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生态学杂志 ›› 2025, Vol. 44 ›› Issue (2): 417-424.doi: 10.13292/j.1000-4890.202502.030

• 森林生态学专栏 • 上一篇    下一篇

长白山阔叶红松林土壤真菌和细菌N2O排放对施氮和降水变化的响应

张蕾1,雷馥歌1,宿振浩1,杨佳诺1,张悦2,3,郭忠玲1,韩旭1*
  

  1. 1北华大学林学院, 吉林吉林 132013; 2中国科学院沈阳应用生态研究所森林生态与保育重点实验室, 沈阳 110016; 3中国科学院大学, 北京 100049)

  • 出版日期:2025-02-10 发布日期:2025-02-10

Responses of soil fungal and bacterial N2O emissions to nitrogen fertilization and precipitation changes in a broad-leaved Korean pine forest in Changbai Mountains, China.

ZHANG Lei1, LEI Fuge1, SU Zhenhao1, YANG Jianuo1, ZHANG Yue2,3, GUO Zhongling1, HAN Xu1*   

  1. (1Forestry College of Beihua University, Jilin 132013, Jilin, China; 2Key Laboratory of Forest Ecology and Silviculture, Institute of Applied Ecology, Chinese Academy of Sciences, Shenyang 110016, China; 3University of Chinese Academy of Sciences, Beijing 100049, China).

  • Online:2025-02-10 Published:2025-02-10

摘要: 以长白山阔叶红松林长期(8年)施氮和减少降水固定样地土壤为对象,通过室内培养试验,结合抗生素抑制技术,分析真菌和细菌两类土壤微生物N2O排放对施氮和减水的响应。结果表明:对照处理中,土壤N2O排放为0.79 nmol·g-1·h-1,单独减水、施氮处理和同时减水施氮处理均显著促进了土壤N2O的排放,分别为3.55、1.84和1.84 nmol·g-1·h-1,且减水和施氮处理之间存在显著交互作用。其中细菌N2O排放受施氮和减水处理的影响,施氮处理促进细菌N2O排放进而提高土壤总N2O排放量。真菌N2O排放主要受减水处理影响,减水施氮处理促进真菌N2O排放进而提高土壤总N2O排放量。而减水处理所造成的N2O排放增加归因于细菌和真菌的共同作用。在对照、减水和施氮处理中,N2O排放以细菌为主,相对贡献率为90.3%、68.2%和91.1%;而在减水施氮处理中,N2O排放以真菌为主,相对贡献率为68.5%。由此可见,干旱情景下,长期施氮会改变土壤N2O排放的主要微生物种类,直接影响土壤真菌和细菌N2O排放量,进而影响土壤N2O的排放总量,对森林生态系统氮循环过程造成影响。


关键词: 土壤N2O排放, 真菌, 细菌, 氮沉降, 减水

Abstract: Combined with the antibiotic inhibition technique, we examined the responses of soil fungal and bacterial N2O emissions in a laboratory culture experiment. Soil samples were collected from fixed plots with long-term (eight years) nitrogen application and precipitation reduction in a broad-leaved Korean pine forest in Changbai Mountains. Results showed that soil N2O emissions were 0.79 nmol·g-1·h-1 in the control. Nitrogen application, precipitation reduction, and simultaneous precipitation reduction and nitrogen application significantly enhanced soil N2O emissions, which were 3.55, 1.84 and 1.84 nmol·g-1·h-1, respectively. There was a significant interaction between precipitation reduction and nitrogen application. Bacterial N2O emissions were affected by nitrogen application and precipitation reduction. Nitrogen application promoted bacterial N2O emissions, thereby promoting total soil N2O emissions. Fungal N2O emissions were mainly affected by precipitation reduction. Simultaneous precipitation reduction and nitrogen application promoted fungal N2O emissions, thereby promoting total soil N2O emissions. The increase in N2O emissions caused by precipitation reduction treatment was attributed to the interaction of bacteria and fungi. In the control, precipitation reduction, and nitrogen application treatments, N2O emissions were mainly contributed by bacteria, with relative contribution rates of 90.3%, 68.2% and 91.1%, respectively. In the nitrogen application and precipitation reduction treatment, N2O emissions were mainly contributed by fungi, with a contribution rate of 68.5%. Therefore, long-term nitrogen application under drought scenario would alter the main microbial species involved in soil N2O emission, directly affect the amount of N2O emissions from soil fungi and bacteria, thereby affecting total soil N2O emissions, which influence nitrogen cycling in forest ecosystems.

Key words: soil N2O emission, fungi, bacteria, nitrogen deposition, precipitation reduction