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. 2022 Dec 12;13:7676. doi: 10.1038/s41467-022-34951-w

Fig. 6. Conceptual model illustrating the bioenergetic control of SOC dynamics and its sensitivity to rhizosphere priming across soil depth and mineral reactivity contexts.

Fig. 6

The width of native SOC decomposition arrows is proportional to its rate. The rhizosphere priming intensity represents the magnitude in the acceleration of native SOC decomposition induced by a given density and energy supply of plant roots. Plant image by Alice Trotel.