欢迎访问《应用生态学报》官方网站,今天是

应用生态学报 ›› 2026, Vol. 37 ›› Issue (5): 1365-1373.doi: 10.13287/j.1001-9332.202605.012

• 稳定同位素生态学专栏 • 上一篇    下一篇

毛竹向阔叶林扩张增加了土壤细菌对异养硝化作用的相对贡献

王晓格1,2, 陈志豪1,2, 王兴萌1,2, 王可成1,2, 邹娜3, 张前前1,2, 李永春1,2*   

  1. 1浙江农林大学环境与资源学院, 杭州 311300;
    2森林食物资源挖掘与利用全国重点实验室, 杭州 311300;
    3江西农业大学园林与艺术学院, 南昌 330045
  • 收稿日期:2025-09-11 接受日期:2026-04-02 出版日期:2026-05-18 发布日期:2026-11-18
  • 通讯作者: * E-mail: ycli@zafu.edu.cn
  • 作者简介:王晓格, 女, 2002年生, 硕士研究生。主要从事植物-土壤互作研究。E-mail: xiaogewang2020@163.com
  • 基金资助:
    国家自然科学基金项目(32071742)和浙江省自然科学基金重点项目(LZ22C160005)

Moso bamboo encroachment into broadleaved forest increased the relative contribution of bacterial community to heterotrophic nitrification.

WANG Xiaoge1,2, CHEN Zhihao1,2, WANG Xingmeng1,2, WANG Kecheng1,2, ZOU Na3, ZHANG Qianqian1,2, LI Yongchun1,2*   

  1. 1College of Environment and Resources, Zhejiang A&F University, Hangzhou 311300, China;
    2State Key Laboratory for Development and Utilization of Forest Food Resources, Hangzhou 311300, China;
    3College of Landscape and Art, Jiangxi Agricultural University, Nanchang 330045, China
  • Received:2025-09-11 Accepted:2026-04-02 Online:2026-05-18 Published:2026-11-18

摘要: 细菌和真菌群落是土壤氮循环的核心驱动者,但亚热带毛竹向常绿阔叶林扩张如何改变土壤矿质氮生产过程及细菌和真菌群落的相对贡献尚不清楚。本研究以次生常绿阔叶林和毛竹入侵阔叶林后形成的纯林为研究对象,采用配对试验设计并结合15N同位素示踪和乙炔抑制法,探究毛竹扩张对次生常绿阔叶林土壤氮转化过程的影响及微生物类群的相对贡献。结果表明:真菌在阔叶林土壤总氮矿化作用中发挥主要作用,毛竹林土壤中细菌和真菌群落均对总氮矿化作用有贡献,其中细菌群落的相对贡献(82.9%)高于真菌群落(49.7%)。毛竹向阔叶林扩张后,总氮矿化作用由真菌主导转向细菌主导。毛竹向阔叶林扩张后土壤总硝化速率降低了21.5%,其中主要是降低了细菌群落主导的自养硝化速率。毛竹向阔叶林扩张前后土壤异养硝化速率分别为0.76和0.68 mg·kg-1·d-1,均占总硝化速率的79%以上,表明异养硝化主导了土壤总硝化过程。毛竹向阔叶林扩张后真菌群落对土壤异养硝化的贡献由89%下降到41.5%,细菌群落对异养硝化的贡献由49.3%上升到79%,表明真菌群落主导了阔叶林土壤的异养硝化,而毛竹扩张后细菌群落对土壤异养硝化的贡献增加。本研究为理解毛竹扩张对土壤矿质氮生产过程的影响及其微生物驱动特征提供了理论依据。

关键词: 总氮矿化速率, 异养硝化速率, 自养硝化速率, 微生物群落, 毛竹扩张

Abstract: Bacterial and fungal communities are critical drivers of soil nitrogen cycling. However, it remains unclear how encroachment of Moso bamboo into subtropical evergreen broadleaved forest alters soil nitrogen minerali-zation and the contributions of bacterial and fungal communities. We used a paired experimental design combined with 15N isotope tracing and the acetylene inhibition method to investigate the effects of Moso bamboo expansion on soil nitrogen transformation and the relative contributions of microbial groups. The results showed that fungi community played a major role in driving soil gross nitrogen mineralization in broadleaved forest, whereas both bacterial and fungal communities contributed to gross nitrogen mineralization in bamboo forest, with the relative contribution of bacteria (82.9%) being higher than fungi (49.7%). After Moso bamboo expansion into broadleaved forest, gross nitrogen mineralization shifted from fungal dominance to bacterial dominance. Following the Moso bamboo expansion, the microbial community structure changed and soil gross nitrification rate decreased by 21.5%, mainly due to a reduction in bacterially dominated autotrophic nitrification. Before and after Moso bamboo expansion, soil heterotrophic nitrification rates were 0.76 and 0.68 mg·kg-1·d-1, respectively. Both accounted for more than 79% of the gross nitrification rate, indicating that heterotrophic nitrification dominated the soil gross nitrification process. After Moso bamboo expansion, the contribution of fungi to soil heterotrophic nitrification decreased from 89% to 41.5%, whereas the contribution of bacteria increased from 49.3% to 79%, indicating that fungi dominated heterotrophic nitrification in broadleaved forest before Moso bamboo expansion and bacteria became dominant after expansion. This study would provide theoretical basis for understanding the effects of Moso bamboo expansion on soil nitrogen mineralization and the microbial mechanisms.

Key words: gross nitrogen mineralization rate, heterotrophic nitrification rate, autotrophic nitrification rate, microbial community, Moso bamboo encroachment