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What nutrients in soil enhance microbial carbon build? 


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Nitrogen (N) and phosphorus (P) are crucial nutrients in soil that enhance microbial carbon build. Research indicates that the addition of N and P influences microbial physiology, leading to increased microbial growth and carbon use efficiency (CUE). Moreover, the interaction of crop residue with supplementary nutrients like N, P, and sulfur influences microbial biomass carbon (MBC) and microbial use efficiency, ultimately affecting soil organic matter (SOM) formation. Additionally, the availability of N, P, and potassium (K) impacts soil carbon cycling by influencing microbial stoichiometric constraints to growth and respiration, with labile organic matter further mediating the response to nutrient additions. Overall, N and P play significant roles in enhancing microbial carbon build and influencing soil carbon dynamics.

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Phosphorus (P) enhances microbial carbon build in soil by increasing CO2 and heat production, while nitrogen (N) suppresses it, showing opposing effects on soil microbial metabolism.
Phosphorus (P) additions in tropical soil can increase microbial carbon build, impacting soil CO2 fluxes and microbial biomass, highlighting the importance of nutrient interactions in carbon cycling.
Nitrogen (N) addition in soil enhances microbial carbon build by increasing glucose-C partitioning into anabolic processes, indicating N limitation influences microbial carbon use efficiency.
Nitrogen, phosphorus, and sulfur nutrients in soil enhance microbial carbon build by increasing residue-derived microbial biomass carbon and carbon-use efficiency, promoting soil organic matter formation.
Nitrogen input enhances microbial carbon use efficiency by altering plant-microbe-mineral interactions, leading to increased microbial growth and carbon utilization efficiency in soil.

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