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Chinese Journal of Ecology ›› 2025, Vol. 44 ›› Issue (1): 85-93.doi: 10.13292/j.1000-4890.202501.047

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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

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