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Chinese Journal of Applied Ecology ›› 2021, Vol. 32 ›› Issue (2): 581-590.doi: 10.13287/j.1001-9332.202102.033

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Co-regulation of rainfall amount and timing on soil carbon mineralization in a typical salt marsh of the Yellow River Delta, China

LI Xue1,2,3, DONG Jie1, LI Pei-guang2,3, WANG Xiao-jie2,3, HAN Guang-xuan2,3, SONG Wei-min2,3*   

  1. 1College of Environment and Planning, Liaocheng University, Liaocheng 252059, Shandong, China;
    2CAS Key Laboratory of Coastal Environmental Processes and Ecological Restoration, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences (CAS), Yantai 264003, Shandong, China;
    3Yellow River Delta Research Station of Coastal Wetland Ecology, Chinese Academy of Sciences, Dongying 257500, Shandong, China
  • Received:2020-06-02 Accepted:2020-10-28 Online:2021-02-15 Published:2021-08-15
  • Contact: *E-mail: wmsong@yic.ac.cn
  • Supported by:
    National Natural Science Foundation of China (41706097), the NSFC-Shandong Union Project (U1906220), and the 13th Five-year Informatization Plan of Chinese Academy of Sciences (XXH13506)

Abstract: Studying the effects of rainfall regimes such as rainfall amount and timing on soil carbon mineralization is of great importance for our understanding the mechanisms underlying the stability and accumulation of soil carbon in coastal salt marshes. In this study, we examined the responses of soil carbon mineralization (CO2 and CH4 fluxes) from undisturbed soil columns to rainfall events in different seasons (dry and wet seasons) with filed experiments in a primary Suaeda salsa region in the Yellow River Delta salt-marsh wetland, which is far away from the coast and not affected by tides. The results showed that rainfall amount and timing had a significant interaction in affecting soil CO2 flux rates. During the dry season, large rainfall events significantly reduced soil CO2 flux rates but had no significant effect in the wet season, which might be closely related to the significant increase in soil water content and salinity. Rainfall amount, rainfall timing and their interactions had no significant effect on soil CH4 efflux rates. Rainfall timing and rainfall amount did not affect CH4/CO2. CH4/CO2 increased with increasing soil water content and salinity. Soil water content and soil salinity showed similar increases to increasing rainfall amount. Our results suggested that the changing rainfall regime under climate change in the future would have a great impact on soil carbon mineralization and carbon sink function by regulating soil water and salt migration in this region.

Key words: rainfall regime, climate change, the Yellow River Delta, salt marsh, carbon sink, soil carbon mineralization