Effect of water-sediment regulation of the Xiaolangdi reservoir on the concentrations, characteristics, and fluxes of suspended sediment and organic carbon in the Yellow River

被引:93
作者
Xia, Xinghui [1 ]
Dong, Jianwei [1 ]
Wang, Minghu [2 ]
Xie, Hui [1 ]
Xia, Na [1 ]
Li, Husheng [1 ]
Zhang, Xiaotian [1 ]
Mou, Xinli [1 ,3 ]
Wen, Jiaojiao [1 ]
Bao, Yimeng [1 ]
机构
[1] Beijing Normal Univ, State Key Lab Water Environm Simulat, Key Lab Water & Sediment Sci, Minist Educ,Sch Environm, Beijing 100875, Peoples R China
[2] Yellow River Conservancy Commiss, Aishan Hydrol Stn, Hydrol & Water Resources Survey Bur Shandong Prov, Liaocheng 252216, Shandong, Peoples R China
[3] Chongqing Three Gorges Univ, Sch Chem & Environm Engn, Chongqing 404100, Peoples R China
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
Suspended sediment; Organic carbon; Water-sediment regulation; Sediment resuspension-deposition; Yellow River; Water conservancy project; POLYCYCLIC AROMATIC-HYDROCARBONS; YANGTZE-RIVER; BLACK CARBON; DISSOLVED CONCENTRATIONS; PARTICULATE MATTER; LOWER REACHES; MEKONG RIVER; IMPACTS; DISCHARGE; HUANGHE;
D O I
10.1016/j.scitotenv.2016.07.015
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Water-sediment regulation (WSR) of the Xiaolangdi Reservoir in the Yellow River is different from other water conservancy projects, with sediment resuspending along the river downstream of the reservoir during water regulation while some suspended sediment depositing during sediment regulation. In this study, samples were collected before, during, and after WSR to investigate the effect of WSR on the suspended sediment and organic carbon downstream of the reservoir. The suspended sediment concentration ([SAS]) increased with the river flow velocity (V) as a power function ([SAS] = 1.348 V-2.519) during the three periods. The suspended sediment grain size decreased along the river during water and sediment regulations and after WSR; they were generally below 200 pm with the fine particles (<50 mu m) of 68.0%-93.7% and positively correlated with the flow velocity. The black carbon content in suspended sediment elevated along the river during both water and sediment regulations, and it increased with 2-50 mu m fraction during water regulation and with <2 mu m fraction during sediment regulation, suggesting that black carbon mainly exists in fine particles and is influenced by both suspended sediment source and characteristics. There was no significant difference in dissolved organic carbon (DOC) concentration during water regulation, sediment regulation, and after WSR, inferring that the effect of sediment resuspension/deposition on DOC concentration was insignificant. The contribution of DOC flux (27.3%) during WSR period to the annual flux was comparable to that (22.6%) of water, but lower than the sediment (32.5%) and particulate organic carbon (POC) (49.5%). This study suggests that WSR will exert significant influence on the concentrations, characteristics and fluxes of POC (p < 0.05) and sediment (p < 0.05) but have no significant influence on DOC (p > 0.1) of the Yellow River. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:487 / 497
页数:11
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