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Spatiotemporal Distribution Characteristics of Soil Organic Carbon in Newborn Coastal Wetlands of the Yellow River Delta Estuary
Author(s) -
Yu Junbao,
Dong Hongfang,
Li Yunzhao,
Wu Huifeng,
Guan Bo,
Gao Yongjun,
Zhou Di,
Wang Yongli
Publication year - 2014
Publication title -
clean – soil, air, water
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.444
H-Index - 66
eISSN - 1863-0669
pISSN - 1863-0650
DOI - 10.1002/clen.201100511
Subject(s) - transect , environmental science , estuary , soil carbon , wetland , river delta , total organic carbon , delta , hydrology (agriculture) , carbon sink , soil horizon , floodplain , ecosystem , soil test , soil water , soil science , oceanography , ecology , geology , geotechnical engineering , aerospace engineering , biology , engineering
The distribution and seasonal variation of soil organic carbon (SOC) in newborn coastal wetland of the Yellow River Delta (YRD) estuary at eastern China were studied based on monitoring data in 2009 at two transects from the bank of the Yellow River to the seaside. The results showed that SOC contents of 0–60 cm soil layer in transects ranged from 0.46 to 10.15 g kg −1 and average values of soil profiles ranged from 2.15 to 5.00 g kg −1 . The SOC contents tended to increase from the river flood land to the salt beach, which could be accounted for the organic matters including large algae, the bodies and excretion of marine animals due to the feedback of tides. The significant difference of SOC contents at different vegetation communities was observed, while the difference of SOC in soil profiles was not obvious. The SOC contents in 0–30 cm soil layers decreased with plant growth period, while in 40–60 cm soil layers were relatively stable. The mean soil organic carbon density was 3.05 kg C m −2 in study region, which was much lower than that reported in other ecosystems, and its spatiotemporal variations were consistent with that of SOC content. Further analysis revealed that SOC was positively correlated with total nitrogen and clay contents. Our findings indicated that the newborn coastal wetland in the YRD should be a potential sink of SOC.