The Polytechnic School, Ira A. Fulton Schools of Engineering, Arizona State University, 7171 E. Sonoran Arroyo Mall, Mesa, AZ 85212, United States.
The Polytechnic School, Ira A. Fulton Schools of Engineering, Arizona State University, 7171 E. Sonoran Arroyo Mall, Mesa, AZ 85212, United States.
Sci Total Environ. 2016 Sep 1;563-564:965-70. doi: 10.1016/j.scitotenv.2015.11.176. Epub 2015 Dec 7.
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 groundwater, 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 DS=1/2 DP 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.
本研究探索了在连续流动条件下,利用孔表面扩散模型 (PSDM) 预测填充床系统中砷穿透曲线的可能性,从而最大限度地减少进行小规模试验的需要。为了在不进行繁琐的小规模测试的情况下评估纳米金属(氢)氧化物杂化离子交换介质在实际水基质中的性能,在拟平衡条件下进行了多点平衡批量吸附测试;通过 PSDM 在连续流动实验中预测了短床柱(SBC)的砷酸盐穿透曲线;在相同条件下进行了 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实际地下水时,水基质和竞争离子对介质的吸附容量没有任何显著影响。正如预期的那样,PSDM 对仅含砷的模型水的穿透曲线提供了相对较好的预测,这是由颗粒内质量传递限制的。相比之下,地下水的穿透曲线表明颗粒内质量传递明显更快,表明表面扩散过程发生在孔扩散的同时。在硫酸盐存在的情况下,对于描述砷酸盐在金属(氢)氧化物纳米增强杂化离子交换介质中的表面扩散,选择 DS=1/2 DP 似乎就足够了,然而,在不同处理情况下确定表面扩散系数大小的因素的定量描述仍有待探索。