TY  - JOUR
AU  - Srejić, Tanja
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Bajat, Branislav
AU  - Novković, Ivan
AU  - Milošević, Marko
AU  - Carević, Ivana
AU  - Todosijević, Mirjana
AU  - Sedlak, Marko
PY  - 2023
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1286
AB  - The erosion potential model was applied to estimate the soil erosion status of rural settlements during the years 1971 and 2011. We used univariate and bivariate local Moran’s I indices to
detect and visualize the spatial clustering of settlements with respect to changes in erosion intensity
and agricultural land use, as well as their mutual spatial correlation. The study area was differentiated
into four statistically significant clusters using the calculated bivariate local Moran’s I indices. The
statistical analysis examined the two largest clusters, i.e., the high–high and low–low clusters, and
the results of the research indicate that the first four principal components explained 70.50% and
73.47% of the total variance, respectively. In the high–high cluster, the low rates of erosion reduction
(average Index Z = 98) in the most significant types of rural settlements were determined according to
demographic indicators (i.e., the higher population vitality and population density, the smaller share
of the old population and the lower average age of the population) and the large proportion of arable
land and Neogene sediments. In the low–low cluster, high erosion reduction rates were detected
(average index Z = 64). In this cluster, the more statistically significant influence of natural conditions
in combination with demographic–agrarian processes (i.e., the larger share of the old population,
the higher average age of the population, the lower vitality index and deagrarization) were decisive
factors in changing erosion intensity
PB  - Basel : MDPI
T2  - Agriculture
T1  - Agricultural Land Use Changes as a Driving Force of Soil Erosion in the Velika Morava River Basin, Serbia
VL  - 13
IS  - 4
SP  - 778
DO  - 10.3390/agriculture13040778
ER  - 

@article{
author = "Srejić, Tanja and Manojlović, Sanja and Sibinović, Mikica and Bajat, Branislav and Novković, Ivan and Milošević, Marko and Carević, Ivana and Todosijević, Mirjana and Sedlak, Marko",
year = "2023",
abstract = "The erosion potential model was applied to estimate the soil erosion status of rural settlements during the years 1971 and 2011. We used univariate and bivariate local Moran’s I indices to
detect and visualize the spatial clustering of settlements with respect to changes in erosion intensity
and agricultural land use, as well as their mutual spatial correlation. The study area was differentiated
into four statistically significant clusters using the calculated bivariate local Moran’s I indices. The
statistical analysis examined the two largest clusters, i.e., the high–high and low–low clusters, and
the results of the research indicate that the first four principal components explained 70.50% and
73.47% of the total variance, respectively. In the high–high cluster, the low rates of erosion reduction
(average Index Z = 98) in the most significant types of rural settlements were determined according to
demographic indicators (i.e., the higher population vitality and population density, the smaller share
of the old population and the lower average age of the population) and the large proportion of arable
land and Neogene sediments. In the low–low cluster, high erosion reduction rates were detected
(average index Z = 64). In this cluster, the more statistically significant influence of natural conditions
in combination with demographic–agrarian processes (i.e., the larger share of the old population,
the higher average age of the population, the lower vitality index and deagrarization) were decisive
factors in changing erosion intensity",
publisher = "Basel : MDPI",
journal = "Agriculture",
title = "Agricultural Land Use Changes as a Driving Force of Soil Erosion in the Velika Morava River Basin, Serbia",
volume = "13",
number = "4",
pages = "778",
doi = "10.3390/agriculture13040778"
}

Srejić, T., Manojlović, S., Sibinović, M., Bajat, B., Novković, I., Milošević, M., Carević, I., Todosijević, M.,& Sedlak, M.. (2023). Agricultural Land Use Changes as a Driving Force of Soil Erosion in the Velika Morava River Basin, Serbia. in Agriculture
Basel : MDPI., 13(4), 778.
https://doi.org/10.3390/agriculture13040778

Srejić T, Manojlović S, Sibinović M, Bajat B, Novković I, Milošević M, Carević I, Todosijević M, Sedlak M. Agricultural Land Use Changes as a Driving Force of Soil Erosion in the Velika Morava River Basin, Serbia. in Agriculture. 2023;13(4):778.
doi:10.3390/agriculture13040778 .

Srejić, Tanja, Manojlović, Sanja, Sibinović, Mikica, Bajat, Branislav, Novković, Ivan, Milošević, Marko, Carević, Ivana, Todosijević, Mirjana, Sedlak, Marko, "Agricultural Land Use Changes as a Driving Force of Soil Erosion in the Velika Morava River Basin, Serbia" in Agriculture, 13, no. 4 (2023):778,
https://doi.org/10.3390/agriculture13040778 . .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Srejić, Tanja
AU  - Novković, Ivan
AU  - Milošević, Marko
AU  - Gatarić, Dragica
AU  - Carević, Ivana
AU  - Batoćanin, Natalija
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1153
AB  - The intensity of soil erosion is the result of a combined action of natural factors and different
human activities. This work aims to determine the factors controlling the change of soil
erosion. Eleven watersheds from different parts of Serbia were used as the study area. An
Erosion Potential Model was applied to estimate the soil erosion status of the watersheds
in two periods, 1971 and 2010. The model indicated that the reduction of soil erosion
intensity in the watersheds ranges from 12.4% to 82.7%. The statistical analysis examines
quantitative relationships and combined effects between soil erosion and socio-economic
and main physical-geographical determinants in watersheds. Watershed characteristics
were divided into 5 classes, and within each class 22 variables were calculated: two
variables relate to erosion, one to topography, two to land cover, seven to demographic
and ten to agrarian variables. Correlation analysis and Principal Component Analysis (PCA)
have been applied to understand the main variables that contribute to change soil erosion
intensity. The PCA identified four components that can explain at least up to 79.06% of the
variation of all variables. This study explores new indicators for correlations with changing
soil erosion and provides decision makers with access to quantification for environmental
impact assessment and decision-making for adequate soil conservation and management
programs.
PB  - Frontiers Media SA
T2  - Frontiers in Environmental Science
T1  - Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia
VL  - 10
SP  - 888901
DO  - 10.3389/fenvs.2022.888901
ER  - 

