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Experimental and simulation results of the adsorption of Mo and V onto ferrihydrite

机译:钒铁吸附钼和钒的实验和模拟结果

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摘要

This study aims to highlight discrepancies between experimental and simulation linked to the mechanisms of Mo and V adsorption onto ferrihydrite (FHY) nanoparticles. We have measured adsorption capacities and uptake efficiencies and then fitted and compared these with outputs from various geochemical and adsorption models that were run as a function of pH, surface area (SA) and ferrihydrite particles size distributions. Our results revealed that the experimental data for the Mo system could be fitted very well, but this was not the case for the V system, when a model default value for the SA of FHY of 600 m2 g−1 was used. The discrepancy in the results for the V system can be explained by the lack of specific V species and/or associated constants in databases and variation in software versions, which change the outputted chemical species. Our comparative results also confirm that any experimental variables used as modelling inputs need to be checked carefully prior to any modelling exercises.
机译:这项研究旨在强调与Mo和V吸附到三水铁矿(FHY)纳米颗粒上的机理有关的实验和模拟之间的差异。我们已经测量了吸附能力和吸收效率,然后将其与各种地球化学和吸附模型的输出进行拟合,并将这些输出作为pH,表面积(SA)和三水铁矿粒径分布的函数进行分析。我们的结果表明,Mo系统的实验数据可以很好地拟合,但对于V系统,情况并非如此,当FHY的SA的模型默认值为600 m 2 g时,情况并非如此。使用了 -1 。 V系统结果的差异可以通过缺少特定的V种类和/或数据库中相关的常数以及软件版本的变化来解释,这会改变输出的化学种类。我们的比较结果还证实,在进行任何建模练习之前,必须仔细检查用作建模输入的任何实验变量。

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