Deeply rooted perennial plants may help build soil carbon (C) stocks, but most research has focused on shallow soils, resulting in gaps in our understanding of how the balance between decomposition and C inputs shifts and drives soil C accumulation with depth. To address this challenge, researchers at the Center for Advanced Bioenergy and Bioproducts Innovation (CABBI) assessed the distribution and assimilation of 13C-labeled simple carbon in meter-deep (3.3-foot-deep) pits under mature perennial miscanthus stands.
Researchers dug five quantitative soil pits under mature miscanthus plots in Urbana, Illinois, separated and quantified fine root biomass by depth, quantified soil C, microbial respiration, and potential nitrogen mineralization and nitrification, and added 13C-labeled glucose to the soils to determine the fate of simple C inputs with depth.
The work is published in the journal Biogeochemistry.
Fine root biomass, total soil C, mineral-associated organic C (MAOC), particulate organic C (POC), and microbial activity declined with depth. POC declined more rapidly than MAOC, resulting in an increase in MAOC:POC with depth. Incorporation of simple 13C inputs into MAOC was similar across depths. However, these inputs led to net MAOC losses in shallow soils and either small losses or gains in deeper soils.
This work suggests that depth gradients in soil C stocks represent a balance among inputs, decomposition and microbial necromass production and that increases in root C inputs by deep-rooted plants may have the potential to build stable MAOC.
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