Soil organic C fractions at different flooding gradient in the water-level-fluctuating zone of Three Gorges Reservoir Area
The change in soil organic C fraction in wetland ecosystem plays an important role in global climate change. The objective of this study was to character the soil carbon fraction in riparian zone of Three Gorges Reservoir. Three hydrologic gradient sites were chose: permanently flooding site (below 145m), seasonal flooding site (145-175m), and never flooding site (above 175m). The results showed that soil organic carbon (OC), and dissolved organic carbon (DOC) decreased gradually, tended to be lowest in the seasonal flooding site, thereafter they increased significantly with the decreasing duration of flooding, whereas soil microbial biomass carbon (MBC) decreased with duration of flooding. The results indicated that hydrology affected differently the soil organic C fractions.
Water-level-fluctuating Zone OC ROC (Readily oxidizable carbon) DOC MBC
Cao Lei Jia Guo Mei Jia Yan Mei Yu Ji Xin Liao Chang
College of Chemistry & Life Science Three Gorges University Yichang 443002, China
国际会议
哈尔滨
英文
283-285
2012-06-16(万方平台首次上网日期,不代表论文的发表时间)