@article{
author = "Manojlović, Sanja and Sibinović, Mikica and Srejić, Tanja and Novković, Ivan and Milošević, Marko and Gatarić, Dragica and Carević, Ivana and Batoćanin, Natalija",
year = "2022",
abstract = "The intensity of soil erosion is the result of a combined action of natural factors and different
human activities. This work aims to determine the factors controlling the change of soil
erosion. Eleven watersheds from different parts of Serbia were used as the study area. An
Erosion Potential Model was applied to estimate the soil erosion status of the watersheds
in two periods, 1971 and 2010. The model indicated that the reduction of soil erosion
intensity in the watersheds ranges from 12.4% to 82.7%. The statistical analysis examines
quantitative relationships and combined effects between soil erosion and socio-economic
and main physical-geographical determinants in watersheds. Watershed characteristics
were divided into 5 classes, and within each class 22 variables were calculated: two
variables relate to erosion, one to topography, two to land cover, seven to demographic
and ten to agrarian variables. Correlation analysis and Principal Component Analysis (PCA)
have been applied to understand the main variables that contribute to change soil erosion
intensity. The PCA identified four components that can explain at least up to 79.06% of the
variation of all variables. This study explores new indicators for correlations with changing
soil erosion and provides decision makers with access to quantification for environmental
impact assessment and decision-making for adequate soil conservation and management
programs.",
publisher = "Frontiers Media SA",
journal = "Frontiers in Environmental Science",
title = "Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia",
volume = "10",
pages = "888901",
doi = "10.3389/fenvs.2022.888901"
}

Manojlović, S., Sibinović, M., Srejić, T., Novković, I., Milošević, M., Gatarić, D., Carević, I.,& Batoćanin, N.. (2022). Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia. in Frontiers in Environmental Science
Frontiers Media SA., 10, 888901.
https://doi.org/10.3389/fenvs.2022.888901

Manojlović S, Sibinović M, Srejić T, Novković I, Milošević M, Gatarić D, Carević I, Batoćanin N. Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia. in Frontiers in Environmental Science. 2022;10:888901.
doi:10.3389/fenvs.2022.888901 .

Manojlović, Sanja, Sibinović, Mikica, Srejić, Tanja, Novković, Ivan, Milošević, Marko, Gatarić, Dragica, Carević, Ivana, Batoćanin, Natalija, "Factors Controlling the Change of Soil Erosion Intensity in Mountain Watersheds in Serbia" in Frontiers in Environmental Science, 10 (2022):888901,
https://doi.org/10.3389/fenvs.2022.888901 . .

TY  - CONF
AU  - Manojlović, Sanja
AU  - Petrović, Ana M.
AU  - Srejić, Tanja
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1283
AB  - Dynamics of totall dissolved solids (TDS) and suspended sediment concentrations (SSC)
were monitored on the river Nišava at the hydrological station Dimitrovgrad. Water
samples were collected each day in the period from 01.01.2010–31.12.2010. TDS
concentration followed a seasonal pattern imposed by the availability of water, with
higher concentrations recorded in low-flow periods and lower concentration in the highflow period. SSC was extremely variable and dominate mainly with specific high-flow
events. Mean annual discharge (Q=6.68 m3/s, q=13.9 l/s/km2) over the year was 3.3 times
higher than the average for the period of 50 years. In the study period, the annual transport
dissolved load (Qd) was 36962.8 t (specific load Qds=76.7 t/km2/yr) and suspended
sediment load (Qs) was 98861.9 t (specific load Qss=205.1 t/km2/yr). The transport of
dissolved load and suspended sediment load shows temporal variations in different
seasons. The analysis revealed that the maximum loads was transferred during the winter
(Qd=43.3% and Qs=56.8% of the annual transport) and spring season (Qd=37.9% and
Qs=38.9% of the annual transport). A comparative analysis of Q, Qd, and Qs show that
the suspended sediment shows greater variability and exponential pattern of transport.
For instance, 90% of the time was required to export 65% of the total water and
transported 77% of the total dissolved load and only 22% total suspended sediment load.
The most extreme precipitation episodes and extreme temperatures events was recorded
in February 2010. The floods in February contributed by 44.8% of the total Qs transport
over the study period. These findings have important implications for water resource
management in the context of sediments mobilization, erosion, channel management,
water quality and ecological functions.
PB  - Skopje : Geobalcancia Society
C3  - Proceedings of the 8th International scientific conference "Geobalcanica", Belgrade
T1  - Intra-Annual Dynamics Dissolved Solids and Suspended Sediment in the Extreme Hidrological Events – Case Study Nišava River
SP  - 19
EP  - 33
DO  - 10.18509/GBP22019m
ER  - 

@conference{
author = "Manojlović, Sanja and Petrović, Ana M. and Srejić, Tanja",
year = "2022",
abstract = "Dynamics of totall dissolved solids (TDS) and suspended sediment concentrations (SSC)
were monitored on the river Nišava at the hydrological station Dimitrovgrad. Water
samples were collected each day in the period from 01.01.2010–31.12.2010. TDS
concentration followed a seasonal pattern imposed by the availability of water, with
higher concentrations recorded in low-flow periods and lower concentration in the highflow period. SSC was extremely variable and dominate mainly with specific high-flow
events. Mean annual discharge (Q=6.68 m3/s, q=13.9 l/s/km2) over the year was 3.3 times
higher than the average for the period of 50 years. In the study period, the annual transport
dissolved load (Qd) was 36962.8 t (specific load Qds=76.7 t/km2/yr) and suspended
sediment load (Qs) was 98861.9 t (specific load Qss=205.1 t/km2/yr). The transport of
dissolved load and suspended sediment load shows temporal variations in different
seasons. The analysis revealed that the maximum loads was transferred during the winter
(Qd=43.3% and Qs=56.8% of the annual transport) and spring season (Qd=37.9% and
Qs=38.9% of the annual transport). A comparative analysis of Q, Qd, and Qs show that
the suspended sediment shows greater variability and exponential pattern of transport.
For instance, 90% of the time was required to export 65% of the total water and
transported 77% of the total dissolved load and only 22% total suspended sediment load.
The most extreme precipitation episodes and extreme temperatures events was recorded
in February 2010. The floods in February contributed by 44.8% of the total Qs transport
over the study period. These findings have important implications for water resource
management in the context of sediments mobilization, erosion, channel management,
water quality and ecological functions.",
publisher = "Skopje : Geobalcancia Society",
journal = "Proceedings of the 8th International scientific conference "Geobalcanica", Belgrade",
title = "Intra-Annual Dynamics Dissolved Solids and Suspended Sediment in the Extreme Hidrological Events – Case Study Nišava River",
pages = "19-33",
doi = "10.18509/GBP22019m"
}

