Carbon cycle research is the core foundation for understanding the root causes of climate change and developing effective emission reduction strategies. Carbon source-sink dynamics in the water ecologic environment is the key component of the carbon cycle in basins. Jianghan Dongting Plain of the Yangtze River Basin is rich in water resources, but lacks a comprehensive understanding on the carbon source-sink dynamics of water environment. The study integrated literature data and self-tested data to research the carbon source-sink dynamics in surface water and groundwater in the Jianghan Dongting Plain. The study found that there was a coupling effect of HCO3− and DOC between SW (surface water) and GW (groundwater) in the Jianghan-Dongting Plain of the central Yangtze River Basin. The HCO3− in surface water may come from the recharge of groundwater, and the DOC in the groundwater may come from the recharge of surface water. In addition, the high concentration of NH4+-N in groundwater inhibited the release of DOC from the sediment into the groundwater. Decreasing of situation index (SI) values of calcite and dolomite from west to east indicated that under the coupling effect between surface water and groundwater, the water carbonate interaction was enhanced, leading to the carbon sink changing to be carbon source from west to east. The study clarified the spatial pattern of regional carbon effects of “ west sink and east source” for the first time, elevating carbon cycle research from a single water body to a system level of “surface water groundwater continuum”, successfully connecting micro biogeochemical processes with macro regional carbon cycle patterns, which is of great significance for carbon cycling research in the Yangtze River Basin and predicting future environmental changes.
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