TY  - JOUR
AU  - Radonjić, Jasmina
AU  - Ristić, Ratko
AU  - Polovina, Siniša
PY  - 2016
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/764
AB  - Zaštita zemljišta vegetacijom je primarni faktor za borbu protiv vodne erozije uz neophodnu primenu biotehničkih, tehničkih, administrativnih i planskih mera. Jedan od prvih slivova koji je tretiran radovima za zaštitu od erozije i uređenje bujica je sliv Gradašničke reke. Osnovni parametri za prikaz promena hidrološkog statusa zemljišta su stanje erozije, promena koeficijenta erozije, godišnja produkcija nanosa, specifični godišnji pronos nanosa kroz hidrografsku mrežu, vrednost broja krive oticaja kao i vrednost maksimalnog proticaja. Radovi na zaštiti od erozije i uređenju bujica uticali su na smanjenje vrednosti koeficijenta erozije sa Z=0.99 (jaka erozija) na Z=0.40 (slaba erozija), kao i na redukovanje vrednosti maksimalnog proticaja sa Qmax(1956)=108,12 m3/s na vrednost do Qmax(2014)=87.2 m3/s.
AB  - Protection of land with vegetation is the primary factor in the fight against water erosion with necessary application of biotechnical, technical, administrative and planning measures. One of the first basins to be treated with works for the protection against erosion and torrent control is the Gradasnica River basin. The basic parameters to display the changes of the hydrological status of the land are the state of erosion, the change of erosion-coefficient, annual sediment yield, specific annual sediment discharge through the hydrographic network, the value of the runoff curve number and value of the maximal discharge. Works on protection from erosion and regulations of torrents have influenced the decrease in erosion coefficient values from strong erosion (Z=0.99) to the value of weak erosion (Z=0.40), as well as the reduction of the maximum discharge value from Qmax(1956)=108,12m3/s to the value of Qmax(2014)=87.2 m3/s.
PB  - Univerzitet u Beogradu - Šumarski fakultet, Beograd
T2  - Glasnik Šumarskog fakulteta
T1  - Promene hidrološkog statusa sliva usled primene protiverozionih radova
T1  - Changes in the hydrological status of the basin due to the application of erosion control works
EP  - 200
IS  - 114
SP  - 189
DO  - 10.2298/GSF1614189R
UR  - conv_448
ER  - 

@article{
author = "Radonjić, Jasmina and Ristić, Ratko and Polovina, Siniša",
year = "2016",
abstract = "Zaštita zemljišta vegetacijom je primarni faktor za borbu protiv vodne erozije uz neophodnu primenu biotehničkih, tehničkih, administrativnih i planskih mera. Jedan od prvih slivova koji je tretiran radovima za zaštitu od erozije i uređenje bujica je sliv Gradašničke reke. Osnovni parametri za prikaz promena hidrološkog statusa zemljišta su stanje erozije, promena koeficijenta erozije, godišnja produkcija nanosa, specifični godišnji pronos nanosa kroz hidrografsku mrežu, vrednost broja krive oticaja kao i vrednost maksimalnog proticaja. Radovi na zaštiti od erozije i uređenju bujica uticali su na smanjenje vrednosti koeficijenta erozije sa Z=0.99 (jaka erozija) na Z=0.40 (slaba erozija), kao i na redukovanje vrednosti maksimalnog proticaja sa Qmax(1956)=108,12 m3/s na vrednost do Qmax(2014)=87.2 m3/s., Protection of land with vegetation is the primary factor in the fight against water erosion with necessary application of biotechnical, technical, administrative and planning measures. One of the first basins to be treated with works for the protection against erosion and torrent control is the Gradasnica River basin. The basic parameters to display the changes of the hydrological status of the land are the state of erosion, the change of erosion-coefficient, annual sediment yield, specific annual sediment discharge through the hydrographic network, the value of the runoff curve number and value of the maximal discharge. Works on protection from erosion and regulations of torrents have influenced the decrease in erosion coefficient values from strong erosion (Z=0.99) to the value of weak erosion (Z=0.40), as well as the reduction of the maximum discharge value from Qmax(1956)=108,12m3/s to the value of Qmax(2014)=87.2 m3/s.",
publisher = "Univerzitet u Beogradu - Šumarski fakultet, Beograd",
journal = "Glasnik Šumarskog fakulteta",
title = "Promene hidrološkog statusa sliva usled primene protiverozionih radova, Changes in the hydrological status of the basin due to the application of erosion control works",
pages = "200-189",
number = "114",
doi = "10.2298/GSF1614189R",
url = "conv_448"
}

Radonjić, J., Ristić, R.,& Polovina, S.. (2016). Promene hidrološkog statusa sliva usled primene protiverozionih radova. in Glasnik Šumarskog fakulteta
Univerzitet u Beogradu - Šumarski fakultet, Beograd.(114), 189-200.
https://doi.org/10.2298/GSF1614189R
conv_448

Radonjić J, Ristić R, Polovina S. Promene hidrološkog statusa sliva usled primene protiverozionih radova. in Glasnik Šumarskog fakulteta. 2016;(114):189-200.
doi:10.2298/GSF1614189R
conv_448 .

Radonjić, Jasmina, Ristić, Ratko, Polovina, Siniša, "Promene hidrološkog statusa sliva usled primene protiverozionih radova" in Glasnik Šumarskog fakulteta, no. 114 (2016):189-200,
https://doi.org/10.2298/GSF1614189R .,
conv_448 .

