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生态学杂志 ›› 2025, Vol. 44 ›› Issue (1): 85-93.doi: 10.13292/j.1000-4890.202501.047

• 研究报告 • 上一篇    下一篇

天津七里海湿地生长季土壤CO2通量及水热因子变化特征

李世勇1,丁虎1,2,3,4,陈静5,韩晓昆1,2,3,薛浩1,华海锋1,郎赟超1,2,3,4*   

  1. 1天津大学地球系统科学学院, 表层地球系统科学研究院, 天津 300072; 2天津市环渤海地球关键带科学与可持续发展重点实验室, 天津 300072; 3天津环渤海滨海地球关键带国家野外科学观测研究站, 天津 300072; 4物质绿色创造与制造海河实验室, 天津 300192; 5天津市宁河区七里海湿地保护中心, 天津 301509)

  • 出版日期:2025-01-10 发布日期:2025-01-14

Characteristics of soil CO2 flux and hydrothermal factors during the growing season in Qilihai wetland, Tianjin.

LI Shiyong1, DING Hu1,2,3,4, CHEN Jing5, HAN Xiaokun1,2,3, XUE Hao1, HUA Haifeng1, LANG Yunchao1,2,3,4*   

  1. (1Institute of Surface-Earth System Science, School of Earth System Science, Tianjin University, Tianjin 300072, China; 2Tianjin Key Laboratory of Earth Critical Zone Science and Sustainable Development in Bohai Rim, Tianjin 300072, China; 3Tianjin Bohai Rim Coastal Earth Critical Zone National Observation and Research Station, Tianjin 300072, China; 4Haihe Laboratory of Sustainable Chemical Transformations, Tianjin 300192, China; 5Qilihai Wetland Conservation Center, Ninghe District, Tianjin 301509, China).

  • Online:2025-01-10 Published:2025-01-14

摘要: 土壤呼吸是陆地CO2排放的重要来源,明确CO2动态及其控制因素对于全球变化研究具有重要意义。然而,目前关于湿地土壤呼吸的原位连续观测相对较少。本研究以环渤海地区的天津七里海湿地土壤为对象,采用CO2通量传感器和土壤温、湿度传感器进行原位连续观测,探究生长季期间(2022年5月1日至9月30日)湿地土壤的CO2通量昼夜和季节变化及水热因子特征,以及CO2通量对土壤水热因子的响应。结果显示,生长季期间土壤CO2通量先增加后降低,其平均值为6.68±2.55 μmol·m-2·s-1。土壤CO2通量与温度呈显著正相关,指数回归关系可以阐明研究期土壤呼吸75.7%的变化,生长季湿地土壤呼吸温度敏感性较强(Q10=3.21)。昼夜尺度上,CO2通量呈单峰型变化,与土壤温度之间具有滞后效应,主要呈现逆时针的变化特征。此外,土壤呼吸与土壤含水率呈弱负相关。在土壤先前水分条件的限制下,降雨初期会出现瞬时的CO2通量峰值,随后在降雨时CO2排放明显受到抑制,在短期降雨结束后土壤CO2通量快速升高。本研究表明,温度是研究区生长季土壤呼吸的首要控制因子,同时土壤呼吸在降雨事件期间也明显受到土壤含水率影响。因此,在未来气候背景下的升温和降雨频率变化可能导致该湿地生态系统土壤碳通量变化更加强烈。


关键词: 湿地, 土壤呼吸, 土壤温度, Q10, 滞后现象, 降雨事件

Abstract: Soil respiration plays a critical role in the CO2 emissions of terrestrial ecosystems. It is of great significance to identify the dynamics of CO2 and its controlling factors for global change research. Nevertheless, continuous in-situ observations of soil respiration in wetlands are relatively rare. In this study, we utilized CO2 flux sensor and soil temperature and moisture sensors to continuously monitor soil respiration in the Qilihai wetland, located in Tianjin, the Bohai Rim. Our objective was to investigate the diurnal and seasonal variations of CO2 flux, hydrothermal factors in wetland soil, and the response of CO2 flux to soil hydrothermal factors during the growing season (May 1 to September 30, 2022). The results showed that soil CO2 flux exhibited a first increasing and then decreasing trend during the growing season, with a mean value of 6.68±2.55 μmol·m-2·s-1. Temperature was positively correlated with soil CO2 flux, which explained 75.7% of the variation in soil respiration during the study period. Moreover, wetland soil demonstrated a strong temperature sensitivity of soil respiration, with a Q10 value of 3.21. On a diurnal scale, CO2 flux displayed a unimodal variation, with a lag effect to soil temperature and a counterclockwise characteristic overall. Additionally, soil respiration exhibited a weak negative correlation with soil water content. With the limitations of initial soil moisture, CO2 flux reached a transient peak at the beginning of rainfall event, followed by a significant reduction in CO2 emissions during the rainfall, and then a rapid increase in CO2 flux at the end of the short-term rainfall. Overall, our results illustrated that soil temperature was the primary controlling factor for soil respiration during the growing season, and soil respiration was also influenced by soil water content during rainfall events. Thus, future warming and rainfall frequency associated with climate change could lead to significant changes in soil carbon fluxes in wetland ecosystems.


Key words: wetland, soil respiration, soil temperature, Q10, hysteresis, rainfall event