Seasonal variations in the response of soil respiration to rainfall events in a riparian poplar plantation
| Autor: | Mengxun Zhu, Zuosinan Chen, Jiang Lv, Hang Xu, Zhiqiang Zhang, Hans J. De Boeck |
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| Rok vydání: | 2020 |
| Předmět: |
Environmental Engineering
010504 meteorology & atmospheric sciences Rain 010501 environmental sciences 01 natural sciences Carbon cycle Soil respiration Soil Forest ecology Environmental Chemistry Riparian forest Ecosystem Biology Waste Management and Disposal Water content 0105 earth and related environmental sciences Riparian zone Hydrology geography geography.geographical_feature_category Temperature Soil carbon Pollution Chemistry Populus Environmental science Seasons |
| Zdroj: | The science of the total environment |
| ISSN: | 0048-9697 |
| DOI: | 10.1016/j.scitotenv.2020.141222 |
| Popis: | Rainfall events have profound influence on the soil carbon release in different forest ecosystems. However, seasonal variations in soil respiration (RS) response to rainfall events and associated regulatory processes are not well documented in riparian forest ecosystems to date. We continuously measured soil respiration in a riparian plantation ecosystem from 2015 to 2018 to explore the relationships between soil respiration and rainfall events. Across the 4 years, 83 individual rainfall events were identified for spring, summer and autumn. We found that mean RS rate after rain (post-RS) was significantly higher than that before rain (pre-RS) (p < 0.05) in spring, and the relative change in soil respiration (RSrc) increased against rainfall size due to the stimulation by the significant increases in soil moisture content (ΔSM). In contrast, mean post-RS was lower than pre-RS and RSrc was significantly decreased with the increasing rainfall size (p < 0.01) in summer and autumn. Reduced changes in soil temperature (ΔTS) and increased soil moisture content after rain (post-SM) contributed to the decreased RS due to frequently occurring heavy rain events in summer. Increased ΔSM following rainfall events coupled with groundwater level increase suppressed RSrc in autumn, even though increased ΔTS could offset the negative effects of SM on RS to some extent. In addition, we found that higher post-SM after large rainfall events (>10 mm day−1) changed the response of RS to soil temperature (TS) by reducing the temperature sensitivity (Q10) even in this riparian plantation ecosystem. Our study highlights the importance of integrating seasonal difference in soil respiration response to rainfall events and the impact of large rainfall events on soil C release for estimating forest soil carbon cycling at multiple scales. |
| Databáze: | OpenAIRE |
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