Author
Listed:
- Junwei Zhang
(College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China
State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China)
- Tao Du
(School of Water Conservancy and Hydroelectric Power, Hebei University of Engineering, Handan 056038, China
Chinese Hydraulic Engineering Society, Beijing 100053, China)
- Shanshan Liu
(State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China)
- Sintayehu A. Abebe
(Hydraulic and Water Resources Engineering Department, Debre Markos University Institute of Technology, Debre Markos 269, Ethiopia)
- Sheng Yan
(State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China
College of Conservancy Engineering, Zhengzhou University, Zhengzhou 450000, China)
- Wei Li
(State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China)
- Tianling Qin
(State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin, China Institute of Water Resources and Hydropower Research, Beijing 100038, China)
Abstract
This study adopted the method of “exchanging space for time” and set up three experimental groups based on the shape, degree of damage, and degree of humification of the litter, namely the undecomposed layer, the semi-decomposed layer, and the decomposed layer. Using typical slopes of arbor and bamboo forests in the Pi River Basin as the research object, from October 2021 to December 2022, the soil carbon release flux was measured by using a closed static chamber gas chromatography method to reveal the carbon release law at the soil–air interface during the decomposition process of litter and quantitatively characterize the dynamic impact of the litter decomposition process on soil carbon release flux. Results showed that soil methane flux remained negative (sink) while soil carbon dioxide flux was positive (source) in both litter-covered and bare soil conditions. The methane and carbon dioxide release from soil was positively correlated with and significantly influenced by environmental factors such as soil moisture content and temperature. The methane release flux from soil showed a linear fitting relationship with soil moisture content and temperature, while the carbon dioxide release flux from soil was more in line with the exponential fitting relationship with soil moisture content and temperature. However, there were significant differences in the roles of various factors under different types of litter.
Suggested Citation
Junwei Zhang & Tao Du & Shanshan Liu & Sintayehu A. Abebe & Sheng Yan & Wei Li & Tianling Qin, 2024.
"Carbon Release Characteristics at Soil–Air Interface under Litter Cover with Different Decomposition Degrees in the Arbor and Bamboo Forests of Pi River Basin,"
Land, MDPI, vol. 13(4), pages 1-19, March.
Handle:
RePEc:gam:jlands:v:13:y:2024:i:4:p:427-:d:1364860
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