively good prediction of the breakthrough profile for arsenic-only model water limited by intraparticle mass transports. In contrast, the groundwater breakthrough curve demonstrated significantly faster intraparticle mass transport suggesting to a surface diffusion process, which occurs in parallel to the pore diffusion. A simple selection of D_s = 1/2 D_p appears to be sufficient when describing the facilitated surface diffusion of arsenate inside metal (hydr)oxide nano-enabled hybrid ion-exchange media in presence of sulfate, however, quantification of the factors determining the surface diffusion coefficient's magnitude under different treatment scenarios remained unexplored.
机译:这项研究探索了使用孔隙表面扩散模型(PSDM)来预测在连续水条件下以实际地下水运行的填充床系统的砷穿透曲线的可能性,从而最大程度地减少了进行中试规模测试的需要。为了提供纳米金属(氢)氧化物混合离子交换介质在实际水基质中的性能而无需进行繁重的中试规模测试,在拟均衡条件下进行了多点平衡批吸附实验; PSDM在连续流动实验中预测了短床柱(SBC)的砷酸盐穿透曲线;在相同条件下进行SBC测试以验证模型。重叠的Freundlich等温线表明,当基质从仅含砷的模型水变为真实的地下水时,水基质和竞争离子对介质的吸附能力没有任何影响。如预期的那样,PSDM为仅限于砷的模型水受颗粒内质量传输限制提供了突破性的相对预测。相反,地下水突破曲线显示出明显更快的颗粒内质量传输,暗示了与孔隙扩散平行发生的表面扩散过程。当描述砷酸盐在硫酸盐存在下促进金属(氢)氧化物纳米活化的杂化离子交换介质内部的砷表面促进扩散时,简单选择D_s = 1/2 D_p似乎已足够,但是,量化确定表面的因素的数量在不同的治疗方案下,扩散系数的大小尚待探索。

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