Manojlović, S., Petrović, A. M.,& Srejić, T.. (2022). Intra-Annual Dynamics Dissolved Solids and Suspended Sediment in the Extreme Hidrological Events – Case Study Nišava River. in Proceedings of the 8th International scientific conference "Geobalcanica", Belgrade
Skopje : Geobalcancia Society., 19-33.
https://doi.org/10.18509/GBP22019m

Manojlović S, Petrović AM, Srejić T. Intra-Annual Dynamics Dissolved Solids and Suspended Sediment in the Extreme Hidrological Events – Case Study Nišava River. in Proceedings of the 8th International scientific conference "Geobalcanica", Belgrade. 2022;:19-33.
doi:10.18509/GBP22019m .

Manojlović, Sanja, Petrović, Ana M., Srejić, Tanja, "Intra-Annual Dynamics Dissolved Solids and Suspended Sediment in the Extreme Hidrological Events – Case Study Nišava River" in Proceedings of the 8th International scientific conference "Geobalcanica", Belgrade (2022):19-33,
https://doi.org/10.18509/GBP22019m . .

TY  - CONF
AU  - Manojlović, Sanja
AU  - Srejić, Tanja
AU  - Sibinović, Mikica
AU  - Carević, Ivana
AU  - Batoćanin, Natalija
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1287
AB  - Intenzitet erozije zemljišta rezultat je kombinovanog delovanja različitih prirodnih i antropogenih faktora. Ovaj rad ima za cilj da utvrdi agrarne indikatore kao determinante promene intenziteta erozije zemljišta u slivovima Crnice i Rasničke reke. Model potencijala erozije primenjen je za procenu stanja erozije zemljišta za dva perioda 1971. godine i 2010. godine. Koeficijent erozije u slivu Crnice iznosio je Z1=0,390 i Z2=0,360, a specifična produkcija nanosa Ws1=529 m3/km2/god i Ws2=463 m3/km2/god. Koeficijent erozije u slivu Rasničke reke iznosio je Z1=0,437 i Z2=0,374, a specifična produkcija nanosa Ws1=861 m3/km2/god i Ws2=622 m3/km2/god. Ekstremno smanjenje agrarnog pritiska na zemljište, veliki udeo naselja regresivnog tipa od 80 %, kao i intenzivan proces depopulacije rezultiralo je većoj redukciji erozije zemljišta u slivu Rasničke reke. Rezulati ove studije mogu omogućiti donosiocima odluka nove pristupe za adekvatno upravljanje zemljišnim resursima u ruralnim sredinama.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Devetog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Veliko Gradište
T1  - Ruralna deagrarizacija kao faktor promene intenziteta erozije zemljišta
SP  - 263
EP  - 270
UR  - https://hdl.handle.net/21.15107/rcub_gery_1287
ER  - 

@conference{
author = "Manojlović, Sanja and Srejić, Tanja and Sibinović, Mikica and Carević, Ivana and Batoćanin, Natalija",
year = "2022",
abstract = "Intenzitet erozije zemljišta rezultat je kombinovanog delovanja različitih prirodnih i antropogenih faktora. Ovaj rad ima za cilj da utvrdi agrarne indikatore kao determinante promene intenziteta erozije zemljišta u slivovima Crnice i Rasničke reke. Model potencijala erozije primenjen je za procenu stanja erozije zemljišta za dva perioda 1971. godine i 2010. godine. Koeficijent erozije u slivu Crnice iznosio je Z1=0,390 i Z2=0,360, a specifična produkcija nanosa Ws1=529 m3/km2/god i Ws2=463 m3/km2/god. Koeficijent erozije u slivu Rasničke reke iznosio je Z1=0,437 i Z2=0,374, a specifična produkcija nanosa Ws1=861 m3/km2/god i Ws2=622 m3/km2/god. Ekstremno smanjenje agrarnog pritiska na zemljište, veliki udeo naselja regresivnog tipa od 80 %, kao i intenzivan proces depopulacije rezultiralo je većoj redukciji erozije zemljišta u slivu Rasničke reke. Rezulati ove studije mogu omogućiti donosiocima odluka nove pristupe za adekvatno upravljanje zemljišnim resursima u ruralnim sredinama.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Devetog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Veliko Gradište",
title = "Ruralna deagrarizacija kao faktor promene intenziteta erozije zemljišta",
pages = "263-270",
url = "https://hdl.handle.net/21.15107/rcub_gery_1287"
}

Manojlović, S., Srejić, T., Sibinović, M., Carević, I.,& Batoćanin, N.. (2022). Ruralna deagrarizacija kao faktor promene intenziteta erozije zemljišta. in Zbornik radova Devetog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Veliko Gradište
Beograd : Asocijacija prostornih planera Srbije., 263-270.
https://hdl.handle.net/21.15107/rcub_gery_1287

Manojlović S, Srejić T, Sibinović M, Carević I, Batoćanin N. Ruralna deagrarizacija kao faktor promene intenziteta erozije zemljišta. in Zbornik radova Devetog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Veliko Gradište. 2022;:263-270.
https://hdl.handle.net/21.15107/rcub_gery_1287 .

