Vujanović, Aleksandar

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  • Vujanović, Aleksandar (3)
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Author's Bibliography

Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach

Đorđević, Dejana; Tamás, Enikő Anna; Mihajlović, Ljubiša; Abonyi, Csaba; Vujanović, Aleksandar; Kalocsa, Béla

(MDPI, 2023)

TY  - JOUR
AU  - Đorđević, Dejana
AU  - Tamás, Enikő Anna
AU  - Mihajlović, Ljubiša
AU  - Abonyi, Csaba
AU  - Vujanović, Aleksandar
AU  - Kalocsa, Béla
PY  - 2023
UR  - https://grafar.grf.bg.ac.rs/handle/123456789/3191
AB  - The subject of this study is an approximately 300 km long Middle Danube River reach that
spans from river kilometer (rkm) 1581 in Hungary to (rkm) 1255 in Serbia. The observed drying of
floodplains in Hungary some thirty years ago initiated the hydrological studies. However, problems
related to the navigation route maintenance of the Danube River and those in the water supply of
irrigation and drainage canal networks are now present in the whole free-flowing middle Danube
region. The study aims at investigating the correlation between the observed water level decrease
and recorded incision of the river bed at gauging stations and the indirect estimation of the long-term sediment transport along the sand-bed reach based on the surveillance cross-sections’ data
collected during regular monitoring surveys on the navigable Danube. It starts with hydrological
analyses of the 70-year-long time series of water level and discharge yearly data and continues
with morphological and correlation studies. It ends with the estimation of sediment transport. The
decreasing trend in water levels and the increasing trend in cross-sectional areas are persistent. There is a linear correlation between the two. Longitudinal changes in sediment transport indicate the existence of both degrading and aggrading riverbed reaches.
PB  - MDPI
T2  - Applied Sciences, MDPI, Special Issue: Sediment Transport
T1  - Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach
IS  - Special Issue: Sediment Transport
SP  - 10513
VL  - 13
DO  - 10.3390/app131810513
ER  - 
@article{
author = "Đorđević, Dejana and Tamás, Enikő Anna and Mihajlović, Ljubiša and Abonyi, Csaba and Vujanović, Aleksandar and Kalocsa, Béla",
year = "2023",
abstract = "The subject of this study is an approximately 300 km long Middle Danube River reach that
spans from river kilometer (rkm) 1581 in Hungary to (rkm) 1255 in Serbia. The observed drying of
floodplains in Hungary some thirty years ago initiated the hydrological studies. However, problems
related to the navigation route maintenance of the Danube River and those in the water supply of
irrigation and drainage canal networks are now present in the whole free-flowing middle Danube
region. The study aims at investigating the correlation between the observed water level decrease
and recorded incision of the river bed at gauging stations and the indirect estimation of the long-term sediment transport along the sand-bed reach based on the surveillance cross-sections’ data
collected during regular monitoring surveys on the navigable Danube. It starts with hydrological
analyses of the 70-year-long time series of water level and discharge yearly data and continues
with morphological and correlation studies. It ends with the estimation of sediment transport. The
decreasing trend in water levels and the increasing trend in cross-sectional areas are persistent. There is a linear correlation between the two. Longitudinal changes in sediment transport indicate the existence of both degrading and aggrading riverbed reaches.",
publisher = "MDPI",
journal = "Applied Sciences, MDPI, Special Issue: Sediment Transport",
title = "Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach",
number = "Special Issue: Sediment Transport",
pages = "10513",
volume = "13",
doi = "10.3390/app131810513"
}
Đorđević, D., Tamás, E. A., Mihajlović, L., Abonyi, C., Vujanović, A.,& Kalocsa, B.. (2023). Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach. in Applied Sciences, MDPI, Special Issue: Sediment Transport
MDPI., 13(Special Issue: Sediment Transport), 10513.
https://doi.org/10.3390/app131810513
Đorđević D, Tamás EA, Mihajlović L, Abonyi C, Vujanović A, Kalocsa B. Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach. in Applied Sciences, MDPI, Special Issue: Sediment Transport. 2023;13(Special Issue: Sediment Transport):10513.
doi:10.3390/app131810513 .
Đorđević, Dejana, Tamás, Enikő Anna, Mihajlović, Ljubiša, Abonyi, Csaba, Vujanović, Aleksandar, Kalocsa, Béla, "Estimation of Changes in Sediment Transport along the Free-Flowing Middle Danube River Reach" in Applied Sciences, MDPI, Special Issue: Sediment Transport, 13, no. Special Issue: Sediment Transport (2023):10513,
https://doi.org/10.3390/app131810513 . .
2

