Hydrodynamic disturbance on phosphorus release across the sediment-water interface in Xuanwu Lake, China

被引:7
作者
Bai, Yu [1 ]
Zeng, Yuhong [1 ]
Nie, Bei [1 ]
Jiang, Helong [2 ]
Zhang, Xiaofeng [1 ]
机构
[1] Wuhan Univ, Sch Water Resources & Hydropower Engn, Wuhan 430072, Hubei, Peoples R China
[2] Chinese Acad Sci, Nanjing Inst Geog & Limnol, State Key Lab Lake Sci & Environm, Nanjing 210008, Jiangsu, Peoples R China
关键词
eutrophication; hydrodynamic disturbance; lattice Boltzmann method; phosphorus release; shear velocity; CYANOBACTERIAL GROWTH; DIFFUSION; RESUSPENSION; ADSORPTION; CONVECTION; EXCHANGE; MEDIA; FLUX; SEA;
D O I
10.2166/ws.2018.115
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Excess phosphorus in lakes may cause algal blooming, and total phosphorus (TP) is an important index for lake eutrophication. As an important source of TP, lake sediment contributes a lot to TP release. TP release across the sediment-water interface varies with the hydrodynamic conditions of the overlying water, and in this paper the release characteristics of TP under hydrodynamic disturbance has been investigated. The sediment samples from Xuanwu Lake are collected and their release characteristics of TP under varying shear velocity are simulated in laboratory apparatus. Results show that increasing shear velocity contributes to the release of TP from sediment and the combination of varying shear velocity in different stages has a significant influence on the distribution of TP concentration. Further, the lattice Boltzmann method (LBM) is used to simulate the process of TP release from the sediment-water interface and the predicted values agree well with the measured data, which proves that the LBM can be used in simulating the process of TP release from sediment.
引用
收藏
页码:735 / 742
页数:8
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