Manojlović, Sanja, Srejić, Tanja, Sibinović, Mikica, Carević, Ivana, Batoćanin, Natalija, "Ruralna deagrarizacija kao faktor promene intenziteta erozije zemljišta" in Zbornik radova Devetog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Veliko Gradište (2022):263-270,
https://hdl.handle.net/21.15107/rcub_gery_1287 .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Srejić, Tanja
AU  - Sibinović, Mikica
AU  - Milošević, Marko
AU  - Bajat, Branislav
AU  - Kostadinov, Stanimir
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1285
AB  - Sediment transport time series have shown a severe change in the suspended sediment load transported by the Velika Morava 
River (Republic of Serbia) during the last few decades. The research objectives of this study were to determine the suspended 
sediment trends, and to assess the impact of variations in precipitation and human activities on the suspended sediment load. 
The causes and timing of this severe decrease were analyzed, and the results show that there has been a signifcant sudden 
shift downwards for the suspended sediment load (p<0.0001) during the research period. The change points for sediment load 
were very similar and the transition years all ranged between 1982 and 1984. The combined efects of precipitation and human 
activities are responsible for the decrease in the suspended sediment load, with human activity being the most active factor in 
the sediment regime changes. The contribution rate for human activities amounts to 87.7–91.9%, while precipitation explains 
8.1–12.3% of the reduction in the suspended sediment load. The processes of deagrarization and depopulation had an infuence 
on the sediment load decrease in the study area. The results of the spatial autocorrelation analysis of rural settlements showed 
that the reduction in sediment was due to the process of depopulation and the large reduction in the amount of arable land in 
rural areas and settlements. The changes in sediment regimes were also infuenced by soil and water conservation programmes.
PB  - Springer Nature
T2  - Arabian Journal of Geosciences
T1  - Impact of precipitation and human activities on suspended sediment  transport load in the Velika Morava River Basin (Serbia)
VL  - 15
IS  - 13
SP  - 1209
DO  - 10.1007/s12517-022-10475-x
ER  - 

@article{
author = "Manojlović, Sanja and Srejić, Tanja and Sibinović, Mikica and Milošević, Marko and Bajat, Branislav and Kostadinov, Stanimir",
year = "2022",
abstract = "Sediment transport time series have shown a severe change in the suspended sediment load transported by the Velika Morava 
River (Republic of Serbia) during the last few decades. The research objectives of this study were to determine the suspended 
sediment trends, and to assess the impact of variations in precipitation and human activities on the suspended sediment load. 
The causes and timing of this severe decrease were analyzed, and the results show that there has been a signifcant sudden 
shift downwards for the suspended sediment load (p<0.0001) during the research period. The change points for sediment load 
were very similar and the transition years all ranged between 1982 and 1984. The combined efects of precipitation and human 
activities are responsible for the decrease in the suspended sediment load, with human activity being the most active factor in 
the sediment regime changes. The contribution rate for human activities amounts to 87.7–91.9%, while precipitation explains 
8.1–12.3% of the reduction in the suspended sediment load. The processes of deagrarization and depopulation had an infuence 
on the sediment load decrease in the study area. The results of the spatial autocorrelation analysis of rural settlements showed 
that the reduction in sediment was due to the process of depopulation and the large reduction in the amount of arable land in 
rural areas and settlements. The changes in sediment regimes were also infuenced by soil and water conservation programmes.",
publisher = "Springer Nature",
journal = "Arabian Journal of Geosciences",
title = "Impact of precipitation and human activities on suspended sediment  transport load in the Velika Morava River Basin (Serbia)",
volume = "15",
number = "13",
pages = "1209",
doi = "10.1007/s12517-022-10475-x"
}

Manojlović, S., Srejić, T., Sibinović, M., Milošević, M., Bajat, B.,& Kostadinov, S.. (2022). Impact of precipitation and human activities on suspended sediment  transport load in the Velika Morava River Basin (Serbia). in Arabian Journal of Geosciences
Springer Nature., 15(13), 1209.
https://doi.org/10.1007/s12517-022-10475-x

Manojlović S, Srejić T, Sibinović M, Milošević M, Bajat B, Kostadinov S. Impact of precipitation and human activities on suspended sediment  transport load in the Velika Morava River Basin (Serbia). in Arabian Journal of Geosciences. 2022;15(13):1209.
doi:10.1007/s12517-022-10475-x .

Manojlović, Sanja, Srejić, Tanja, Sibinović, Mikica, Milošević, Marko, Bajat, Branislav, Kostadinov, Stanimir, "Impact of precipitation and human activities on suspended sediment  transport load in the Velika Morava River Basin (Serbia)" in Arabian Journal of Geosciences, 15, no. 13 (2022):1209,
https://doi.org/10.1007/s12517-022-10475-x . .

TY  - JOUR
AU  - Gatarić, Dragica
AU  - Đerčan, Bojan
AU  - Bubalo-Zivkovic, Milka
AU  - Ostojić, Miloš
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Lukić, Tamara
AU  - Jeftić, Marija R.
AU  - Lutovac, Miloš
AU  - Lutovac, Milena
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1201
AB  - The key problem of rural settlements in the South Banat district lasted into the 21st century
through the spread of depopulated areas. Considering that settlements give a cultural
landscape its basic features, that they are the main bearers of functional organization, and
the hotspots of geo-spatial transformation, based on quantitative-qualitative indicators this
paper analyzes the spatial-demographic determinants of the development of 94
settlements, and the impact of depopulation on the changes in the surrounding forest
cover. The time span included in the analytical-statistical research of the demographic
components and forest dislocation lasted from 1990 to 2018. Geo-spatial data for forest
areas were taken from the Corine Land Cover database. The data obtained were then
turned into visual representations, or maps, using the GIS ArcMap 10.8. software. The
results indicated that total depopulation has been an ongoing, 30-years process in this
area on the one hand, while the forest cover in the depopulated settlements located on the
outskirts of the Deliblato sands (a special nature reserve) has decreased, and the forest
cover in the depopulated settlements in the zone of the Vršac mountains has increased, on
the other. These analyses are useful for obtaining more detailed insight into the state of
forested areas in this part of Serbia, which is the least afforested one.
PB  - Frontiers Media SA
T2  - Frontiers in Environmental Science
T1  - Can Depopulation Stop Deforestation? The Impact of Demographic Movement on Forest Cover Changes in the Settlements of the South Banat District (Serbia)
VL  - 10
SP  - 897201
DO  - 10.3389/fenvs.2022.897201
ER  - 

