EGU26-11867, updated on 14 Mar 2026
https://doi.org/10.5194/egusphere-egu26-11867
EGU General Assembly 2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Wednesday, 06 May, 10:45–12:30 (CEST), Display time Wednesday, 06 May, 08:30–12:30
 
Hall X3, X3.118
Rapid Electron Transfer at the Organo–OrganicInterface: Black Carbon-Mediated Electron Shuttling Enhances ROS Generation during Solid Organic Matter Oxidation
Jiabao Sun, yao du, yu chen, teng ma, and yanxin wang
Jiabao Sun et al.
  • china university of geosciences, Institute of Geological Survey, China (sjb@cug.edu.cn)

Black carbon (BC) is produced by incomplete biomass combustion and serves as a key electron shuttle in subsurface environments, where it coexists with reduced solid organic matter (SOMred). However, the role of BC’s abundant redox moieties in mediating electron transfer from SOMred to O2 during redox fluctuations remains unexplored. In this study, four BC types were prepared from distinct biomass precursors (pine wood and zein) at different pyrolysis temperatures (500°C and 800°C). BC enhanced hydroxyl radical (•OH) production by 1.2–1.8 fold compared with SOMred alone. Notably, a two-electron transfer pathway dominated •OH formation in both systems. BC amplified •OH production mainly by promoting electron release from the solid phase of SOMred. Characterization and model experiments revealed that graphite crystallites accelerated electron transfer, while quaternary N groups increased electron release from SOMred, as demonstrated by electrochemical analysis and DFT calculation. This •OH-enhancement process further facilitated As(III) removal. These findings highlight BC’s significant potential to mediate solid-phase electron transfer in SOM-rich environments.

How to cite: Sun, J., du, Y., chen, Y., ma, T., and wang, Y.: Rapid Electron Transfer at the Organo–OrganicInterface: Black Carbon-Mediated Electron Shuttling Enhances ROS Generation during Solid Organic Matter Oxidation, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-11867, https://doi.org/10.5194/egusphere-egu26-11867, 2026.