Biochar amendment alleviates soil microbial nitrogen and phosphorus limitation and increases soil heterotrophic...

Nitrogen (N) and carbon (C) inputs substantially affect soil microbial functions. However, the influences of long-term N and C additions on soil microbial resource limitation and heterotrophic respiration-fundamental microbial functional traits-remain unclear, impeding the understanding of how soil C dynamics respond to global change. In this study, the responses of soil microbial resource limitation and heterotrophic respiration (Rh) to 7-year N and biochar (BC) additions in a subtropical Moso bamboo (Phyllostachys edulis) plantation were investigated. We used eight treatments: Control, no N and BC addition; N30, 30 kg N (ammonium nitrate)·hm^-2·a^-1; N60, 60 kg N·hm^-2·a^-1; N90, 90 kg N·hm^-2·a^-1; BC20, 20 t BC (originating from Moso bamboo chips) hm^-2; N30 + BC20, 30 kg N·hm^-2·a^-1 + 20 t BC hm^-2; N60 + BC20, 60 kg N·hm^-2·a^-1 + 20 t BC hm^-2; and N90 + BC20, 90 kg N·hm^-2·a^-1 + 20 t BC hm^-2. Soil microbes were co-limited by N and phosphorus (P) and not limited by C in the control treatments. Long-term N addition enhanced soil microbial N and P limitation but significantly reduced soil Rh by 15.1 %-20.0 % relative to that in the control treatments. BC amendment alleviated soil microbial N and P limitation and significantly decreased C use efficiency by 10.9 %-42.1 % but increased Rh by 33.6 %-91.6 % in the long-term N-free and N-supplemented treatments (P < 0.05). Soil C- and N-acquisition enzyme activities were the dominant drivers of soil microbial resource limitation. Furthermore, microbial resource limitation was a more reliable predictor of Rh than soil resources or microbial biomass. The results suggested that long-term N and BC additions affect Rh by regulating microbial resource limitation, highlighting its significance in understanding soil C cycling under environmental change.