Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas

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 art...

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Main Authors: Dawid Szatten, Michał Habel, Luisa Pellegrini, Michael Maerker
Format: Article
Language:English
Published: MDPI AG 2018-11-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/10/11/1681
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spelling doaj-7c37cc6364ee4e01b5d6dfd86aafb6a82020-11-25T01:56:30ZengMDPI AGWater2073-44412018-11-011011168110.3390/w10111681w10111681Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical FormulasDawid Szatten0Michał Habel1Luisa Pellegrini2Michael Maerker3Department of Revitalization of Waterways, Kazimierz Wielki University in Bydgoszcz, Kościeleckich Square 8, 85-033 Bydgoszcz, PolandDepartment of Revitalization of Waterways, Kazimierz Wielki University in Bydgoszcz, Kościeleckich Square 8, 85-033 Bydgoszcz, PolandDepartment of Earth and Environmental Sciences, Pavia University, Via Ferrata 1, 27100 Pavia, ItalyDepartment of Earth and Environmental Sciences, Pavia University, Via Ferrata 1, 27100 Pavia, ItalyArtificial 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.https://www.mdpi.com/2073-4441/10/11/1681sediment transportsuspended sedimentsreservoir siltingartificial reservoirsKoronowski Reservoirlowland rivers
collection DOAJ
language English
format Article
sources DOAJ
author Dawid Szatten
Michał Habel
Luisa Pellegrini
Michael Maerker
spellingShingle Dawid Szatten
Michał Habel
Luisa Pellegrini
Michael Maerker
Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
Water
sediment transport
suspended sediments
reservoir silting
artificial reservoirs
Koronowski Reservoir
lowland rivers
author_facet Dawid Szatten
Michał Habel
Luisa Pellegrini
Michael Maerker
author_sort Dawid Szatten
title Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
title_short Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
title_full Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
title_fullStr Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
title_full_unstemmed Assessment of Siltation Processes of the Koronowski Reservoir in the Northern Polish Lowland Based on Bathymetry and Empirical Formulas
title_sort assessment of siltation processes of the koronowski reservoir in the northern polish lowland based on bathymetry and empirical formulas
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2018-11-01
description 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.
topic sediment transport
suspended sediments
reservoir silting
artificial reservoirs
Koronowski Reservoir
lowland rivers
url https://www.mdpi.com/2073-4441/10/11/1681
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