Relating Lake Circulation Patterns to Sediment, Nutrient, and Water Hyacinth Distribution in a Shallow Tropical Highland Lake

被引:2
作者
Kebedew, Mebrahtom G. [1 ,2 ,3 ]
Tilahun, Seifu A. [1 ,4 ]
Zimale, Fasikaw A. [1 ]
Belete, Mulugeta A. [1 ]
Wosenie, Mekete D. [1 ]
Steenhuis, Tammo S. [1 ,3 ]
机构
[1] Bahir Dar Univ, Bahir Dar Inst Technol, Fac Civil & Water Resources Engn, POB 26, Bahir Dar, Ethiopia
[2] Mekelle Univ, Ethiopian Inst Technol Mekelle, Sch Civil Engn, POB 231, Mekelle, Ethiopia
[3] Cornell Univ, Dept Biol & Environm Engn, Ithaca, NY 14853 USA
[4] Int Water Management Inst, PMB CT 112, Accra, Ghana
关键词
Delft3D; flow pattern; Lake Tana; Ethiopia; phosphorus; tracer; aquatic vegetation; impaired water bodies; BLUE NILE BASIN; TANA BASIN; PHOSPHORUS; POLLUTION; QUALITY; TAIHU;
D O I
10.3390/hydrology10090181
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Excess sediment and nutrient losses from intensifying agriculture degrade water quality and boost plant growth. The relationship between circulation patterns, spatial water quality degradation, and water hyacinth infestation is not adequately studied. The objective of this study is, therefore, to investigate the effect of lake circulation patterns on sediment and nutrient distribution and its implication on the spread of water hyacinth in a tropical lake. This study was carried out in Lake Tana, the largest freshwater lake in Ethiopia, where sediment and nutrient concentrations are increasing, and water hyacinths have become a challenge since 2011. The lake circulation pattern was simulated by the Delft3D model based on a bathymetry survey, discharge, and meteorological forcings. To predict the transport path of sediments and dissolved nutrients, an inert tracer was released in the four main river inlets of the lake. Observed lake water level measurements were used to validate the model. Our results show that the lake circulation pattern could explain the transport path of sediment and nutrients and the location of the water hyacinths found in the northeast of the lake. Sediments and nutrients from the largest river, Gilgel Abay, in the southeast of Lake Tana, flow through the two outlets nearby with little sediment deposition due to the relatively short retention time. The phosphorus-rich sediments of the 24 h at 105 degrees C remaining three main rivers joining the lake at the north and east are transported to the northeast. Thus, the management and control of water hyacinths should focus on the northern and eastern catchment areas of Lake Tana.
引用
收藏
页数:16
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