Denitrification plays a critical role in mitigating anthropogenic nitrate (NO3–) accumulation in ecosystems. The isotopic composition of NO3– (δ15N and δ18O) serves as a powerful tracer for identifying N sources and transformation processes. Denitrification often superimposed on the isotope effects of NO2– oxidation, resulting in parallel enrichment of δ15N- and δ18O-NO3– (Δδ18O:Δδ15N trajectory) that causes them to be either below or above 1. This study compared the Δδ18O:Δδ15N trajectory during denitrification, functional genes (narG, napA, and nxrA), and carbon sources from metabolites in the Δδ18O:Δδ15N trajectories below or above 1 in unsaturated zones. The results revealed that NO3– reduction was more important for variation in the Δδ18O:Δδ15N trajectory because the difference in isotope effects (15εNO3 reduction and 18εNO3 reduction) between the two Δδ18O:Δδ15N trajectory groups was significant, whereas the difference in isotope effects (15εnxr and 18εnxr) upon NO2– oxidation was not. Carbon sources in the group with Δδ18O:Δδ15N trajectories below 1 facilitated more efficient electron production to promote NO3– reduction because of their low molecular weight and simple structure. Conversely, the lower electron production efficiency due to the high molecular weight and complex structures of carbon sources in the group with Δδ18O:Δδ15N trajectories above 1 downregulated the expression of the three functional genes (narG, napA, and nxrA). The group with Δδ18O:Δδ15N trajectories below 1 showed significantly higher levels of 15εNO3 reduction, 18εNO3 reduction, NO2– oxidation ratio, and copy numbers of narG, napA, and nxrA genes compared to the other group, revealing that NO3– reduction at the cellular level was more active in the former group. This study elucidated the integrated influence of isotope effects, NO3– reductase and NO2– oxidoreductase activities, and carbon sources from metabolites. These findings are significant for understanding the Δδ18O:Δδ15N trajectories of N cycling in terrestrial ecosystems and support groundwater conservation by improving carbon supplementation approaches that stimulate denitrification, with Δδ18O:Δδ15N trajectories serving as effective tracers for assessing denitrification performance in terrestrial environments.
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Microbial denitrification and anaerobic ammonium oxidation (anammox) are two critical processes involved in nitrate (
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