Hydrological indicators of the riverbed incision along the free-flowing Danube River reach from Budapest to Slankamen relevant for the lateral connectivity between the river channel and floodplains

Tamás, Enikö Ana; Đorđević, Dejana; Kalocsa, Béla; Vujanović, Aleksandar

(Catholic University of Eichstätt-Ingolstadt, 2021)

TY  - CONF
AU  - Tamás, Enikö Ana
AU  - Đorđević, Dejana
AU  - Kalocsa, Béla
AU  - Vujanović, Aleksandar
PY  - 2021
UR  - https://edoc.ku.de/id/eprint/28094/
UR  - https://grafar.grf.bg.ac.rs/handle/123456789/2446
AB  - Hydrological regime plays a primary role in the sustainable management of floodplains, as floodplain ecosystem dynamics and balance are largely dependent on the dynamics of the flow regime of rivers. In the 1980’s a drying process of floodplains on the lower Danube reach in Hungary became evident while in the 2000s continuous unimpeded water supply of the main canal network in the Danube-Tisza-Danube water supply and drainage canal system became an alarming problem. In view of these problems, the present analysis aims at: 1) recognising hydrological indicators of the incision and/or aggradation of the riverbed, 2) estimating the extent of these processes and the rate of change of the riverbed in time based on these indicators, as well as 3) estimating possible consequent changes in the frequency of extremities. The study has shown that the lateral connectivity is at risk along the whole reach as the deepening of the riverbed still continues and according to some parameters (e.g. the gradient of decrease of mean water levels) is even increasing.
PB  - Catholic University of Eichstätt-Ingolstadt
C3  - Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin
T1  - Hydrological indicators of the riverbed incision along  the free-flowing Danube River reach from Budapest to  Slankamen relevant for the lateral connectivity  between the river channel and floodplains
EP  - 69
SP  - 62
VL  - 43
DO  - https://doi.org/10.17904/ku.edoc.28094
ER  - 
@conference{
author = "Tamás, Enikö Ana and Đorđević, Dejana and Kalocsa, Béla and Vujanović, Aleksandar",
year = "2021",
abstract = "Hydrological regime plays a primary role in the sustainable management of floodplains, as floodplain ecosystem dynamics and balance are largely dependent on the dynamics of the flow regime of rivers. In the 1980’s a drying process of floodplains on the lower Danube reach in Hungary became evident while in the 2000s continuous unimpeded water supply of the main canal network in the Danube-Tisza-Danube water supply and drainage canal system became an alarming problem. In view of these problems, the present analysis aims at: 1) recognising hydrological indicators of the incision and/or aggradation of the riverbed, 2) estimating the extent of these processes and the rate of change of the riverbed in time based on these indicators, as well as 3) estimating possible consequent changes in the frequency of extremities. The study has shown that the lateral connectivity is at risk along the whole reach as the deepening of the riverbed still continues and according to some parameters (e.g. the gradient of decrease of mean water levels) is even increasing.",
publisher = "Catholic University of Eichstätt-Ingolstadt",
journal = "Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin",
title = "Hydrological indicators of the riverbed incision along  the free-flowing Danube River reach from Budapest to  Slankamen relevant for the lateral connectivity  between the river channel and floodplains",
pages = "69-62",
volume = "43",
doi = "https://doi.org/10.17904/ku.edoc.28094"
}
Tamás, E. A., Đorđević, D., Kalocsa, B.,& Vujanović, A.. (2021). Hydrological indicators of the riverbed incision along  the free-flowing Danube River reach from Budapest to  Slankamen relevant for the lateral connectivity  between the river channel and floodplains. in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin
Catholic University of Eichstätt-Ingolstadt., 43, 62-69.
https://doi.org/https://doi.org/10.17904/ku.edoc.28094
Tamás EA, Đorđević D, Kalocsa B, Vujanović A. Hydrological indicators of the riverbed incision along  the free-flowing Danube River reach from Budapest to  Slankamen relevant for the lateral connectivity  between the river channel and floodplains. in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin. 2021;43:62-69.
doi:https://doi.org/10.17904/ku.edoc.28094 .
Tamás, Enikö Ana, Đorđević, Dejana, Kalocsa, Béla, Vujanović, Aleksandar, "Hydrological indicators of the riverbed incision along  the free-flowing Danube River reach from Budapest to  Slankamen relevant for the lateral connectivity  between the river channel and floodplains" in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin, 43 (2021):62-69,
https://doi.org/https://doi.org/10.17904/ku.edoc.28094 . .

