scholarly journals Effect of suspended solids on interaction between filter-feeding fish Aristichthys nobilis and zooplankton in a shallow lake using a mesocosm experiment

2016 ◽  
Vol 32 (1) ◽  
pp. 219-227 ◽  
Author(s):  
Meijun Chen ◽  
Feizhou Chen
2018 ◽  
Vol 64 (2) ◽  
pp. 616-631 ◽  
Author(s):  
Ulrike Scharfenberger ◽  
Erik Jeppesen ◽  
Meryem Beklioğlu ◽  
Martin Søndergaard ◽  
David G. Angeler ◽  
...  

Inland Waters ◽  
2018 ◽  
Vol 8 (4) ◽  
pp. 474-487 ◽  
Author(s):  
Camino Fernández-Aláez ◽  
Cristina Trigal ◽  
Jorge García-Girón ◽  
Margarita Fernández-Aláez

2016 ◽  
Vol 187 (4) ◽  
pp. 315-324 ◽  
Author(s):  
Jian Zhou ◽  
Xiaoxia Han ◽  
Boqiang Qin ◽  
C�line Casenave ◽  
Guijun Yang

Hydrobiologia ◽  
2014 ◽  
Vol 752 (1) ◽  
pp. 21-31 ◽  
Author(s):  
Leonardo Lagomarsino ◽  
Nadia Diovisalvi ◽  
José Bustingorry ◽  
Roberto Escaray ◽  
Horacio E. Zagarese

2016 ◽  
Vol 88 ◽  
pp. 256-264 ◽  
Author(s):  
Xiufeng Zhang ◽  
Zhengwen Liu ◽  
Erik Jeppesen ◽  
William D. Taylor ◽  
Lars G. Rudstam

1985 ◽  
Vol 17 (6-7) ◽  
pp. 903-914 ◽  
Author(s):  
R. H. Aalderink ◽  
L. Lijklema ◽  
J. Breukelman ◽  
W. van Raaphorst ◽  
A. G. Brinkman

The mass balance of suspended solids in a shallow lake was modelled as the net result of resuspension and settling. Four different formulations for the flux of resuspension were used. Two equations were based on the conception of wave induced resuspension, the other two used the flow field induced shear stress as the driving force for resuspension. Parameter estimations based on experimental time series of wind velocity and SS concentration produced lower least square values with the models based on flow induced resuspension. The model parameter representing settling was in reasonable accordance with the settling velocity obtained from sediment traps. The spread in results can be explained by a lack of homogeneity and horizontal transport.


2021 ◽  
Author(s):  
Philiphi de Rozari

In 2007/08, a study was undertaken on sediment dynamics in shallow Lake Markermeer, The Netherlands. Firstly, the sediment characteristics median grain size, mud content and loss on ignition showed a spatial as well as water depth related pattern indicating wind-induced sediment transport. Sediment dynamics were investigated in a sediment trap field survey at two stations. Sediment yields, virtually all coming from sediment resuspension, were significantly correlated with wind speeds. Resuspension rates for Lake Markermeer were very high, viz. ca. 1,000 g/m2 day as an annual average, leading to high suspended solids (SS) contents, due to the large lake area and its shallowness (high ‘Dynamic Ratio’). Sediment resuspension behaviour was further investigated in preliminary laboratory experiments using a ‘micro-flume’, applying increasing water currents onto five Lake Markermeer sediments. Resuspension showed a clear exponential behaviour. Finally, a 3-D model was set up for water quality and SS contents in Lake Markermeer; first results showed a good agreement between modelled and actual SS contents. Construction of artificial islands and dams will reduce wind fetches and may be expected to cause a substantial decrease in lake water turbidity.


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