Chin J Plant Ecol ›› 2026, Vol. 50 ›› Issue (1): 55-69.DOI: 10.17521/cjpe.2024.0417  cstr: 32100.14.cjpe.2024.0417

• Research Articles • Previous Articles     Next Articles

Effects of nitrogen and phosphorus additions on the stability of soil aggregates and their carbon and nitrogen contents in evergreen broadleaf forests

DAI Yun-Ze1,2, YAO Liang-Jin3, CHEN Miao4, XU Xiao-Niu2,*()   

  1. 1 Suzhou Polytechnic Institute of Agriculture, Suzhou, Jiangsu 215008, China
    2 School of Forestry & Landscape Architecture, Anhui Agricultural University, Hefei 230036, China
    3 Zhejiang Academy of Forestry, Hangzhou 310023, China
    4 Ecological Restoration and Conservation on Forest and Wetland Key Laboratory of Sichuan Province, Sichuan Academy of Forestry, Chengdu 610081, China
  • Received:2024-11-22 Accepted:2025-02-26 Online:2026-01-20 Published:2026-02-13
  • Contact: XU Xiao-Niu
  • Supported by:
    National Natural Science Foundation of China(31770672);National Natural Science Foundation of China(31370626);National Key Basic Research Program of China(2010CB950602);General Project of Basic Sciences in Higher Education Institutions in Jiangsu Province(23KJB220009)

Abstract:

Aims Ecosystem reactive nitrogen (N) and phosphorus (P) inputs induced by recent industrial and agricultural development can modify soil carbon (C) storage capacity by affecting soil aggregate structure and stabilization. However, observational studies on modeling the effects of N and P deposition on soil aggregates are still lacking in subtropical regions, with research on P-N interactions being comparatively scarce.

Methods In order to investigate how ecosystem N enrichment and its interactions with P deposition affect C sequestration mechanisms in soil aggregates, N and P addition experiments were conducted for 7 consecutive years in a subtropical forest in southern China. Sample plots of four N addition types were established (control: CK, 0 kg N·hm-2·a-1; low N addition: LN, 50 kg N·hm-2·a-1; N addition: NA, 100 kg N·hm-2·a-1; N and P addition: N+P, 100 kg N·hm-2·a-1 + 50 kg P·hm-2·a-1). Soil properties, soil aggregates and their C, N contents, and C, N stable isotopes composition of aggregates at each aggregate level were determined.

Important findings Evergreen broadleaf forest macroaggregates (diameter > 250 μm) were the dominant soil aggregate size, accounting for 83%-87% of the total soil mass, and LN treatment increased macroaggregate formation, mean mass diameter and mean geometric diameter, while NA and N+P treatments marginally reduced soil aggregate stability. N enrichment in this region primarily increased the C and N contents of aggregate, attributable on an increase in the concentration of these elements at each grain level. The added organic matter was predominantly enriched in macroaggregates, which were characterized by a high C to N ratio and rich 13C abundance. Conversely, excessive N input was detrimental to the stabilization of soil aggregate structure and C sequestration, in comparison with low N addition. The addition of P did not significantly alter the stability of local aggregates or their C and N components. The total soil C, N, and P contents of evergreen broadleaf forests under N addition did not promote soil aggregate formation, and the decrease in pH significantly promoted the increase of C and N contents of aggregates. The results of this study enhance our understanding of the mechanisms of aggregate change, and thus represent important references for predicting the potential of soil C sinks in evergreen broadleaf forests and other areas with similar conditions under future N and P deposition.

Key words: nitrogen and phosphorus addition, evergreen broadleaf forest, soil aggregates, carbon content, nitrogen content, stable isotope