Relationship between soil carbon sequestration and the ability of soil aggregates to transport dissolved oxygen

Zhang, Xiaoxian; Gregory, Andrew S.; Whalley, William R.; Coleman, Kevin; Neal, Andrew L.; Bacq-Labreuil, Aurelie; Mooney, Sacha J.; Crawford, John W.; Soga, Kenichi; Illangasekare, Tissa H.

Abstract

A key finding in soil carbon studies over the past decade is that soil organic carbon (SOC) stabilization is not controlled by its molecular complexity or adsorption to clay, but by its physicochemical protection including occlusion in aggregates and sorption/precipitation with organo-mineral associations. The organo-mineral complexes and the adsorbed SOC can be dissolved microbially under anoxic conditions, which is an important pathway in carbon cycle but has been overlooked by most carbon models. As organo-mineral associations are reported to form in aerobic conditions and can be lost under anaerobic conditions, there should be a positive correlation between SOC and ability of the aggregates to transport dissolved oxygen. We develop a simulation model to test this using soil structural data from two long-term experiments which naturally created a SOC gradient: One is a winter wheat experiment established in 1843 to compare the effects of different fertilizations on the yield of winter wheat and the other one is a ley-arable experiment established in 1948 to investigate the consequence of cropping system changes for ecological yield. Aggregates from different treatments on the two experiments were scanned using X-ray Computed Tomography to simulate oxygen transport using a pore-scale model. We compared porosity and diffusion coefficient of all aggregates and linked them to soil organic carbon measured from the two experiments. The agronomic practice changes which occurred 67 or 172 years ago substantially reshaped the intra-aggregate structure (less than 2mm), and the accrual of SOC is positively correlated with diffusion coefficient of the aggregates to transport oxygen. However, the diffusion coefficient increases with SOC asymptotically, plateauing when SOC exceeds a threshold value. We also found the diffusion coefficient of the aggregates in chemically fertilized soils trended with their porosity approximately in the same way, deviating from those for other non-cropped treatments or fertilized with farmyard manure.

Citation

Zhang, X., Gregory, A. S., Whalley, W. R., Coleman, K., Neal, A. L., Bacq-Labreuil, A., …Illangasekare, T. H. (2021). Relationship between soil carbon sequestration and the ability of soil aggregates to transport dissolved oxygen. Geoderma, 403, Article 115370. https://doi.org/10.1016/j.geoderma.2021.115370

• Journal Article Type: Article
• Acceptance Date: Jul 29, 2021
• Online Publication Date: Aug 4, 2021
• Publication Date: Dec 1, 2021
• Deposit Date: Aug 2, 2021
• Publicly Available Date: Aug 5, 2022
• Journal: Geoderma
• Print ISSN: 0016-7061
• Peer Reviewed: Peer Reviewed
• Volume: 403
• Article Number: 115370
• DOI: https://doi.org/10.1016/j.geoderma.2021.115370
• Keywords: Rothamsted long-term experiments; soil organic carbon; aggregates, transport 41 properties; pore-scale simulation
• Public URL: https://nottingham-repository.worktribe.com/output/5951373
• Publisher URL: https://www.sciencedirect.com/science/article/abs/pii/S001670612100450X