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小浪底水库水沙调控对黄河干流悬移质和有机碳浓度、特性及通量的影响。

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.

机构信息

State Key Laboratory of Water Environment Simulation, Key Laboratory for Water and Sediment Sciences of Ministry of Education, School of Environment, Beijing Normal University, Beijing 100875, China.

State Key Laboratory of Water Environment Simulation, Key Laboratory for Water and Sediment Sciences of Ministry of Education, School of Environment, Beijing Normal University, Beijing 100875, China.

出版信息

Sci Total Environ. 2016 Nov 15;571:487-97. doi: 10.1016/j.scitotenv.2016.07.015. Epub 2016 Jul 9.

Abstract

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 ([SPS]) increased with the river flow velocity (V) as a power function ([SPS]=1.348V(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 200μm with the fine particles (<50μm) 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 2-50μm fraction during water regulation and with <2μm 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.

摘要

黄河小浪底水库的水沙调节(WSR)与其他水利工程不同,在调水过程中,水库下游泥沙会重新悬浮,而在调沙过程中则会有部分悬移质泥沙沉积。本研究在调水前后采集了样品,以调查 WSR 对水库下游悬移质和有机碳的影响。在三个时期,悬浮泥沙浓度 ([SPS]) 随水流速度 (V) 呈幂函数增加 ([SPS]=1.348V(2.519))。在水沙调节和 WSR 后,悬浮泥沙粒径沿程减小;它们通常低于 200μm,其中细颗粒 (<50μm) 占 68.0%-93.7%,与流速呈正相关。在水沙调节过程中,悬浮泥沙中的黑碳含量沿程升高,在水调节过程中,黑碳含量随 2-50μm 颗粒增加,而在泥沙调节过程中,黑碳含量随<2μm 颗粒增加,表明黑碳主要存在于细颗粒中,并受悬浮泥沙来源和特性的影响。在水调节、泥沙调节和 WSR 后,溶解有机碳 (DOC) 浓度没有显著差异,这表明泥沙再悬浮/沉积对 DOC 浓度的影响不显著。WSR 期间 DOC 通量(27.3%)对年通量的贡献与水(22.6%)相当,但低于泥沙(32.5%)和颗粒有机碳(POC)(49.5%)。本研究表明,WSR 将对 POC(p<0.05)和泥沙(p<0.05)的浓度、特性和通量产生显著影响,但对黄河 DOC(p>0.1)的影响不显著。

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