TY  - JOUR
AU  - Ristić, Ratko
AU  - Ljujić, Milanko
AU  - Despotović, Jovan
AU  - Aleksić, Velimir
AU  - Radić, Boris
AU  - Nikić, Zoran
AU  - Milčanović, Vukašin
AU  - Malušević, Ivan
AU  - Radonjić, Jasmina
PY  - 2013
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/520
AB  - Dams have always been a precious means of collecting, storage and managing of water resources throughout history. Today, there are about 845000 dams with a total volume of about 6000 km(3). Reservoir sedimentation is a very complex problem both worldwide and in Serbia. Natural conditions and anthropogenic activities have strong influence on sedimentation intensity and hydrological processes, which is represented at the experimental watershed of the Dicina River, in Western Serbia. Reservoir of 340000 m(3) was formed after construction of a 17 m high dam, in 1966. Sedimentation of the "Velika Dicina" reservoire was determined on the basis of a survey from October 1966 to October 2011, along longitudinal profile, 750 m upstream from the dam, with 15 cross section profiles (at a spacing of 50 m). Land use changes were analyzed on the basis of a comparison of watershed conditions in 1966 and 2012, using the CORINE methodology and the MapInfo software. Sediment yield of the area and intensity of erosion processes were estimated on the basis of the "Erosion Potential Method" (EPM). The hydrological conditions in 1966 and 2012 (after the performed Erosion and Torrent Control Works-ETCWs) were assessed on the basis of a historical overview of land use changes and their impact on computed maximal discharges. Total quantity of deposited sediment in the reservoir amounts to 18750 m(3). Intensity of sedimentation has continuously been decreasing since 2002 as the consequence of land use changes, performed ETCWs and depopulation. The values of computed maximal discharges and volumes of computed hydrographs are significantly reduced. Depopulation caused a decrease in the anthropogenic pressure on the agricultural and forest surfaces in the watershed. The realization of restoration works contributed to a decrease in the annual yield of erosive material from W-a=16007 m(3) to W-a=1930 m(3).
T2  - Carpathian Journal of Earth and Environmental Sciences
T1  - Reservoir sedimentation and hydrological effects of land use changes-case study of the experimental Dicina river watershed
EP  - 98
IS  - 1
SP  - 91
VL  - 8
UR  - conv_2172
ER  - 

@article{
author = "Ristić, Ratko and Ljujić, Milanko and Despotović, Jovan and Aleksić, Velimir and Radić, Boris and Nikić, Zoran and Milčanović, Vukašin and Malušević, Ivan and Radonjić, Jasmina",
year = "2013",
abstract = "Dams have always been a precious means of collecting, storage and managing of water resources throughout history. Today, there are about 845000 dams with a total volume of about 6000 km(3). Reservoir sedimentation is a very complex problem both worldwide and in Serbia. Natural conditions and anthropogenic activities have strong influence on sedimentation intensity and hydrological processes, which is represented at the experimental watershed of the Dicina River, in Western Serbia. Reservoir of 340000 m(3) was formed after construction of a 17 m high dam, in 1966. Sedimentation of the "Velika Dicina" reservoire was determined on the basis of a survey from October 1966 to October 2011, along longitudinal profile, 750 m upstream from the dam, with 15 cross section profiles (at a spacing of 50 m). Land use changes were analyzed on the basis of a comparison of watershed conditions in 1966 and 2012, using the CORINE methodology and the MapInfo software. Sediment yield of the area and intensity of erosion processes were estimated on the basis of the "Erosion Potential Method" (EPM). The hydrological conditions in 1966 and 2012 (after the performed Erosion and Torrent Control Works-ETCWs) were assessed on the basis of a historical overview of land use changes and their impact on computed maximal discharges. Total quantity of deposited sediment in the reservoir amounts to 18750 m(3). Intensity of sedimentation has continuously been decreasing since 2002 as the consequence of land use changes, performed ETCWs and depopulation. The values of computed maximal discharges and volumes of computed hydrographs are significantly reduced. Depopulation caused a decrease in the anthropogenic pressure on the agricultural and forest surfaces in the watershed. The realization of restoration works contributed to a decrease in the annual yield of erosive material from W-a=16007 m(3) to W-a=1930 m(3).",
journal = "Carpathian Journal of Earth and Environmental Sciences",
title = "Reservoir sedimentation and hydrological effects of land use changes-case study of the experimental Dicina river watershed",
pages = "98-91",
number = "1",
volume = "8",
url = "conv_2172"
}

Ristić, R., Ljujić, M., Despotović, J., Aleksić, V., Radić, B., Nikić, Z., Milčanović, V., Malušević, I.,& Radonjić, J.. (2013). Reservoir sedimentation and hydrological effects of land use changes-case study of the experimental Dicina river watershed. in Carpathian Journal of Earth and Environmental Sciences, 8(1), 91-98.
conv_2172

Ristić R, Ljujić M, Despotović J, Aleksić V, Radić B, Nikić Z, Milčanović V, Malušević I, Radonjić J. Reservoir sedimentation and hydrological effects of land use changes-case study of the experimental Dicina river watershed. in Carpathian Journal of Earth and Environmental Sciences. 2013;8(1):91-98.
conv_2172 .

Ristić, Ratko, Ljujić, Milanko, Despotović, Jovan, Aleksić, Velimir, Radić, Boris, Nikić, Zoran, Milčanović, Vukašin, Malušević, Ivan, Radonjić, Jasmina, "Reservoir sedimentation and hydrological effects of land use changes-case study of the experimental Dicina river watershed" in Carpathian Journal of Earth and Environmental Sciences, 8, no. 1 (2013):91-98,
conv_2172 .