Long-term nitrogen amendments alter soil properties and diazotrophic communities in heavy metal-contaminated soils
Fangming Yu1, Wenjie Wang2, Pu Huang2
1Guangxi Key Laboratory of Environmental Processes and Remediation in Ecologically Fragile Regions, Guangxi Normal University, Guilin 541004, China; University Engineering Research Center of Green Remediation and Low Carbon Development for Lijiang River Basin, Guangxi Normal University, Guilin 541004, China; Key Laboratory of Ecology of Rare and Endangered Species and Environmental Protection (Guangxi Normal University), Ministry of Education, Guilin 541004, China.
Abstract:
Mining activities cause severe nutrient depletion and ecological fragility, strongly constraining the restoration of contaminated soils. Prolonged disturbance disrupts soil nutrient pools and biogeochemical stability, with nitrogen (N) deficiency playing a pivotal role by limiting microbial growth, enzymatic activity, and nutrient cycling recovery. To assess the long-term impacts of N inputs, a three-year pot experiment was conducted using heavy metal-contaminated soils to examine changes in soil physicochemical properties, extracellular enzyme activities, and diazotrophic microbial communities. Nitrogen amendments significantly modified soil pH, total carbon (C) and phosphorus (P), total and available N forms, microbial biomass C and N, and available P, indicating substantial shifts in nutrient status and microbial nutrient availability, with stronger effects under urea treatments. Activities of C-, N-, and P-acquiring enzymes (e.g., β-glucosidase, N-acetylglucosaminidase, and alkaline phosphatase) increased consistently, suggesting enhanced microbial nutrient acquisition and organic matter turnover rather than generalized metabolic stimulation. In contrast, prolonged N fertilization markedly reduced nifH gene abundance, particularly under high-N regimes, indicating suppression of biological N fixation rather than a simple dilution effect of external N inputs. Structural equation modeling further identified ammonium N and soil pH as key regulatory factors, exerting direct and indirect effects on microbial diversity and functional gene expression through microbial biomass and enzyme-mediated nutrient transformations. Overall, our results reveal a trade-off between nutrient supplementation and microbial functional capacity, emphasizing the need for optimized N management to balance nutrient supply with the preservation of microbial functions and to support sustainable recovery of mining-degraded soils.
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