植物生态学报 ›› 2026, Vol. 50 ›› Issue (1): 55-69.DOI: 10.17521/cjpe.2024.0417

• 研究论文 • 上一篇    下一篇

氮磷添加对常绿阔叶林土壤团聚体稳定性及其碳氮含量的影响

戴允泽1,2, 姚良锦3, 陈淼4, 徐小牛2,*()   

  1. 1 苏州农业职业技术学院, 苏州 215008
    2 安徽农业大学林学与园林学院, 合肥 230036
    3 浙江省林业科学研究院, 杭州 310023
    4 四川省林业科学研究院森林和湿地生态恢复与保育四川省重点实验室, 成都 610081
  • 收稿日期:2024-11-22 接受日期:2025-02-26 出版日期:2026-01-20 发布日期:2026-02-13
  • 通讯作者: *徐小牛(xnxu2007@ahau.edu.cn)
  • 基金资助:
    国家自然科学基金(31770672);国家自然科学基金(31370626);国家重点基础研究发展计划(2010CB950602);江苏省高等学校基础科学研究面上项目(23KJB220009)

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 (xnxu2007@ahau.edu.cn)
  • 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)

摘要:

近代工农业发展引起的生态系统活性氮(N)和磷(P)输入可以通过影响土壤团聚体结构及其稳定性, 改变土壤储碳(C)能力。目前, 亚热带地区还缺少关于模拟N、P沉降对土壤团聚体影响的观测研究, 且较少关注P沉降与N沉降的相互作用。为了探明生态系统N富集及其与P沉降相互作用如何影响土壤团聚体固碳机制, 在中国南方亚热带森林中进行了连续7年的N、P添加实验, 实验设计了对照(CK, 0 kg N·hm-2·a-1)、低氮添加(LN, 50 kg N·hm-2·a-1)、氮添加(NA, 100 kg N·hm-2·a-1)、氮磷添加(N+P, 100 kg N·hm-2·a-1 + 50 kg P·hm-2·a-1) 4个处理, 测定了土壤性质、土壤团聚体及其C、N含量和各粒级团聚体C、N稳定同位素组成。结果表明, 常绿阔叶林大团聚体(直径>250 μm)是土壤优势粒级, 占土壤总质量的83%-87%, LN处理增加大团聚体形成和平均质量直径、平均几何直径, 而NA和N+P处理小幅降低土壤团聚体稳定性。该地区N富集主要通过提高各粒级团聚体C、N浓度来增加团聚体C、N含量, 增加的有机质主要富集在大团聚体中。大团聚体主要增加高C:N、富13C的有机质。相比于低N添加, 过量的N输入不利于土壤团聚体结构稳定及其C固存。在N添加条件下, 添加P并未显著改变该地区团聚体稳定性及其碳氮含量。N、P添加下, 常绿阔叶林土壤C、N、P总含量对土壤团聚体形成没有促进作用, 而土壤pH的显著降低对团聚体C、N含量增加有显著的促进意义。该研究结果提高了对常绿阔叶林团聚体变化机制的了解, 从而对预测未来N、P沉降下常绿阔叶林和其他条件相似地区的土壤C汇潜力有重要参考价值。

关键词: 氮磷添加, 常绿阔叶林, 土壤团聚体, 碳含量, 氮含量, 稳定同位素

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