植物生态学报 ›› 2025, Vol. 49 ›› Issue (3): 502-512.DOI: 10.17521/cjpe.2024.0178  cstr: 32100.14.cjpe.2024.0178

• • 上一篇    

武夷山中山草甸土壤呼吸组分特征及影响因素

葛小彩1,李锦隆1,孙俊2,武盼盼1,胡丹丹1,程栋梁3,钟全林3   

  1. 1. 福建师范大学
    2. 安庆师范大学资源环境学院
    3. 福建师范大学地理科学学院, 湿润亚热带山地生态国家重点实验室培育基地
  • 收稿日期:2024-05-28 修回日期:2024-10-01 出版日期:2025-03-20 发布日期:2024-10-11

Characteristics of soil respiration components and influencing factors in the Zhongshan meadows of Wuyi Mountain

Xiao-Cai GE1,2, 1,2,Jun Sun3,Pan-Pan WU1,2,dan-dan HU1,2,Dong-Liang CHENG3,Quan-Lin ZHONG   

  • Received:2024-05-28 Revised:2024-10-01 Online:2025-03-20 Published:2024-10-11

摘要: 武夷山中山草甸是亚热带中国东南部分布最高的草甸, 分析亚热带中山草甸土壤碳通量组分的变化特征, 探究其与环境因子的关系及温度敏感性(Q10), 对准确估计区域土壤碳收支和完善对中山草甸碳通量的认识具有重要意义。于2020年5月至2021年4月采用LI-8100 CO2通量测定仪对武夷山山顶草甸土壤呼吸速率(RS)进行监测, 并利用根去除法区分自养呼吸速率(RA)和异养呼吸速率(RH)。结果显示: (1)亚热带武夷山中山草甸土壤呼吸及组分动态均呈双峰曲线, 5-10 月, RS、RA、RH均高与其他月份。全年RA的变异幅度大于RH, RA在RS中占比约45% (2)多模型比较分析表明武夷山中山草甸土壤温度(T)与土壤呼吸及组分呈指数增长关系, 土壤呼吸及各组分的温度敏感系数Q10排序为RA (Q10 = 1.96) > RS (Q10 = 1.94) > RH (Q10 = 1.67)。土壤湿度(W)对RS有一定影响, 但与RA, RH关系不显著。T, W双因素模型对RS的拟合优于单因素模型, 二者可共同解释48%的RS变异。综上, 武夷山中山草甸土壤呼吸以异养呼吸为主, 自养呼吸比异养呼吸对温度更敏感, 土壤温度和湿度是影响武夷山中山草甸土壤呼吸的重要环境因子, 低温和湿度大对呼吸有抑制作用。该研究有助于增强对中山草甸土壤呼吸及组分季节动态和影响因素的认识, 为区域土壤碳通量和碳循环研究提供现实支撑。

关键词: 土壤呼吸, 自养呼吸, 异养呼吸, 温度敏感性, 中山草甸

Abstract: Aims Characterizing the variation of soil carbon flux components in the Zhongshan meadow of Wuyi Mountain, the highest distributed meadows in the subtropical region of southeastern China, and exploring their relationships with environmental factors and temperature sensitivity (Q10) holds significant importance. This research contributes to the accurate estimation of regional soil carbon income and expenditure, refining the understanding of carbon fluxes in Zhongshan meadows. Methods From May 2020 to April 2021, the LI-8100 CO2 flux analyzer was utilized to systematically monitor the soil respiration rate (RS) in the meadow located at the summit of Wuyi Mountain. Additionally, the root exclusion technique was applied to differentiate between the autotrophic respiration rate (RA) and the heterotrophic respiration rate (RH). Important findings (1) The dynamics of RS, RA and RH exhibited bimodal curves, with consistently higher values observed from May to October compared to other months. Notably, RA displayed greater variability than RH throughout the year. RA accounts for 45% of RS. (2) Multi-model comparative analysis suggests that the temperature (T) of the Zhongshan meadow soil in Wuyi Mountain exhibits an exponential growth correlation with soil respiration and its components. The ranking of Q10 values for soil respiration and its components was RA (Q10 = 1.96) > RS (Q10 = 1.94) > RH (Q10 = 1.67). While soil moisture (W) had a certain effect on RS, no significant relationship was observed between RA and RH. The T and W two-factor models demonstrated a better fit for RS compared to the single factor models jointly explaining 48% of the variation in RS. In conclusion, both T and W are important environmental factors influencing soil respiration in Zhongshan meadow. In Zhongshan Meadow of Wuyi Mountain, soil respiration is dominated by heterotrophic respiration, with autotrophic respiration displaying higher sensitivity to temperature changes. Notably, soil temperature and humidity emerge as important environmental factors affecting soil respiration in Zhongshan Meadow of Wuyi Mountain, respiration is inhibited by low temperatures and high humidity. This study helps to enhance the understanding of the seasonal dynamics and influencing factors of soil respiration and its components in the Zhongshan meadow, and also provides practical support for the study of regional soil carbon flux and carbon cycle. Key words soil respiration; autotrophic respiration; heterotrophic respiration; temperature sensitivity (Q10); Zhongshan meadow

Key words: soil respiration, autotrophic respiration, heterotrophic respiration, temperature sensitivity (Q10), Zhongshan meadow