Metal Speciation in Water of the Flooded Mine “Arsenic” (Karelia, Russia): Equilibrium-Kinetic Modeling with a Focus on the Influence of Humic Substances

• Published in: Aquatic geochemistry 2021-06, Vol.27 (2), p.141-158
• Main Authors: Cherkasova, Elena V., Konyshev, Artem A., Soldatova, Evgeniya A., Sidkina, Evgeniya S., Mironenko, Mikhail V.
• Format: Article
• Language: English
• Subjects: Analytical Chemistry; Anthropogenic factors; Arsenic; Biogeosciences; Calcium; Copper; Drainage water; Earth and Environmental Science; Earth Sciences; Earth System Sciences; Environmental effects; Equilibrium; Fulvic acids; Gangue; Geochemistry; Heavy metals; Human influences; Humic substances; Iron; Ligands; Magnesium; Man-induced effects; Metal concentrations; Metals; Mine drainage; Mine flooding; Minerals; Modelling; Oceanography; Open systems; Organic matter; Original Article; Speciation; Water pollution; Zinc
• ISSN: 1380-6165; 1573-1421
• DOI: 10.1007/s10498-021-09393-3

Equilibrium-kinetic modeling allows investigating metal behavior in the water–rock-organic matter system with time to evaluate anthropogenic effects on the environment. In the article, the interactions of stagnant mine drainage water of the flooded mine “Arsenic” with ore and gangue minerals were simulated using different organic matter incorporation approaches. If the model is closed to humic substances (no additional organic matter input), most fulvic acids are bound in the Fe fulvate complex. While under the removal of Fe fulvate from the model, the Cu fulvate becomes prevalent, the contribution of the fulvate complexes with Zn, Mg, and Ca also increases. This scenario simulates the organo-mineral complexes behavior well and allows identifying the sequence of metal binding to organic ligands as follows Fe > Cu > Zn > Mg > Ca. The second scenario imitates the constant input of organic matter to the model (open system regarding humic substances). The dissolved metal concentrations in the model solution are extremely high in comparison to the mine drainage water. This scenario demonstrates that excessive input of organic matter leads to the accumulation of the metals in a dissolved form and blocks the secondary mineral formation despite the faster dissolution of the primary minerals under a more acidic pH than in the first scenario. However, despite the differences between the model solution and the mine drainage water, this scenario is useful to address specific issues associated with changes in natural and anthropogenic conditions. Both scenarios show the importance of organic matter incorporation to the equilibrium-kinetic models.