Decoupling Precipitation and Surface Complexation during Mn(II) Removal by Biochar via Experiments and Atomistic Simulations
Audrey Ngambia, Anastasiia Gavrilova, Haitao Huang, Zhuodong Lyu, Ond\v{r}ej Ma\v{s}ek, Margaret Graham, and Valentina Erastova

TL;DR
This study combines experiments and simulations to elucidate how biochar removes Mn(II) from water, distinguishing between precipitation and surface complexation mechanisms, and offers insights for designing better water remediation materials.
Contribution
It provides a mechanistic framework combining experimental and atomistic simulation data to differentiate Mn(II) removal pathways by biochar, guiding engineered biochar design.
Findings
High-temperature biochar achieves ~50% Mn removal and raises pH to 9.
Lower-temperature biochars remove 20-30% Mn with neutral pH.
Deprotonated biochar surfaces promote strong Mn(II) adsorption.
Abstract
Manganese(II) mobilised by mining activity poses a persistent water-quality challenge, yet the mechanisms by which low-cost sorbents, such as biochar, sequester Mn(II) remain poorly resolved. This study identifies the specific chemical drivers of Mn(II) sequestration by combining fixed-bed column and batch experiments with atomistic molecular dynamics simulations. Oilseed rape straw biochars, produced at 350\textdegree C, 550\textdegree C, and 700\textdegree C, removed 20-50% of dissolved Mn from acidic influent (pH 4, 5 ppm). High-temperature biochar achieved the greatest removal (50%) and rapidly increased effluent pH to 9, triggering alkaline precipitation. Conversely, lower-temperature biochars removed 20-30% of Mn while maintaining a near-neutral pH (7-7.5). Enhanced \ce{K+} release in these systems indicates significant cation exchange and non-precipitative pathways.…
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Taxonomy
TopicsAdsorption and biosorption for pollutant removal · Geochemistry and Elemental Analysis · Phosphorus and nutrient management