@article{
author = "Gatarić, Dragica and Đerčan, Bojan and Bubalo-Zivkovic, Milka and Ostojić, Miloš and Manojlović, Sanja and Sibinović, Mikica and Lukić, Tamara and Jeftić, Marija R. and Lutovac, Miloš and Lutovac, Milena",
year = "2022",
abstract = "The key problem of rural settlements in the South Banat district lasted into the 21st century
through the spread of depopulated areas. Considering that settlements give a cultural
landscape its basic features, that they are the main bearers of functional organization, and
the hotspots of geo-spatial transformation, based on quantitative-qualitative indicators this
paper analyzes the spatial-demographic determinants of the development of 94
settlements, and the impact of depopulation on the changes in the surrounding forest
cover. The time span included in the analytical-statistical research of the demographic
components and forest dislocation lasted from 1990 to 2018. Geo-spatial data for forest
areas were taken from the Corine Land Cover database. The data obtained were then
turned into visual representations, or maps, using the GIS ArcMap 10.8. software. The
results indicated that total depopulation has been an ongoing, 30-years process in this
area on the one hand, while the forest cover in the depopulated settlements located on the
outskirts of the Deliblato sands (a special nature reserve) has decreased, and the forest
cover in the depopulated settlements in the zone of the Vršac mountains has increased, on
the other. These analyses are useful for obtaining more detailed insight into the state of
forested areas in this part of Serbia, which is the least afforested one.",
publisher = "Frontiers Media SA",
journal = "Frontiers in Environmental Science",
title = "Can Depopulation Stop Deforestation? The Impact of Demographic Movement on Forest Cover Changes in the Settlements of the South Banat District (Serbia)",
volume = "10",
pages = "897201",
doi = "10.3389/fenvs.2022.897201"
}

Gatarić, D., Đerčan, B., Bubalo-Zivkovic, M., Ostojić, M., Manojlović, S., Sibinović, M., Lukić, T., Jeftić, M. R., Lutovac, M.,& Lutovac, M.. (2022). Can Depopulation Stop Deforestation? The Impact of Demographic Movement on Forest Cover Changes in the Settlements of the South Banat District (Serbia). in Frontiers in Environmental Science
Frontiers Media SA., 10, 897201.
https://doi.org/10.3389/fenvs.2022.897201

Gatarić D, Đerčan B, Bubalo-Zivkovic M, Ostojić M, Manojlović S, Sibinović M, Lukić T, Jeftić MR, Lutovac M, Lutovac M. Can Depopulation Stop Deforestation? The Impact of Demographic Movement on Forest Cover Changes in the Settlements of the South Banat District (Serbia). in Frontiers in Environmental Science. 2022;10:897201.
doi:10.3389/fenvs.2022.897201 .

Gatarić, Dragica, Đerčan, Bojan, Bubalo-Zivkovic, Milka, Ostojić, Miloš, Manojlović, Sanja, Sibinović, Mikica, Lukić, Tamara, Jeftić, Marija R., Lutovac, Miloš, Lutovac, Milena, "Can Depopulation Stop Deforestation? The Impact of Demographic Movement on Forest Cover Changes in the Settlements of the South Banat District (Serbia)" in Frontiers in Environmental Science, 10 (2022):897201,
https://doi.org/10.3389/fenvs.2022.897201 . .

TY  - CONF
AU  - Manojlović, Sanja
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1725
AB  - Proučavanje kraških terena u Srbiji ima tradiciju dugu više od jednog veka.  Kvantitativna istraživanja utvrdjivanje intenziteta korozije i hemjiske erozije datira od  sredine osamdesetih godina XX veka, kada su počela prva eksperimentalna istraživanja  primenom metoda standardnih tableta (pločica). S obzirom da je količina hemijski  rastvorenogh nanosa koju u jedinici vremena rečni tok iznese iz sliva, direktna funkcija  količine oticajne vode i njene mineralizacije, uspostavljena su terenska istraživanja bazirana  na monitroingu uzimanja uzoraka i utvrdjiva hemizma površinskih voda i kraških izvora  primenom hidrohemijskih metoda. Za utvrdjivanje prostorne komponente intenziteta  hemijske erozije, na osnovu višegodišnjih laboratorijiskih i terenskih istraživanja,  forimani su numerički modeli. Empirijski metod zasnovan je na odnosu specifičnog  oticaja i odgovarajuće mineralizacije vode, a za izdvojene litološko-petrološke kompleke.  Rezultat primene empirijskog metoda je izrada Karte hemijske erozije Srbije. Prema ovoj  karti prosečan intenziet hemijske erozije kraških terena u Srbiji iznosi 105 t/km2 /god.
PB  - Београд : Универзитет у Београду - Географски факултет
C3  - Zbornik radova sa naučnog skupa "Kras - vekovna naučna inspiracija - posvećen dr Dušanu Gavriloviću, profesoru Geografskog fakulteta, 1934 - 2020", Beograd
T1  - Intenzitet hemijske erozije kraških terena u Srbiji
SP  - 113
EP  - 127
UR  - https://hdl.handle.net/21.15107/rcub_gery_1725
ER  - 

@conference{
author = "Manojlović, Sanja",
year = "2022",
abstract = "Proučavanje kraških terena u Srbiji ima tradiciju dugu više od jednog veka.  Kvantitativna istraživanja utvrdjivanje intenziteta korozije i hemjiske erozije datira od  sredine osamdesetih godina XX veka, kada su počela prva eksperimentalna istraživanja  primenom metoda standardnih tableta (pločica). S obzirom da je količina hemijski  rastvorenogh nanosa koju u jedinici vremena rečni tok iznese iz sliva, direktna funkcija  količine oticajne vode i njene mineralizacije, uspostavljena su terenska istraživanja bazirana  na monitroingu uzimanja uzoraka i utvrdjiva hemizma površinskih voda i kraških izvora  primenom hidrohemijskih metoda. Za utvrdjivanje prostorne komponente intenziteta  hemijske erozije, na osnovu višegodišnjih laboratorijiskih i terenskih istraživanja,  forimani su numerički modeli. Empirijski metod zasnovan je na odnosu specifičnog  oticaja i odgovarajuće mineralizacije vode, a za izdvojene litološko-petrološke kompleke.  Rezultat primene empirijskog metoda je izrada Karte hemijske erozije Srbije. Prema ovoj  karti prosečan intenziet hemijske erozije kraških terena u Srbiji iznosi 105 t/km2 /god.",
publisher = "Београд : Универзитет у Београду - Географски факултет",
journal = "Zbornik radova sa naučnog skupa "Kras - vekovna naučna inspiracija - posvećen dr Dušanu Gavriloviću, profesoru Geografskog fakulteta, 1934 - 2020", Beograd",
title = "Intenzitet hemijske erozije kraških terena u Srbiji",
pages = "113-127",
url = "https://hdl.handle.net/21.15107/rcub_gery_1725"
}

