期刊
WETLANDS
卷 40, 期 5, 页码 1433-1443出版社
SPRINGER
DOI: 10.1007/s13157-020-01286-5
关键词
Tidal salt marshes; Drying-rewetting cycle; CO2 and CH4 emissions; Dissolved organic carbon
资金
- National Nature Science Foundation of China [41671089]
- Science and Technology Service Network Initiative [KFJ-STS-ZDTP-023]
- Key deployment project of Chinese Academy of Sciences [KFZD-SW-112]
- Strategic Priority Research Program of the Chinese Academy of Sciences [XDA23050202]
Tidal salt marshes, as blue carbon ecosystems, play a critical role in mitigation of global climate change since their large soil organic carbon (SOC) pool. Drying-rewetting cycles induced by periodic tides have profound influence on soil carbon cycling in tidal salt marshes. However, the magnitude and mechaanism of the effects of drying-rewetting frequency on SOC loss in tidal salt marshes is still uncertain. Here, we conducted a mesocosm experiment to identify how drying-rewetting frequency changes alter the vertical (CO2 and CH4) and lateral (dissolved organic carbon) carbon losses of soils in a tidal salt marsh in the Yellow River Delta (YRD). We found that increasing soil moisture inhibited CO2 emission but stimulated CH4 emission in a tidal salt marsh. Soil dissolved organic carbon (DOC) was produced in the drying phase and rewetting lead to the loss of DOC. Soil moisture and salinity change induced by drying-rewetting cycles were the critical factors controlling vertical organic carbon loss in a tidal salt marsh. DOC had significant effects on CO2 emissions. Changes of tidal action and drying-rewetting cycle induced by global change can affect the pathway of carbon loss in a tidal salt marsh.
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