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Nitrogen is an essential plant nutrient that also shapes soil properties and microbial communities, but its interactions with residual organic pollutants remain poorly resolved. In a 15-year field experiment, we evaluated four nitrogen (N) fertilization rates and collected surface soil (0-20 cm) to determine their effects on soil physicochemical properties, microbial community structure, exploratory co-occurrence networks, metagenomic functional profiles, and residual polycyclic aromatic hydrocarbons (PAHs). Relative to the control (CK), total N and Ca concentrations in the high-N treatment (N3) were 2.25 and 1.38 times higher, respectively. N addition was associated with differences in exploratory microbial network topology: in N3, average degree increased by 15% for bacteria and 31% for fungi, whereas in the low-N treatment (N1), modularity decreased by 12% and 30%, respectively. High N also showed a higher relative representation of genes assigned to carbon metabolism and changes in the relative abundance of genes in the PAH-degradation pathway (ko00624). Mantel tests indicated treatment-dependent associations between microbial community composition and residual PAH profiles, particularly under low N. Overall, long-term N fertilization was associated with shifts in soil microbial communities and their functional potential related to carbon, nitrogen, and PAH metabolism. These association-based results do not demonstrate pathway activity, PAH degradation rates, or environmental risk; direct process-rate and bioavailability measurements would be required for those inferences. These findings support site-specific N management that accounts for both crop nutrient demand and the persistence of legacy organic contaminants.
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Xu et al. (2026) studied this question.
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