Vujacić, D.

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  • Vujacić, D. (2)
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Author's Bibliography

The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro

Spalević, V.; Barović, G.; Vujacić, D.; Curović, M.; Behzadfar, M.; Djurović, Nevenka; Dudić, B.; Billi, P.

(MDPI AG, 2020)

TY  - JOUR
AU  - Spalević, V.
AU  - Barović, G.
AU  - Vujacić, D.
AU  - Curović, M.
AU  - Behzadfar, M.
AU  - Djurović, Nevenka
AU  - Dudić, B.
AU  - Billi, P.
PY  - 2020
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/5429
AB  - Land use change in all river basins leads to changes in hydrologic response, soil erosion, and sediment dynamics characteristics. Those changes are often viewed as the main cause of accelerated erosion rates. We studied the impact of land use changes on soil erosion processes in one of the watersheds in Montenegro: the Miocki Potok, using this watershed as a pilot river basin for this area. We simulated responses of soil erosion processes by using a process-oriented soil erosion Intensity of Erosion and Outflow (IntErO) model, with different settings of land use for the years 1970, 1980, 1990, 2000, 2010, and 2020. The model provides fast, effective, and affordable insight into the effects of land use change on soil erosion processes. Testing of the applied procedures was important for the further establishment of watershed management methodologies at the national level, for the other 300 river basins of Montenegro. For the current state of land use, calculated peak discharge for the Miocki Potok was 364 m3 s−1 (2020)–372 m3 s−1 (1970) for the incidence of 100 years, and there is a possibility for large flood waves to appear in the studied basin. Real soil losses, Gyear, were calculated at 13680 m3 year−1 (2020) and specific 333 m3 km−2 year−1 (2020). A Z coefficient value of 0.439 (2020) indicated that the river basin belongs to destruction category III. The strength of the erosion process was medium, and according to the erosion type, it was mixed erosion. According to our analysis, the land use changes in the last 50 years influenced a decrease in the soil erosion intensity for 14% in the Miocki Potok River Basin. Further studies should be focused on the detailed analysis of the land use changes trends with the other river basins at the national level, closely following responses of soil erosion to the changed land use structure, and effects of plant-and-soil interaction on soil erosion and sediment dynamics.
PB  - MDPI AG
T2  - Water (Switzerland)
T1  - The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro
EP  - 28
IS  - 11
SP  - 1
VL  - 12
DO  - 10.3390/w12112973
ER  - 
@article{
author = "Spalević, V. and Barović, G. and Vujacić, D. and Curović, M. and Behzadfar, M. and Djurović, Nevenka and Dudić, B. and Billi, P.",
year = "2020",
abstract = "Land use change in all river basins leads to changes in hydrologic response, soil erosion, and sediment dynamics characteristics. Those changes are often viewed as the main cause of accelerated erosion rates. We studied the impact of land use changes on soil erosion processes in one of the watersheds in Montenegro: the Miocki Potok, using this watershed as a pilot river basin for this area. We simulated responses of soil erosion processes by using a process-oriented soil erosion Intensity of Erosion and Outflow (IntErO) model, with different settings of land use for the years 1970, 1980, 1990, 2000, 2010, and 2020. The model provides fast, effective, and affordable insight into the effects of land use change on soil erosion processes. Testing of the applied procedures was important for the further establishment of watershed management methodologies at the national level, for the other 300 river basins of Montenegro. For the current state of land use, calculated peak discharge for the Miocki Potok was 364 m3 s−1 (2020)–372 m3 s−1 (1970) for the incidence of 100 years, and there is a possibility for large flood waves to appear in the studied basin. Real soil losses, Gyear, were calculated at 13680 m3 year−1 (2020) and specific 333 m3 km−2 year−1 (2020). A Z coefficient value of 0.439 (2020) indicated that the river basin belongs to destruction category III. The strength of the erosion process was medium, and according to the erosion type, it was mixed erosion. According to our analysis, the land use changes in the last 50 years influenced a decrease in the soil erosion intensity for 14% in the Miocki Potok River Basin. Further studies should be focused on the detailed analysis of the land use changes trends with the other river basins at the national level, closely following responses of soil erosion to the changed land use structure, and effects of plant-and-soil interaction on soil erosion and sediment dynamics.",
publisher = "MDPI AG",
journal = "Water (Switzerland)",
title = "The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro",
pages = "28-1",
number = "11",
volume = "12",
doi = "10.3390/w12112973"
}
Spalević, V., Barović, G., Vujacić, D., Curović, M., Behzadfar, M., Djurović, N., Dudić, B.,& Billi, P.. (2020). The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro. in Water (Switzerland)
MDPI AG., 12(11), 1-28.
https://doi.org/10.3390/w12112973
Spalević V, Barović G, Vujacić D, Curović M, Behzadfar M, Djurović N, Dudić B, Billi P. The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro. in Water (Switzerland). 2020;12(11):1-28.
doi:10.3390/w12112973 .
Spalević, V., Barović, G., Vujacić, D., Curović, M., Behzadfar, M., Djurović, Nevenka, Dudić, B., Billi, P., "The impact of land use changes on soil erosion in the river basin of miocki potok, montenegro" in Water (Switzerland), 12, no. 11 (2020):1-28,
https://doi.org/10.3390/w12112973 . .
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Channel morphology changes in the river Pestan, Serbia