Hydrological indicators of the riverbed incision along the free-flowing Danube River reach from Budapest to Slankamen relevant for the lateral connectivity between the river channel and floodplains

Tamás, Enikö Anna; Đorđević, Dejana; Kalocsa, Béla; Vujanović, Aleksandar

(Catholic University of Eichstätt-Ingolstadt, 2021)

TY  - CONF
AU  - Tamás, Enikö Anna
AU  - Đorđević, Dejana
AU  - Kalocsa, Béla
AU  - Vujanović, Aleksandar
PY  - 2021
UR  - https://www.ku.de/fileadmin/150307/43rd_IAD_Conference_Proceedings.pdf
UR  - https://grafar.grf.bg.ac.rs/handle/123456789/2447
AB  - Hydrological regime plays a primary role in the sustainable management of floodplains, as floodplain ecosystem dynamics and balance are largely based on the dynamics of the flow regime of rivers. In the 1980’s a drying process of the floodplains on the lower Danube reach in Hungary became evident. The first statistical analyses were made for the Hungarian reach in 1992, because foresters noticed an alarming drying process of the floodplain forests. Analyses indicated the lowering of the riverbed of the Danube River. It is considered that the river training works were the main reason for the incision of the riverbed. 

To the authors’ knowledge, no comprehensive analysis of the changes in the water regime for the whole alluvial reach of the middle Danube has been made to date. To fill this gap, authors analyse available time series of the water level and discharge data for the free-flowing alluvial reach of the Danube River, downstream of Budapest, Hungary to the confluence of the Tisa River, in Slankamen, Serbia. This analysis aims at: 1) recognising hydrological indicators of the incision and/or aggradation of the riverbed, 2) estimating the extent of the two processes and the rate 
of change of the riverbed in time based on these indicators, as well as 3) estimating possible 
consequent changes in the frequency of extremities (low flows and high flows).
According to the Water Framework Directive (WFD) the „good status” of the Danube River reach must be achieved. As the river and its floodplains constitute a complex ecological system, this can only be done through the harmonisation of the nature protection aspect reconstruction projects, WFD programmes of measures, flood management measures and navigation development.
If traditional river training activities continue, riverbed erosion will persist or increase in the future, 
resulting in slow, but continuous drying of floodplains, that are very important nature conservation 
areas. Consequently, the majority of floodplain reconstruction works’ effects might become negligible, while navigation problems will remain unsolved.
In the EU Floods Directive, natural flood management is an important issue, with a focus on increasing water retention capacities by e.g. the re-connection of rivers with their floodplains and restoration of wetlands which can store flood water and help “slow the flow” of flood waters. In this respect, lateral connectivity is one of the most essential issues, as it is for the species inhabiting floodplains and rivers. However, floodplain lateral connectivity is already severed by the decreasing frequency and extent of inundation. The studied hydrological regime is the most important determinant of floodplain habitats.
PB  - Catholic University of Eichstätt-Ingolstadt
C3  - Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin
T1  - Hydrological indicators of the riverbed incision along the free-flowing Danube  River reach from Budapest to Slankamen relevant for the lateral connectivity  between the river channel and floodplains
SP  - 6
VL  - 43
UR  - https://hdl.handle.net/21.15107/rcub_grafar_2447
ER  - 
@conference{
author = "Tamás, Enikö Anna and Đorđević, Dejana and Kalocsa, Béla and Vujanović, Aleksandar",
year = "2021",
abstract = "Hydrological regime plays a primary role in the sustainable management of floodplains, as floodplain ecosystem dynamics and balance are largely based on the dynamics of the flow regime of rivers. In the 1980’s a drying process of the floodplains on the lower Danube reach in Hungary became evident. The first statistical analyses were made for the Hungarian reach in 1992, because foresters noticed an alarming drying process of the floodplain forests. Analyses indicated the lowering of the riverbed of the Danube River. It is considered that the river training works were the main reason for the incision of the riverbed. 

