In paddy fields, water management creates long-term anaerobic conditions in which soil organic carbon (SOC) mineralisation is largely coupled with redox processes. Iron oxides are one of the main minerals in paddy soils, and over 80% of soil anaerobic respiration depends on iron reduction.
Microbial biomass change shifts the role of iron oxides in organic C mineralization in anoxic paddy soil
- 16. 10 2020 (19:18)