原文服务方: 地球化学学报(英文)       
摘要:
Organic carbon (OC) source attribution for cascade reservoir sediments has been identified as a critical gap in understanding the effective carbon sink of inland waters. In this study, nine sediment cores were collected from cascade reservoirs in the Wujiang and Pearl Rivers. We analyzed lignin phenol (Λ8), total organic carbon(TOC) content, and stable carbon isotopic composition (δ13C) of the sediments, focusing on the changes of terrigenous OC, and the variation of OC source in cascade reservoir sediments after damming. Our results showed that the Σ8 and TOC contents decreased from upstream to downstream reservoirs, indicating the significant interception of terrigenous OC by cascade damming. Additionally, the Λ8 content in the Pearl River reservoir sediments was much higher than that in the Wujiang River. From the three-end-member mixing model, we estimated that OC in reservoir sediments mainly comes from soil and plankton. After damming, the proportion of plankton OC in TOC slightly increased in seasonal and annual regulation reservoirs due to the limnetic evolution of the reservoir. These findings suggest that the cascade damming increases the interception capacity of the river to terrigenous OC and nutrients, and that slowing of water velocity caused by damming affected primary productivity and fluvial carbon cycling.
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篇名 Identification of terrigenous and autochthonous organic carbon in sediment cores from cascade reserv
来源期刊 地球化学学报(英文) 学科
关键词 Cascade reservoirs Terrigenous OC Lignin Autochthonous OC Three-end-member mixing model
年,卷(期) 2022,(5) 所属期刊栏目
研究方向 页码范围 753-764
页数 11页 分类号
字数 语种 英文
DOI 10.1007/s11631-022-00551-0
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Cascade reservoirs
Terrigenous OC
Lignin
Autochthonous OC
Three-end-member mixing model
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地球化学学报(英文)
双月刊
2096-0956
52-1161/P
大16开
贵州省贵阳市观水路46号地球化学研究所
1982-01-03
英文
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