Djeković, V.; Milošević, N.; Andjelković, A.; Djurović, Nevenka; Barović, G.; Vujacić, D.; Spalević, V.

(Scibulcom Ltd., 2016)

TY  - JOUR
AU  - Djeković, V.
AU  - Milošević, N.
AU  - Andjelković, A.
AU  - Djurović, Nevenka
AU  - Barović, G.
AU  - Vujacić, D.
AU  - Spalević, V.
PY  - 2016
UR  - http://aspace.agrif.bg.ac.rs/handle/123456789/4211
AB  - The formation of a river channel stream profile in natural conditions is a long process that lasts for hundreds of years. Research at experimental sections of streams is necessary to discover the initial phases of river beds morphological development. In order to achieve this, this study focused on the period after regulatory earth works. From this initial period, the earthy regulated channel is left to the natural processes of morphological formation. This paper presents the research on morphological changes in the Pestan River (H min, 44 degrees 26'08.4" N 20 degrees 15'23.2" E) from 1978 to 2013, after the regulatory works. One of the possible reasons for permanent morphological changes is reaching the balance between transport and disposition of river sediment, and transport capacity of the stream. The experimental stream reach is located upstream from the mouth of the Pestan into the Kolubara. The goal of the research was to determine the causes of steady morphological changes of the regulated channel, from the initial phase, after the regulatory works, until today.
PB  - Scibulcom Ltd.
T2  - Journal of Environmental Protection and Ecology
T1  - Channel morphology changes in the river Pestan, Serbia
EP  - 1213
IS  - 3
SP  - 1203
VL  - 17
UR  - https://hdl.handle.net/21.15107/rcub_agrospace_4211
ER  - 
@article{
author = "Djeković, V. and Milošević, N. and Andjelković, A. and Djurović, Nevenka and Barović, G. and Vujacić, D. and Spalević, V.",
year = "2016",
abstract = "The formation of a river channel stream profile in natural conditions is a long process that lasts for hundreds of years. Research at experimental sections of streams is necessary to discover the initial phases of river beds morphological development. In order to achieve this, this study focused on the period after regulatory earth works. From this initial period, the earthy regulated channel is left to the natural processes of morphological formation. This paper presents the research on morphological changes in the Pestan River (H min, 44 degrees 26'08.4" N 20 degrees 15'23.2" E) from 1978 to 2013, after the regulatory works. One of the possible reasons for permanent morphological changes is reaching the balance between transport and disposition of river sediment, and transport capacity of the stream. The experimental stream reach is located upstream from the mouth of the Pestan into the Kolubara. The goal of the research was to determine the causes of steady morphological changes of the regulated channel, from the initial phase, after the regulatory works, until today.",
publisher = "Scibulcom Ltd.",
journal = "Journal of Environmental Protection and Ecology",
title = "Channel morphology changes in the river Pestan, Serbia",
pages = "1213-1203",
number = "3",
volume = "17",
url = "https://hdl.handle.net/21.15107/rcub_agrospace_4211"
}
Djeković, V., Milošević, N., Andjelković, A., Djurović, N., Barović, G., Vujacić, D.,& Spalević, V.. (2016). Channel morphology changes in the river Pestan, Serbia. in Journal of Environmental Protection and Ecology
Scibulcom Ltd.., 17(3), 1203-1213.
https://hdl.handle.net/21.15107/rcub_agrospace_4211
Djeković V, Milošević N, Andjelković A, Djurović N, Barović G, Vujacić D, Spalević V. Channel morphology changes in the river Pestan, Serbia. in Journal of Environmental Protection and Ecology. 2016;17(3):1203-1213.
https://hdl.handle.net/21.15107/rcub_agrospace_4211 .
Djeković, V., Milošević, N., Andjelković, A., Djurović, Nevenka, Barović, G., Vujacić, D., Spalević, V., "Channel morphology changes in the river Pestan, Serbia" in Journal of Environmental Protection and Ecology, 17, no. 3 (2016):1203-1213,
https://hdl.handle.net/21.15107/rcub_agrospace_4211 .
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