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This study evaluated the influence of dissolved organic matter (DOM) properties on the speciation of Pb, Zn, and Cd. A total of six DOM samples were categorized into autochthonous and allochthonous sources based on their absorbance and fluorescence properties. The concentration of free metal ions ( C M 2+ ) measured by titration using the absence of gradients and Nernstian equilibrium stripping (AGNES) method was compared with that predicted by the Windermere humic aqueous model (WHAM). At the same binding condition (pH, dissolved organic carbon, ionic strength, and total metal concentration) the allochthonous DOM showed a higher level of Pb binding than the autochthonous DOM (84- to 504-fold C Pb 2+ variation). This dependency, however, was less pronounced for Zn (12- to 74-fold C Zn 2+ variation) and least for Cd (2- to 14-fold C Cd 2+ variation). The WHAM performance was affected by source variation through the active DOM fraction ( F ). The commonly used F = 1.3 provided reliable C Pb 2+ for allochthonous DOMs and acceptable C Cd 2+ for all DOM, but it significantly under-predicted C Pb 2+ and C Zn 2+ for autochthonous DOM. Adjusting F improved C M 2+ predictions, but the optimum F values were metal-specific (e.g., 0.03–1.9 for Pb), as shown by linear correlations with specific optical indexes. The results indicate a potential to improve WHAM by incorporating rapid measurement of DOM optical properties for site-specific F .
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Chen et al. (2018) studied this question.
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