Abstract
Pyrogenic carbon is widely regarded as a component of soil organic carbon, yet how small amounts of vertically redistributed pyrogenic carbon influence organo mineral interfaces in subsoils remains unresolved. Here we combine a ten year field ageing experiment along a 200 cm calcareous soil profile in China with electrochemical assays, spectroscopy and nanoscale microscopy to link pyrogenic carbon electron transfer capacity to mineral association. Redistributed pyrogenic carbon retains electron accepting and donating capacities in subsoils despite low concentrations and exhibits faster electron transfer kinetics. This retention reflects oxidative surface transformation, enriching quinone and phenolic redox moieties and mineral complexing oxygen groups. Nanoscale observations show oxidised subsoil pyrogenic carbon surfaces with organo mineral coatings associated with iron and calcium bearing phases, consistent with a coupled redox and sorptive interface rather than passive presence alone. These findings suggest that field-aged pyrogenic carbon contributes to redox coupled mineral stabilisation in calcareous subsoils.
Acknowledgements
Soil samples were collected from the long-term field experiment at Shangzhuang Experimental Station of China Agricultural University, and no additional sampling permission was required. The authors thank Professor Juan Gao and Dr Longgang Chu from the Institute of Soil Science, Chinese Academy of Sciences, for their valuable support with the cyclic voltammetry measurements.
Funding
Y.W. acknowledges support from the Youth Fund of the National Natural Science Foundation of China under grant 42207354, the Young Elite Scientists Sponsorship Program by Beijing Association for Science and Technology under grant BYESS2023124, the China Agriculture Research System of the Ministry of Finance and the Ministry of Agriculture and Rural Affairs under grant CARS23-B15, and the 2115 Talent Development Program of China Agricultural University. J.Y.S. acknowledges support from the National Natural Science Foundation of China under grant 42377305. G.T.L. acknowledges support from the National Natural Science Foundation of China under grant 42177278.
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Wang, Y., Sun, T., Yang, Z. et al. Oxidised pyrogenic carbon sustains electron transfer capacity and organo mineral coupling in subsoils.
Commun Earth Environ (2026). https://doi.org/10.1038/s43247-026-03718-2
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DOI: https://doi.org/10.1038/s43247-026-03718-2
Source: Ecology - nature.com