To the authors’ knowledge, no comprehensive analysis of the changes in the water regime for the whole alluvial reach of the middle Danube has been made to date. To fill this gap, authors analyse available time series of the water level and discharge data for the free-flowing alluvial reach of the Danube River, downstream of Budapest, Hungary to the confluence of the Tisa River, in Slankamen, Serbia. This analysis aims at: 1) recognising hydrological indicators of the incision and/or aggradation of the riverbed, 2) estimating the extent of the two processes and the rate 
of change of the riverbed in time based on these indicators, as well as 3) estimating possible 
consequent changes in the frequency of extremities (low flows and high flows).
According to the Water Framework Directive (WFD) the „good status” of the Danube River reach must be achieved. As the river and its floodplains constitute a complex ecological system, this can only be done through the harmonisation of the nature protection aspect reconstruction projects, WFD programmes of measures, flood management measures and navigation development.
If traditional river training activities continue, riverbed erosion will persist or increase in the future, 
resulting in slow, but continuous drying of floodplains, that are very important nature conservation 
areas. Consequently, the majority of floodplain reconstruction works’ effects might become negligible, while navigation problems will remain unsolved.
In the EU Floods Directive, natural flood management is an important issue, with a focus on increasing water retention capacities by e.g. the re-connection of rivers with their floodplains and restoration of wetlands which can store flood water and help “slow the flow” of flood waters. In this respect, lateral connectivity is one of the most essential issues, as it is for the species inhabiting floodplains and rivers. However, floodplain lateral connectivity is already severed by the decreasing frequency and extent of inundation. The studied hydrological regime is the most important determinant of floodplain habitats.",
publisher = "Catholic University of Eichstätt-Ingolstadt",
journal = "Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin",
title = "Hydrological indicators of the riverbed incision along the free-flowing Danube  River reach from Budapest to Slankamen relevant for the lateral connectivity  between the river channel and floodplains",
pages = "6",
volume = "43",
url = "https://hdl.handle.net/21.15107/rcub_grafar_2447"
}
Tamás, E. A., Đorđević, D., Kalocsa, B.,& Vujanović, A.. (2021). Hydrological indicators of the riverbed incision along the free-flowing Danube  River reach from Budapest to Slankamen relevant for the lateral connectivity  between the river channel and floodplains. in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin
Catholic University of Eichstätt-Ingolstadt., 43, 6.
https://hdl.handle.net/21.15107/rcub_grafar_2447
Tamás EA, Đorđević D, Kalocsa B, Vujanović A. Hydrological indicators of the riverbed incision along the free-flowing Danube  River reach from Budapest to Slankamen relevant for the lateral connectivity  between the river channel and floodplains. in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin. 2021;43:6.
https://hdl.handle.net/21.15107/rcub_grafar_2447 .
Tamás, Enikö Anna, Đorđević, Dejana, Kalocsa, Béla, Vujanović, Aleksandar, "Hydrological indicators of the riverbed incision along the free-flowing Danube  River reach from Budapest to Slankamen relevant for the lateral connectivity  between the river channel and floodplains" in Proceedings of 43rd IAD Conference  Rivers and Floodplains in the  Anthropocene – Upcoming Challenges  in the Danube River Basin, 43 (2021):6,
https://hdl.handle.net/21.15107/rcub_grafar_2447 .