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Soil organic nitrogen (N) mineralization not only supports ecosystem productivity but also weakens carbon and N accumulation in soils. Recalcitrant (mainly mineral‐associated organic matter) and labile (mainly particulate organic matter) organic materials differ dramatically in nature. Yet, the patterns and drivers of recalcitrant (MNrec) and labile (MNlab) organic N mineralization rates and their consequences on ecosystem N retention are still unclear. By collecting MNrec (299 observations) and MNlab (299 observations) from 57 15N tracing studies, we found that soil pH and total N were the master factors controlling MNrec and MNlab, respectively. This was consistent with the significantly higher rates of MNrec in alkaline soils and of MNlab in natural ecosystems. Interestingly, our analysis revealed that MNrec directly stimulated microbial N immobilization and plant N uptake, while MNlab stimulated the soil gross autotrophic nitrification which discouraged ammonium immobilization and accelerated nitrate production. We also noted that MNrec was more efficient at lower precipitation and higher temperatures due to increased soil pH. In contrast, MNlab was more efficient at higher precipitation and lower temperatures due to increased soil total N. Overall, we suggest that increasing MNrec may lead to a conservative N cycle, improving the ecosystem services and functions, while increasing MNlab may stimulate the potential risk of soil N loss. [ABSTRACT FROM AUTHOR]

A 15 N tracing study was conducted with soils from a long-term nitrogen (N) fertilization experiment to quantify the concurrent gross N transformation rates in soil and the underlying mechanisms for crop yield and N2O emission variability. The treatments were chemical fertilization (NPK, NP, PK, NK), organic fertilization (OF), half chemical/organic fertilization (HOF), and no fertilization (control, CK). The results showed that 30 years of repeated organic or chemical N applications significantly stimulated gross rates of N mineralization and autotrophic nitrification compared with CK. In addition, gross rates of N mineralization (except NP) and autotrophic nitrification (except CK, PK) in all treatments were significantly higher in 2019 (30 years) than in 2007 (18 years). However, the immobilization of mineral N decreased significantly (near to zero) after 30 years of repeated N applications compared to CK or the results of 18 years. The highest maize yields were observed in NPK, but they were not significantly different from HOF yields. The OM yields significantly increased with the duration of the experiment and reached values comparable to NPK yields after more than 12 years of repeated N applications. There was a logarithmic positive relationship between maize yields and gross N mineralization rates (p < 0.01), indicating that it was the key factor explaining the variations in yields. Long-term organic or chemical N applications significantly stimulated N2O emission rates, in line with the stimulation of gross autotrophic nitrification rates. Highest N2O emissions were associated with the organic fertilization treatments. Considering the most suitable climate-smart agricultural practice, taking into account yield, N2O emissions, and carbon sequestration, the combination of organic and chemical N fertilizers can be recommended for the region where the study was carried out. [ABSTRACT FROM AUTHOR]