Manojlović, S.. (2022). Intenzitet hemijske erozije kraških terena u Srbiji. in Zbornik radova sa naučnog skupa "Kras - vekovna naučna inspiracija - posvećen dr Dušanu Gavriloviću, profesoru Geografskog fakulteta, 1934 - 2020", Beograd
Београд : Универзитет у Београду - Географски факултет., 113-127.
https://hdl.handle.net/21.15107/rcub_gery_1725

Manojlović S. Intenzitet hemijske erozije kraških terena u Srbiji. in Zbornik radova sa naučnog skupa "Kras - vekovna naučna inspiracija - posvećen dr Dušanu Gavriloviću, profesoru Geografskog fakulteta, 1934 - 2020", Beograd. 2022;:113-127.
https://hdl.handle.net/21.15107/rcub_gery_1725 .

Manojlović, Sanja, "Intenzitet hemijske erozije kraških terena u Srbiji" in Zbornik radova sa naučnog skupa "Kras - vekovna naučna inspiracija - posvećen dr Dušanu Gavriloviću, profesoru Geografskog fakulteta, 1934 - 2020", Beograd (2022):113-127,
https://hdl.handle.net/21.15107/rcub_gery_1725 .

TY  - CONF
AU  - Batoćanin, Natalija
AU  - Carević, Ivana
AU  - Manojlović, Sanja
PY  - 2022
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1707
AB  - Kontinentalni karbonati, koji se talože iz slatkih voda bogatih kalcijum bikarbonatom obuhvataju sledeće sedimentne stene: bigar, travertin i pećinski nakit. Fokus ovog rada je na razlikama između prva dva, kako je u domaćoj literaturi razlika uglavnom bazirana na teksturnim karakteristikama i temperaturi vode iz koje se kalcijum karbonat taloži. Bigar je jako porozna, šupljikava stena, dok je travertin kompaktniji i veoma često laminiran. Takođe, opšte je poznato da se bigar taloži iz hladne, uglavnom rečne vode, a travertin iz tople. Temperatura vode ima direktan uticaj na diverzitet flore i faune, pa će ona uz bigar biti bujna, dok je kod toplih voda organski svet ograničen na određene vrste bakterija. Cirkulacija toplih voda iz kojih se taloži travertin omogućena je preko pukotina ili raseda, pa su pojave travertina kontrolisane lokalnom tektonikom, dok su pojave bigra vezane za klimatske uslove. Osim ovih, parametri koji definišu sedimentnu stenu kao bigar ili travertin su brzina taloženja i odnosi stabilnih izotopa kiseonika i ugljenika. Bigar karakteriše srednja brzina taloženja (nekoliko milimetara godišnje), dok travertin karakteriše velika brzina taloženja (preko nekoliko decimetara godišnje). Stabilni izotopi ugljenika definišu kontinentalne karbonate na taj način što će δ13C vrednosti biti nnegativne za bigar, a pozitivne za travertin. Razlog tome leži u činjenici da je bigar obogaćem lakšim izotopom ugljenika, a travertin težim. Kako odnosi stabilnih izotopa kiseonika direktno zavise od temperature vode, njihov značaj je nedvosmislen. Teksturne karakteristike jesu posledica svih ovih parametara, ali nije redak slučaj da porozna stena prema istim odgovara travertinu, a kompaktna laminirana stena bigru. Takvih primera ima i na području Srbije (bigar reke Sopotnice, kompaktna laminirana stena, ali izotopski odnosi odgovaraju bigru). Kada su u pitanju recentni sedimenti ovaj disbalans ne predstavlja problem, ali kod fosilnih akumulacija trebalo bi izbeći nazive “bigar” i “travertin”, pogotovu ako su isti dati samo na osnovu teksturnih karakteristika.
AB  - Terrestrial carbonates, which are excreted from fresh calcium bicarbonate-rich waters, include the following sedimentary rocks: calcareous tufa, travertine, and speleothems. Focus of this paper is the differences between calcareous tufa and travertine. In domestic literature, difference between tufa and travertine is usually based on structure and water temperature. Tufa is very porous rock, while travertine is more compact and laminated. Furthermore, it is known that tufa precipitates from cold streams, whereas travertine precipitates from warm waters. Temperature of water has strong influence on diversity of living organisms. Tufa deposits are followed with luxuriant vegetation and diversity of fauna, whereas in hot waters the assemblage of living beings is limited to some bacterial species. Circulation of hot, “travertine bearing” fluids is enabled throughout fissures and faults, thus, travertine deposits are controlled by local tectonics and tufa deposits are driven by climatic conditions. Next to these parameters which define sedimentary rock as tufa or travertine are the deposition rate and ratio of stable oxygen and carbon isotopes. Tufa is characterized by medium deposition rate (up to few millimeters per year), while travertine is characterized by high deposition rate (up to few decimeters per year). Values of δ13C will be negative for tufa and positive for travertine. The reason is that tufa is enriched in light 12C isotope and travertine is enriched in heavy, 13C isotope. Due to fact that the ratio of stable oxygen isotope is directly influenced by water temperature, their importance is unambiguous. Structure is a consequence of those parameters, but it is not uncommon that porous rock considers travertine and that compact laminated rock considers tufa. Those cases are well-known, also on the territory of Serbia (tufa of the Sopotnica River, compact laminated rock, despite it, isotope imprint points to travertine). In recently forming sediments, such discrepancy is not a problem, but in the case of fossil accumulations, we should avoid assigning rock as “tufa” or “travertine”, especially if names are based only on their structural characteristics.
PB  - Beograd : Srpsko geološko društvo
PB  - Beograd : Univerzitet u Beogradu – Rudarsko-geološki fakultet
C3  - Zbornik apstrakata 18. Kongresa geologa Srbije "Geologija rešava probleme", Divčibare
T1  - O kontinentalnim karbonatima: bigar vs. travertin
T1  - About terrestrial carbonates: calcareous tufa vs. travertine
SP  - 46
EP  - 47
UR  - https://hdl.handle.net/21.15107/rcub_gery_1707
ER  - 

