环境科学
生物地球化学循环
有机质
氮气
碳循环
总有机碳
碳纤维
生产力
营养物
环境化学
气候变化
生态系统
沉积物
氮气循环
生态学
化学
地质学
生物
宏观经济学
复合数
古生物学
复合材料
经济
有机化学
材料科学
作者
Qibiao Yu,Fang Wang,Weijin Yan,Fengsong Zhang,Shucong Lv,Yanqiang Li
标识
DOI:10.3390/ijerph15122734
摘要
Lakes are a crucial component of the global carbon and nitrogen cycle. As a trend of enhanced human activities and climate change, the mechanisms of burial remain poorly understood. In this study, diverse biogeochemical techniques were applied to analyze the temporal variation of organic carbon and nitrogen burial rates in Chaohu Lake. The results showed that burial rates have ranged from 9.39 to 35.87 g C m−2 yr−1 for carbon and from 1.66 to 5.67 g N m−2 yr−1 for nitrogen since the 1860s. The average rates were 19.6 g C m−2 yr−1 and 3.14 g N m−2 yr−1 after the 1970s, which were significantly higher than the rate before the 1970s, showing an increasing trend. The decrease of C/N ratios as well as organic matter δ13C values indicates that the major organic matter source in sediment has been algal production since the 1970s. The increase of δ15N values indicated that the promotion in productivity was stimulated by nutrient input from sewage and agricultural runoff. The burial rates of organic carbon and nitrogen were significantly positively related to socio-economics and temperature, indicating that Chaohu Lake will become an increasing carbon and nitrogen pool under conditions of enhanced human activities and intensive precipitation.
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