Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland)
The aim of this research was to produce a new methodology for a special river bottom hazard mapping for the stability purposes of the biggest Polish water power plant: Włocławek. During the operation period of the water power plant, an engineering-geological issue in the form of pothole formation on...
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doaj-3819a13afda64ec29f544000288d685d2020-11-25T03:21:26ZengMDPI AGSensors1424-82202020-09-01205004500410.3390/s20175004Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland)Dariusz Popielarczyk0Marian Marschalko1Tomasz Templin2Dominik Niemiec3Isik Yilmaz4Barbara Matuszková5Department of Geodesy, Faculty of Geoengineering, University of Warmia and Mazury, Heweliusza 5, 10-724 Olsztyn, PolandDepartment of Geological Engineering, Faculty of Mining and Geology, VŠB-Technical University of Ostrava, 17 listopadu 15, 708 33 Ostrava, Czech RepublicDepartment of Geodesy, Faculty of Geoengineering, University of Warmia and Mazury, Heweliusza 5, 10-724 Olsztyn, PolandDepartment of Geological Engineering, Faculty of Mining and Geology, VŠB-Technical University of Ostrava, 17 listopadu 15, 708 33 Ostrava, Czech RepublicDepartment of Geological Engineering, Faculty of Engineering, Cumhuriyet University, 58140 Sivas, TurkeyDepartment of Geological Engineering, Faculty of Mining and Geology, VŠB-Technical University of Ostrava, 17 listopadu 15, 708 33 Ostrava, Czech RepublicThe aim of this research was to produce a new methodology for a special river bottom hazard mapping for the stability purposes of the biggest Polish water power plant: Włocławek. During the operation period of the water power plant, an engineering-geological issue in the form of pothole formation on the Wisła River bed in the gravel-sand alluvium was observed. This was caused by increased fluvial erosion resulting from a reduced water level behind the power plant, along with frequent changes in the water flow rates and water levels caused by the varying technological and economic operation needs of the power plant. Data for the research were obtained by way of a 4-year geodetic/bathymetric monitoring of the river bed implemented using integrated GNSS (Global Navigation Satellite System), RTS (Robotized Total Station) and SBES (Single Beam Echo Sounder) methods. The result is a customized river bottom hazard map which takes into account a high, medium, and low risk levels of the potholes for the water power plant structure. This map was used to redevelop the river bed by filling. The findings show that high hazard is related to 5% of potholes (capacity of 4308 m<sup>3</sup>), medium with 38% of potholes (capacity of 36,455 m<sup>3</sup>), and low hazard with 57% of potholes (capacity of 54,396 m<sup>3</sup>). Since the construction of the dam, changes due to erosion identified by the monitoring have concerned approximately 405,252 m<sup>3</sup> of the bottom, which corresponds to 130 Olympic-size pools. This implies enormous changes, while a possible solution could be the construction of additional cascades on the Wisła River.https://www.mdpi.com/1424-8220/20/17/5004bathymetric monitoringalluvial river bottom changesstabilitywater power plant structureGNSS/SBES measurementsriver bottom hazard mapping |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Dariusz Popielarczyk Marian Marschalko Tomasz Templin Dominik Niemiec Isik Yilmaz Barbara Matuszková |
spellingShingle |
Dariusz Popielarczyk Marian Marschalko Tomasz Templin Dominik Niemiec Isik Yilmaz Barbara Matuszková Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) Sensors bathymetric monitoring alluvial river bottom changes stability water power plant structure GNSS/SBES measurements river bottom hazard mapping |
author_facet |
Dariusz Popielarczyk Marian Marschalko Tomasz Templin Dominik Niemiec Isik Yilmaz Barbara Matuszková |
author_sort |
Dariusz Popielarczyk |
title |
Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) |
title_short |
Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) |
title_full |
Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) |
title_fullStr |
Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) |
title_full_unstemmed |
Bathymetric Monitoring of Alluvial River Bottom Changes for Purposes of Stability of Water Power Plant Structure with a New Methodology for River Bottom Hazard Mapping (Wloclawek, Poland) |
title_sort |
bathymetric monitoring of alluvial river bottom changes for purposes of stability of water power plant structure with a new methodology for river bottom hazard mapping (wloclawek, poland) |
publisher |
MDPI AG |
series |
Sensors |
issn |
1424-8220 |
publishDate |
2020-09-01 |
description |
The aim of this research was to produce a new methodology for a special river bottom hazard mapping for the stability purposes of the biggest Polish water power plant: Włocławek. During the operation period of the water power plant, an engineering-geological issue in the form of pothole formation on the Wisła River bed in the gravel-sand alluvium was observed. This was caused by increased fluvial erosion resulting from a reduced water level behind the power plant, along with frequent changes in the water flow rates and water levels caused by the varying technological and economic operation needs of the power plant. Data for the research were obtained by way of a 4-year geodetic/bathymetric monitoring of the river bed implemented using integrated GNSS (Global Navigation Satellite System), RTS (Robotized Total Station) and SBES (Single Beam Echo Sounder) methods. The result is a customized river bottom hazard map which takes into account a high, medium, and low risk levels of the potholes for the water power plant structure. This map was used to redevelop the river bed by filling. The findings show that high hazard is related to 5% of potholes (capacity of 4308 m<sup>3</sup>), medium with 38% of potholes (capacity of 36,455 m<sup>3</sup>), and low hazard with 57% of potholes (capacity of 54,396 m<sup>3</sup>). Since the construction of the dam, changes due to erosion identified by the monitoring have concerned approximately 405,252 m<sup>3</sup> of the bottom, which corresponds to 130 Olympic-size pools. This implies enormous changes, while a possible solution could be the construction of additional cascades on the Wisła River. |
topic |
bathymetric monitoring alluvial river bottom changes stability water power plant structure GNSS/SBES measurements river bottom hazard mapping |
url |
https://www.mdpi.com/1424-8220/20/17/5004 |
work_keys_str_mv |
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