@conference{
author = "Batoćanin, Natalija and Carević, Ivana and Manojlović, Sanja",
year = "2022",
abstract = "Kontinentalni karbonati, koji se talože iz slatkih voda bogatih kalcijum bikarbonatom obuhvataju sledeće sedimentne stene: bigar, travertin i pećinski nakit. Fokus ovog rada je na razlikama između prva dva, kako je u domaćoj literaturi razlika uglavnom bazirana na teksturnim karakteristikama i temperaturi vode iz koje se kalcijum karbonat taloži. Bigar je jako porozna, šupljikava stena, dok je travertin kompaktniji i veoma često laminiran. Takođe, opšte je poznato da se bigar taloži iz hladne, uglavnom rečne vode, a travertin iz tople. Temperatura vode ima direktan uticaj na diverzitet flore i faune, pa će ona uz bigar biti bujna, dok je kod toplih voda organski svet ograničen na određene vrste bakterija. Cirkulacija toplih voda iz kojih se taloži travertin omogućena je preko pukotina ili raseda, pa su pojave travertina kontrolisane lokalnom tektonikom, dok su pojave bigra vezane za klimatske uslove. Osim ovih, parametri koji definišu sedimentnu stenu kao bigar ili travertin su brzina taloženja i odnosi stabilnih izotopa kiseonika i ugljenika. Bigar karakteriše srednja brzina taloženja (nekoliko milimetara godišnje), dok travertin karakteriše velika brzina taloženja (preko nekoliko decimetara godišnje). Stabilni izotopi ugljenika definišu kontinentalne karbonate na taj način što će δ13C vrednosti biti nnegativne za bigar, a pozitivne za travertin. Razlog tome leži u činjenici da je bigar obogaćem lakšim izotopom ugljenika, a travertin težim. Kako odnosi stabilnih izotopa kiseonika direktno zavise od temperature vode, njihov značaj je nedvosmislen. Teksturne karakteristike jesu posledica svih ovih parametara, ali nije redak slučaj da porozna stena prema istim odgovara travertinu, a kompaktna laminirana stena bigru. Takvih primera ima i na području Srbije (bigar reke Sopotnice, kompaktna laminirana stena, ali izotopski odnosi odgovaraju bigru). Kada su u pitanju recentni sedimenti ovaj disbalans ne predstavlja problem, ali kod fosilnih akumulacija trebalo bi izbeći nazive “bigar” i “travertin”, pogotovu ako su isti dati samo na osnovu teksturnih karakteristika., Terrestrial carbonates, which are excreted from fresh calcium bicarbonate-rich waters, include the following sedimentary rocks: calcareous tufa, travertine, and speleothems. Focus of this paper is the differences between calcareous tufa and travertine. In domestic literature, difference between tufa and travertine is usually based on structure and water temperature. Tufa is very porous rock, while travertine is more compact and laminated. Furthermore, it is known that tufa precipitates from cold streams, whereas travertine precipitates from warm waters. Temperature of water has strong influence on diversity of living organisms. Tufa deposits are followed with luxuriant vegetation and diversity of fauna, whereas in hot waters the assemblage of living beings is limited to some bacterial species. Circulation of hot, “travertine bearing” fluids is enabled throughout fissures and faults, thus, travertine deposits are controlled by local tectonics and tufa deposits are driven by climatic conditions. Next to these parameters which define sedimentary rock as tufa or travertine are the deposition rate and ratio of stable oxygen and carbon isotopes. Tufa is characterized by medium deposition rate (up to few millimeters per year), while travertine is characterized by high deposition rate (up to few decimeters per year). Values of δ13C will be negative for tufa and positive for travertine. The reason is that tufa is enriched in light 12C isotope and travertine is enriched in heavy, 13C isotope. Due to fact that the ratio of stable oxygen isotope is directly influenced by water temperature, their importance is unambiguous. Structure is a consequence of those parameters, but it is not uncommon that porous rock considers travertine and that compact laminated rock considers tufa. Those cases are well-known, also on the territory of Serbia (tufa of the Sopotnica River, compact laminated rock, despite it, isotope imprint points to travertine). In recently forming sediments, such discrepancy is not a problem, but in the case of fossil accumulations, we should avoid assigning rock as “tufa” or “travertine”, especially if names are based only on their structural characteristics.",
publisher = "Beograd : Srpsko geološko društvo, Beograd : Univerzitet u Beogradu – Rudarsko-geološki fakultet",
journal = "Zbornik apstrakata 18. Kongresa geologa Srbije "Geologija rešava probleme", Divčibare",
title = "O kontinentalnim karbonatima: bigar vs. travertin, About terrestrial carbonates: calcareous tufa vs. travertine",
pages = "46-47",
url = "https://hdl.handle.net/21.15107/rcub_gery_1707"
}

Batoćanin, N., Carević, I.,& Manojlović, S.. (2022). O kontinentalnim karbonatima: bigar vs. travertin. in Zbornik apstrakata 18. Kongresa geologa Srbije "Geologija rešava probleme", Divčibare
Beograd : Srpsko geološko društvo., 46-47.
https://hdl.handle.net/21.15107/rcub_gery_1707

Batoćanin N, Carević I, Manojlović S. O kontinentalnim karbonatima: bigar vs. travertin. in Zbornik apstrakata 18. Kongresa geologa Srbije "Geologija rešava probleme", Divčibare. 2022;:46-47.
https://hdl.handle.net/21.15107/rcub_gery_1707 .

Batoćanin, Natalija, Carević, Ivana, Manojlović, Sanja, "O kontinentalnim karbonatima: bigar vs. travertin" in Zbornik apstrakata 18. Kongresa geologa Srbije "Geologija rešava probleme", Divčibare (2022):46-47,
https://hdl.handle.net/21.15107/rcub_gery_1707 .

