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生态学杂志 ›› 2026, Vol. 45 ›› Issue (8): 2541-2552.doi: 10.13292/j.1000-4890.202608.027

• 研究论文 • 上一篇    下一篇

长白山阔叶红松林土壤温室气体通量的动态变化及其对土壤冻融的响应

施清娴1,2,郭初莹3,张雷明1,2*   

  1. 1中国科学院地理科学与资源研究所, 北京 100101; 2中国科学院大学资源与环境学院, 北京 101408; 3厦门大学环境与生态学院, 福建厦门 361102)

  • 出版日期:2026-08-10 发布日期:2026-08-13

Temporal variations of soil greenhouse gas fluxes and their responses to freeze-thaw cycles in a broadleaved Korean pine forest of Changbai Mountain.

SHI Qingxian1,2, GUO Chuying3, ZHANG Leiming1,2*   

  1. (1Institute of Geographic of Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2College of Resources and Environment, University of Chinese Academy of Sciences, Beijing 101408, China; 3College of the Environment and Ecology, Xiamen University, Xiamen 361102, Fujian, China).

  • Online:2026-08-10 Published:2026-08-13

摘要: 土壤温室气体排放是生态系统碳源汇评估中的重要内容,土壤冻融通过改变土壤碳(C)和氮(N)的循环进而影响了土壤温室气体排放,但目前对春季冻融期土壤温室气体通量的动态变化及其调控因子的认识仍比较缺乏。本研究以长白山温带阔叶红松林为对象,采用静态箱法开展了土壤温室气体通量的定位观测,并分析了土壤环境条件变化对温室气体排放的影响。结果表明,2019—2021年长白山温带阔叶红松林土壤表现为CO2、N2O的排放源和CH4的吸收汇,土壤CO2、CH4和N2O的年均累积量分别为107.96±8.32、-50.99±7.41和10.17±2.41 mmol·m-2·a-1。春季冻融期土壤CO2排放和CH4吸收明显低于生长季,而N2O排放量却远高于生长季。春季冻融期的土壤CO2和CH4的累积通量对全年累积通量的贡献分别为5.51%和8.44%,而N2O通量达到51.43%。多元回归分析显示,春季冻融期CO2通量随着土壤温度升高而增强,而土壤温度对CH4和N2O通量的影响均较小;在生长季,CO2通量主要受土壤温度和表层土壤NO3-含量的显著影响,CH4通量主要受土壤含水量的调控,而N2O通量则受到来自土壤pH的微弱影响。虽然土壤冻融对温室气体排放的动态变化产生了明显作用,但由于受土壤碳氮过程复杂性和土壤异质性的影响,对其动态变化和控制机制仍需开展更多的观测研究,以更准确地评估土壤在生态系统碳汇中的作用。


关键词: 土壤温室气体通量, 土壤冻融, 温带森林, 定位观测, 箱式法

Abstract: Soil greenhouse gas emissions are a critical component in assessing the function of ecosystems as carbon sources and sinks. Soil freeze-thaw cycles influence these emissions by altering soil carbon (C) and nitrogen (N) cycling. However, there remains a limited understanding about the temporal variations in soil greenhouse gas fluxes during freeze-thaw periods and the regulating factors. We conducted in-situ observations of soil greenhouse gas fluxes with the method of static chambers in a temperate broadleaf Korean pine forest in Changbai Mountain, and analyzed the impact of soil variables on greenhouse gas emissions. The results showed that soils acted as a CO2 and N2O source and a CH4 sink during 2019-2021. The annual cumulative fluxes of soil CO2, CH4, and N2O were 107.96±8.32, -50.99±7.41, and 10.17±2.41 mmol·m-2·a-1, respectively. Soil CO2 emission and CH4 uptake during the spring freeze-thaw period were significantly lower than those in the growing season, while N2O emission was much higher. The cumulative fluxes of soil CO2 and CH4 during the spring freeze-thaw period contributed 5.51% and 8.44% to the annual total fluxes respectively, while the contribution of N2O flux reached 51.43%. Multivariate regression analysis revealed that during the spring freeze-thaw period, CO2 fluxes increased with rising soil temperature, and that soil temperature had minimal effects on CH4 and N2O fluxes. In the growing season, CO2 fluxes were primarily influenced by soil temperature and soil NO3- content in surface layer. CH4 fluxes were mainly regulated by soil moisture, while N2O fluxes were weakly affected by soil pH. Soil freeze-thaw exerts a remarkable effect on the temporal variations of greenhouse gas emissions. Considering the complexity of soil C and N cycling and soil heterogeneity, more observations are required on greenhouse gas emissions and control mechanisms to accurately assess the role of soil in ecosystem C sequestration.


Key words: soil greenhouse gas flux, soil freeze-thaw, temperate forest, position observation, static chamber method