Explores electron transfer mechanisms in iron autotrophic denitrification, suggesting structural variations impact efficiency.
Pyrogenic carbon can regulate iron cycle due to their electrochemical properties, but the underlying mechanisms by which their different structure-dominated electron transfer continuously mediates iron autotrophic denitrification (IAD) remain unclear. Therefore, this study explored the influence of structural evolution of pyrogenic carbon on electron transfer and the iron-nitrogen transformation processes. When oxygen-containing functional groups dominated electron transfer, their high abundance (1.14 mmol/g), particularly -OH and C═O, endowed pyrogenic carbon with high electron exchange capacity, facilitating electron transfer for Fe(III) reduction and denitrification processes. As a result, cumulative nitrogen removal increased by 1.67-fold, and the abundances of IAD-related microorganisms and their contributions to functional genes were significantly increased. Moreover, the electron donating capacity increased by 2.51-fold, elevating the Fe(III) reduction rate constant by 3.07-fold and ensuring the long-term utilization of iron. When graphitic structures dominated electron transfer, the electrical conductivity of pyrogenic carbon reached 1.61 S/cm, rapidly facilitating electron transfer in IAD, but the large amount of released iron ions was quickly oxidized and densely covered the carbon and iron surfaces, causing a 54.86% decrease in nitrogen removal. This study provides mechanistic insights into the regulatory effect of different pyrogenic carbons on IAD.
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Hou et al. (2026) studied this question.
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