Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China
Abstract Background Although soil erosion plays a key role in the carbon cycle, a holistic and mechanistic understanding of the soil erosion process within the cycle is still lacking. The aim of this study was therefore to improve our mechanistic understanding of soil organic carbon (SOC) and soil r...
| Main Authors: | , , , , , , |
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| Format: | Article |
| Language: | English |
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SpringerOpen
2019-08-01
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| Series: | Ecological Processes |
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| Online Access: | http://link.springer.com/article/10.1186/s13717-019-0184-6 |
| _version_ | 1818273051726315520 |
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| author | Tong Li Haicheng Zhang Xiaoyuan Wang Shulan Cheng Huajun Fang Gang Liu Wenping Yuan |
| author_facet | Tong Li Haicheng Zhang Xiaoyuan Wang Shulan Cheng Huajun Fang Gang Liu Wenping Yuan |
| author_sort | Tong Li |
| collection | DOAJ |
| description | Abstract Background Although soil erosion plays a key role in the carbon cycle, a holistic and mechanistic understanding of the soil erosion process within the cycle is still lacking. The aim of this study was therefore to improve our mechanistic understanding of soil organic carbon (SOC) and soil respiration dynamics through an experiment conducted in an eroding black soil farmland landscape in Northeast China. Results The depositional profiles store 5.9 times more SOC than the eroding profiles and 3.3 times more SOC than the non-eroding profiles. A linear correlation between the SOC and 137Cs (Caesium-137) was observed in our study, suggesting that the SOC decreased with increased soil erosion. Furthermore, the fractions of intermediate C and the microaggregate C were lowest at the eroding position and highest at the depositional position. In the depositional topsoil, the input of labile materials plays a promotional role in soil respiration. Conversely, in the subsoil (i.e., below 10 cm), the potential mineralization rates were lowest at the depositional position—due to effective stabilization by physical protection within soil microaggregates. The field results of soil surface respiration also suggest that the depositional topsoil SOC is prone to be mineralized and that SOC at this depositional context is stabilized at subsoil depth. In addition, the high water contents at the depositional position can limit the decomposition rates and stabilize the SOC at the same time. Conclusions The findings from this study support that a majority of the SOC at footslope is stored within most of the soil profile (i.e., below 10 cm) and submitted to long-term stabilization, and meanwhile support that the depositional profile emits more CO2 than the summit due to its high amount and quality of SOC. |
| first_indexed | 2024-12-12T21:51:49Z |
| format | Article |
| id | doaj.art-ad5038a6f0d54b46b5b41442be4daaf9 |
| institution | Directory Open Access Journal |
| issn | 2192-1709 |
| language | English |
| last_indexed | 2024-12-12T21:51:49Z |
| publishDate | 2019-08-01 |
| publisher | SpringerOpen |
| record_format | Article |
| series | Ecological Processes |
| spelling | doaj.art-ad5038a6f0d54b46b5b41442be4daaf92022-12-22T00:10:46ZengSpringerOpenEcological Processes2192-17092019-08-018111010.1186/s13717-019-0184-6Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast ChinaTong Li0Haicheng Zhang1Xiaoyuan Wang2Shulan Cheng3Huajun Fang4Gang Liu5Wenping Yuan6State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal UniversityLe Laboratoire des Sciences du Climat et de l’Environnement, IPSL-LSCECEA/CNRS/UVSQ SaclayState Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal UniversityCollege of Resources and Environment, University of Chinese Academy of SciencesKey Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of SciencesState Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal UniversityGuangdong Province Key Laboratory for Climate Change and Natural disaster Studies, School of Atmospheric Sciences, Sun Yat-sen UniversityAbstract Background Although soil erosion plays a key role in the carbon cycle, a holistic and mechanistic understanding of the soil erosion process within the cycle is still lacking. The aim of this study was therefore to improve our mechanistic understanding of soil organic carbon (SOC) and soil respiration dynamics through an experiment conducted in an eroding black soil farmland landscape in Northeast China. Results The depositional profiles store 5.9 times more SOC than the eroding profiles and 3.3 times more SOC than the non-eroding profiles. A linear correlation between the SOC and 137Cs (Caesium-137) was observed in our study, suggesting that the SOC decreased with increased soil erosion. Furthermore, the fractions of intermediate C and the microaggregate C were lowest at the eroding position and highest at the depositional position. In the depositional topsoil, the input of labile materials plays a promotional role in soil respiration. Conversely, in the subsoil (i.e., below 10 cm), the potential mineralization rates were lowest at the depositional position—due to effective stabilization by physical protection within soil microaggregates. The field results of soil surface respiration also suggest that the depositional topsoil SOC is prone to be mineralized and that SOC at this depositional context is stabilized at subsoil depth. In addition, the high water contents at the depositional position can limit the decomposition rates and stabilize the SOC at the same time. Conclusions The findings from this study support that a majority of the SOC at footslope is stored within most of the soil profile (i.e., below 10 cm) and submitted to long-term stabilization, and meanwhile support that the depositional profile emits more CO2 than the summit due to its high amount and quality of SOC.http://link.springer.com/article/10.1186/s13717-019-0184-6Soil erosionSoil organic carbonSoil respirationSloping farmland |
| spellingShingle | Tong Li Haicheng Zhang Xiaoyuan Wang Shulan Cheng Huajun Fang Gang Liu Wenping Yuan Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China Ecological Processes Soil erosion Soil organic carbon Soil respiration Sloping farmland |
| title | Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China |
| title_full | Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China |
| title_fullStr | Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China |
| title_full_unstemmed | Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China |
| title_short | Soil erosion affects variations of soil organic carbon and soil respiration along a slope in Northeast China |
| title_sort | soil erosion affects variations of soil organic carbon and soil respiration along a slope in northeast china |
| topic | Soil erosion Soil organic carbon Soil respiration Sloping farmland |
| url | http://link.springer.com/article/10.1186/s13717-019-0184-6 |
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