Nitrogen addition reshapes elemental distribution within soil aggregates: availability and stoichiometry of carbon–nitrogen-phosphorus-sulfur in a mown meadow steppe
摘要
Anthropogenic nitrogen (N) enrichment and grassland management strongly influence soil elemental cycling and stoichiometric balance. Our study aimed to elucidate how N enrichment and mowing influence elemental distribution across soil aggregate fractions.
MethodsBased on a 7-year field experiment, we quantified how N addition (0–50 g m−2 yr−1 as (NH4)2SO4) and mowing altered carbon (C), N, phosphorus (P), and sulfur (S) availability and stoichiometry across soil aggregate fractions in a Eurasian meadow steppe.
ResultsSoil pH decreased by 0.68–1.85 units and reduced microbial biomass C under N application, accompanied by marked increases in available N, P, and S. Small macroaggregates (250–2000 μm) were enriched in total C, N, and P, whereas microaggregates (< 250 μm) had the highest total S concentrations and maintained the most stable element stoichiometry. It significantly reduced total elemental ratios of C:N, C:S, N:S, and P:S while increasing N:P under N addition, with mowing generally amplifying these stoichiometric responses under higher N input.
ConclusionOur findings demonstrate that N enrichment reshapes elemental stoichiometry within soil aggregates by modifying soil pH and shifts labile nutrient availability. Mowing amplifies these effects under high N input, leading to hierarchical responses across soil aggregates, with macroaggregates more sensitive and microaggregates more stable, highlighting the importance of incorporating management interactions and aggregate-level heterogeneity into biogeochemical models and grassland management.