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The river Trave is characterised by its low sedimentation rate of approximately 10,000 m3 per year.
These horizons are likely the result of cumulative incorporation of organic material under conditions of particularly low sedimentation rates.
None of the scenarios shows the ideal combination of high flood peak reduction, low sedimentation, and high biodiversity.
The electrostatic repulsion between the particles is responsible for the low sedimentation volume and poor redispersibility of the drug.
The electrostatic repulsion between the particles is responsible for the low sedimentation volume and easy redispersibility of the polymer.
Additionally, low sedimentation rates, c, were determined for both single and mixed cultures: 0.33 to 0.63 h−1 and 0.24 to 0.94 h−1, respectively.
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Lowest sedimentation was associated with the flood with the smallest peak discharge, peak sediment concentration and sediment load.
The lowest sedimentation rate, viscosity, density and D32 were achieved in the minimum concentrations of salt and dry matter.
The highest sedimentation rate using Duboys is 2.06 lb-sec/ft was obtained at Station 3 and the lowest sedimentation rate is 0.073 lb-sec/ft also at Station 3 but in different day.
The lowest sedimentation coefficients implying the weakest interaction were obtained with the mutants T37E, S95E, S410E, and Y354E.
During stage (2), bank-excavated blocks were redistributed in the channel, which aided the appearance of gravel mesoforms within depressions on the channel bed and subsequent low stage sedimentation leading to the formation of channel element CH2.
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