Abstract
Artificial reservoirs have an important role in water management of river systems in terms of flood control, water supply and sediment budgeting. Therefore, it is important to maximize the time of their effective functioning. Sediment budgeting mainly depends on sediment transport dynamics. This article illustrates the impact of the Koronowski Reservoir on suspended sediments transported by the Brda River. The river system and the reservoir represent a typical lowland river environment. Our research is based on hydrological and sedimentological investigations on the reservoir and the river system. Field measurements were used to create the respective hydrological and sediment budgets. Moreover, we carried out bathymetric measurements to generate present day bathymetry and to calculate the reservoir’s capacity. We assessed the silting of the reservoir following the approaches proposed by Goncarov and Stonawski. We show that the size and dynamics of suspended sediments are mainly determined by the hydrological conditions. Moreover, we illustrate that the suspended sediment measurements made with the filtration method correlate with the nephelometric results. Generally, we show that the Koronowski Reservoir is mainly filled up by suspended sediments. We further illustrate that the level of siltation estimated with the empirical formulas deviates significantly from calculations made by bathymetric measurements.
Highlights
The creation of artificial reservoirs results in water retention by inhibiting water outflows, and has serious implications on qualitative and quantitative changes in the circulation of matter and energy in the whole river system
We carried out a detailed study of the suspended sediment dynamics in the Koronowski
Our results for the continuity of suspended sediments on the rivers with artificial reservoirs are confirmed by various authors
Summary
The creation of artificial reservoirs results in water retention by inhibiting water outflows, and has serious implications on qualitative and quantitative changes in the circulation of matter and energy in the whole river system. The impact of reservoirs on the dynamics of sediment transport are quite significant, as documented in various studies in the last decades, for example, Van Rijn [3], Kondolf [4], Łajczak [5], Vörösmarty et al [6], Shotbolt et al [7], Babiński [8], Gierszewski [9], Hu et al [10], Magnuszewski et al [11] and Habel et al [12].
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