Wind-induced sediment resuspension as a potential factor sustaining eutrophication in large and shallow Lake Peipsi

2013 ◽  
Vol 75 (4) ◽  
pp. 559-570 ◽  
Author(s):  
Olga Tammeorg ◽  
Juha Niemistö ◽  
Tõnu Möls ◽  
Reet Laugaste ◽  
Kristel Panksep ◽  
...  
1988 ◽  
Vol 20 (6-7) ◽  
pp. 263-270 ◽  
Author(s):  
K. Otsubo ◽  
K. Muraoka

The dispersion and resuspension of sediments in Takahamairi Bay basin of Lake Kasumigaura were studied by means of field research and numerical simulation. The field data on wind direction and velocity, lake current, water wave, and turbidity were shown. Based on these results, we discuss how precipitated sediments were resuspended in this shallow lake. To predict the turbidity and the depth of bed erosion, a simulation model was established for this lake. The calculated turbidity showed good agreement with the field data. According to the simulated results, the turbidity reaches 200 ppm, and the bed is eroded several millimeters deep when the wind velocity exceeds 12 m/s in the lake.


2015 ◽  
Vol 2015 ◽  
pp. 1-10 ◽  
Author(s):  
Bo Wang ◽  
Qianqian Qi

In the shallow lake ecosystems, the recovery of the aquatic macrophytes and the increase in the water transparency have been the main contents of the ecological restoration. Using the shallow lake ecological degradation and restoration model, CNOP method is adopted to discuss the instability and sensitivity of the ecosystem to the finite-amplitude perturbations related to the initial condition and the parameter condition. Results show that the linearly stable clear (turbid) water states can be nonlinearly unstable with the finite-amplitude perturbations, which represent the nature factors and the human activities such as the excessive harvest of the macrophytes and the sediment resuspension caused by artificially dynamic actions on the ecosystems. The results also support the viewpoint of Scheffer et al., whose emphasis is that the facilitation interactions between the submerged macrophytes and the water transparency are the main trigger for an occasional shift from a turbid to a clear state. Also, by the comparison with CNOP-I, CNOP-P, CNOP, and (CNOP-I, CNOP-P), results demonstrate that CNOP, which is not a simple combination of CNOP-I and CNOP-P, could induce the shallow lake ecosystem larger departure from the same ground state rather than CNOP-I, CNOP-P, and (CNOP-I, CNOP-P).


Hydrobiologia ◽  
2015 ◽  
Vol 760 (1) ◽  
pp. 133-144 ◽  
Author(s):  
Olga Tammeorg ◽  
Jukka Horppila ◽  
Reet Laugaste ◽  
Marina Haldna ◽  
Juha Niemistö

2017 ◽  
Vol 108 ◽  
pp. 2-9 ◽  
Author(s):  
Theis Kragh ◽  
Kaj Sand-Jensen ◽  
Kathrine Petersen ◽  
Emil Kristensen

2017 ◽  
Vol 29 (4) ◽  
pp. 1009-1017 ◽  
Author(s):  
XIAO Wei ◽  
◽  
FU Jingru ◽  
WANG Wei ◽  
WEN Xuefa ◽  
...  

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