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应用生态学报 ›› 2026, Vol. 37 ›› Issue (5): 1488-1496.doi: 10.13287/j.1001-9332.202605.010

• 研究论文 • 上一篇    下一篇

北方林草交错带不同恢复类型植被-土壤碳氮磷化学计量及其驱动因素

闵雪1, 吴叶礼2, 丁国栋1,3,4,5*   

  1. 1北京林业大学水土保持学院, 北京 100083;
    2北京林丰源生态环境规划设计院有限公司, 北京 100083;
    3北京林业大学林业生态工程教育部工程研究中心, 北京 100083;
    4北京林业大学水土保持国家林业和草原局重点实验室, 北京 100083;
    5宁夏盐池毛乌素沙地生态系统国家定位观测研究站, 宁夏盐池 751500
  • 收稿日期:2025-08-11 接受日期:2026-03-25 出版日期:2026-05-18 发布日期:2026-11-18
  • 通讯作者: * E-mail: dch1999@263.net
  • 作者简介:闵 雪, 女, 1997年生, 硕士研究生。主要从事荒漠化防治研究。E-mail: minxue11@163. com
  • 基金资助:
    呼和浩特市森林生态系统碳储量监测评价项目(150101-WWTCG-CS-20220003)

Carbon, nitrogen, and phosphorus stoichiometry of plant and soil and the driving factors across different restoration types of the northern forest-grass land ecotone.

MIN Xue1, WU Yeli2, DING Guodong1,3,4,5*   

  1. 1School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
    2Beijing Linfengyuan Ecological Environment Planning and Design Institute Co., Ltd., Beijing 100083, China;
    3Engineering Research Center of Forestry Ecological Engineering of Ministry of Education, Beijing Forestry University, Beijing 100083, China;
    4Key Laboratory of State Forestry and Grassland Administration on Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China;
    5Yanchi National Observation and Research Station of Maowusu Sandy Land Ecosystem, Yanchi 751500, Ningxia, China
  • Received:2025-08-11 Accepted:2026-03-25 Online:2026-05-18 Published:2026-11-18

摘要: 植被与土壤碳(C)、氮(N)、磷(P)化学计量特征是揭示不同恢复类型植被生态功能发挥差异的重要指标。本研究以北方林草交错带人工乔木林、人工灌木林和天然草地3种典型恢复植被为对象,分析植物组分(叶片、枯落物、根系)及0~100 cm土层土壤C、N、P化学计量特征及其驱动因素。结果表明:植物叶片、枯落物、根系的C平均含量分别为371.60~402.07、378.59~413.66、364.05~406.83 g·kg-1,N平均含量分别为13.23~27.81、9.52~12.06、5.20~13.31 g·kg-1,P平均含量分别为0.85~1.02、0.28~0.82、0.16~0.89 g·kg-1,叶片在养分分配中占主导地位。人工乔木林倾向于高叶片与根系C含量,人工灌木林以高植物组分N含量为特征,而天然草地以高枯落物与根系P含量为特征。C含量在乔木林植物组分间无显著差异,在灌木林和草地中表现为枯落物>叶片>根系,N、P含量在人工植被中主要分配于叶片,而在天然草地中均衡分布。3种植被的表层土壤(0~20 cm)C、N、P含量的均值范围分别为7.45~10.76、0.38~0.54、0.31~0.46 g·kg-1,C/N、C/P、N/P均值范围分别为19.9~24.2、24.1~27.1、1.2~1.5,其中N含量与N/P明显低于中国土壤平均水平,土壤养分存在氮限制;各土层天然草地土壤C含量均显著高于人工植被,人工灌木林土壤P含量显著最低,3种植被间土壤N含量、C/N、C/P和N/P差异不显著。天然草地叶片与根系的N-P间、土壤C-N-P含量间均呈显著正相关,元素协同性较强。冗余分析显示,3种植被的土壤C、N、P化学计量主要受土壤pH、NO3--N及植物组分养分调控,不同植被呈现出特异性响应。综上,天然草地协调开放的养分循环机制,有利于研究区土壤养分涵养与生态系统长期稳定。

关键词: 植被恢复, 叶片, 枯落物, 根, 土壤, 生态化学计量

Abstract: The stoichiometric characteristics of carbon (C), nitrogen (N), and phosphorus (P) in plant and soil are important indicators for ecological functions of vegetation under different restoration types. We analyzed C:N:P stoichiometric characteristics and the driving factors in plant components (leaves, litter, roots) and 0-100 cm soil layers across three typical restored vegetation types in the northern forest-grassland ecotone, including artificial arbor forest, artificial shrub forest, and natural grassland. The results showed that the average C contents in plant leaves, litter, and roots ranged from 371.60 to 402.07, 378.59 to 413.66, and 364.05 to 406.83 g·kg-1; the average N contents ranged from 13.23 to 27.81, 9.52 to 12.06, and 5.20 to 13.31 g·kg-1; and the average P contents ranged from 0.85 to 1.02, 0.28 to 0.82, and 0.16 to 0.89 g·kg-1, respectively. Leaves had the highest nutrient concentrations. Artificial arbor forest tended to have high C contents in leaves and roots. Artificial shrub forest was characterized by high N contents in plant components. Natural grassland featured high P contents in litter and roots. There was no difference in C content among components in arbor forest, but C content followed the order of litter > leaves > roots in shrub forest and grassland. N and P contents were higher in leaves than other tissue in artificial vegetation, but they were evenly distributed across tissues in natural grassland. The average contents of soil C, N, and P in the surface layer (0-20 cm) of the three vegetation types ranged from 7.45 to 10.76, 0.38 to 0.54, and 0.31 to 0.46 g·kg-1; the average C/N, C/P, and N/P ranged from 19.9 to 24.2, 24.1 to 27.1, and 1.2 to 1.5, respectively. Soil N content and N/P were significantly lower than the average level of Chinese soils, indicating N limitation in this area. In all soil layers, soil C content in natural grassland was significantly higher than that in artificial vegetation, soil P content in artificial shrub forest was the lowest, and no significant differences in soil N content, C/N, C/P, and N/P among vegetation types. There were significant positive correlations between N and P in leaves and roots, and among soil C, N, and P contents in natural grassland, showing strong element synergy. Redundancy analysis demonstrated that soil C:N:P stoichiometry were mainly regulated by soil pH, NO3--N, and nutrient contents in plants, with specific responses in different vegetation types. In conclusion, the coordinated and open nutrient cycling of natural grassland is conducive to soil nutrient conservation and long-term ecosystem stability.

Key words: vegetation restoration, leaf, litter, root, soil, ecological stoichiometry