TY  - CONF
AU  - Manojlović, Sanja
AU  - Srejić, Tanja
AU  - Sibinović, Mikica
AU  - Carević, Ivana
AU  - Batoćanin, Natalija
PY  - 2021
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1291
AB  - Prostorno-vremenska dinamika suspendovnog nanosa u rekama širom sveta u fokusu je istraživanja naučnika od sredine 20. veka. Posebna pažnja vidno izražena u protekla dve decenije 21. veka usmerena je na procenu uticaja klimatskih promena i antropogenog faktora na režim nanosa. Razumevanje režima suspendovanog nanosa je ključni preduslov adekvatnog upravljanja vodnim resursima. Pored istraživanja na globalnom novou, pojedine zemlje razvile su adekvatne nacionalne programe upravljanja rečnim geosistemima u kojima su inkorporirale monitoring suspendovanog nanosa kao jedan od primarnih faktora praćenja promena u životnoj sredini. Značaj proučavanja sedimenata u rekama je višestruk. Promene u režimu nanosa imaju direktne reprekusije na stanje i kvalitet vodnih ekosistema, posledice pojave poplavnih talasa, sa posebnim uticajem na povećanje troškova prečišćavanja voda, postojeća energetska postrojenja i vodne akumulacije. U ovom radu dat je novi pristup vremenskoj determinaciji transporta suspendovanog nanosa, kao i uticaj antropogenog faktora sa aspekta promene načina korišćenja zemljišta na režim nanosa za dugoročne vremenske serije.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac
T1  - Prilog proučavanju dinamike transporta suspendovanog nanosa kao posledica promena u životnoj sredini
SP  - 387
EP  - 393
UR  - https://hdl.handle.net/21.15107/rcub_gery_1291
ER  - 

@conference{
author = "Manojlović, Sanja and Srejić, Tanja and Sibinović, Mikica and Carević, Ivana and Batoćanin, Natalija",
year = "2021",
abstract = "Prostorno-vremenska dinamika suspendovnog nanosa u rekama širom sveta u fokusu je istraživanja naučnika od sredine 20. veka. Posebna pažnja vidno izražena u protekla dve decenije 21. veka usmerena je na procenu uticaja klimatskih promena i antropogenog faktora na režim nanosa. Razumevanje režima suspendovanog nanosa je ključni preduslov adekvatnog upravljanja vodnim resursima. Pored istraživanja na globalnom novou, pojedine zemlje razvile su adekvatne nacionalne programe upravljanja rečnim geosistemima u kojima su inkorporirale monitoring suspendovanog nanosa kao jedan od primarnih faktora praćenja promena u životnoj sredini. Značaj proučavanja sedimenata u rekama je višestruk. Promene u režimu nanosa imaju direktne reprekusije na stanje i kvalitet vodnih ekosistema, posledice pojave poplavnih talasa, sa posebnim uticajem na povećanje troškova prečišćavanja voda, postojeća energetska postrojenja i vodne akumulacije. U ovom radu dat je novi pristup vremenskoj determinaciji transporta suspendovanog nanosa, kao i uticaj antropogenog faktora sa aspekta promene načina korišćenja zemljišta na režim nanosa za dugoročne vremenske serije.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac",
title = "Prilog proučavanju dinamike transporta suspendovanog nanosa kao posledica promena u životnoj sredini",
pages = "387-393",
url = "https://hdl.handle.net/21.15107/rcub_gery_1291"
}

Manojlović, S., Srejić, T., Sibinović, M., Carević, I.,& Batoćanin, N.. (2021). Prilog proučavanju dinamike transporta suspendovanog nanosa kao posledica promena u životnoj sredini. in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac
Beograd : Asocijacija prostornih planera Srbije., 387-393.
https://hdl.handle.net/21.15107/rcub_gery_1291

Manojlović S, Srejić T, Sibinović M, Carević I, Batoćanin N. Prilog proučavanju dinamike transporta suspendovanog nanosa kao posledica promena u životnoj sredini. in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac. 2021;:387-393.
https://hdl.handle.net/21.15107/rcub_gery_1291 .

Manojlović, Sanja, Srejić, Tanja, Sibinović, Mikica, Carević, Ivana, Batoćanin, Natalija, "Prilog proučavanju dinamike transporta suspendovanog nanosa kao posledica promena u životnoj sredini" in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac (2021):387-393,
https://hdl.handle.net/21.15107/rcub_gery_1291 .

TY  - CONF
AU  - Carević, Ivana
AU  - Batoćanin, Natalija
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Srejić, Tanja
PY  - 2021
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1290
AB  - Eksploatacija geoloških resursa je oduvek imala značajnu ulogu u razvoju društva.
Širom sveta, pa i na teritoriji Srbije, rudarstvo ima dugu tradiciju i predstavlja važnu privrednu delatnost. Savremenom društvu su neophodni resursi mineralnih sirovina, a samim tim i
rudarska industrija, jer proizvodi dobijeni ovom delatnošću poboljšavaju kvalitet života i omogućavaju društveni rast. Podizanjem ekološke svesti i usvajanjem novih zakonskih regulativa,
gotovo sve rudarske kompanije usvajaju rigoroznu politiku i procedure zbog potrebe održivosti.
U razvijenim zemljama rudarska aktivnost je sada usko regulisana, a uticaji na životnu sredinu
se sve više kontrolišu. Obavezan deo plana zatvaranja rudnika predstavlja svakako rekultivacija
zemljišta, odnosno vraćanje zemljišta na kom se odvijala eksploatacija mineralnih sirovina u
prirodno ili ekonomski upotrebljivo stanje sa ciljem ublažavanja posledica rudarske aktivnosti
na životnu sredinu. Sastavni je deo zakonskih regulativa i procene uticaja na životnu sredinu u
mnogim zemljama.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac
T1  - Značaj geoloških resursa i uticaj njihove eksploatacije na životnu sredinu
SP  - 219
EP  - 224
UR  - https://hdl.handle.net/21.15107/rcub_gery_1290
ER  - 

@conference{
author = "Carević, Ivana and Batoćanin, Natalija and Manojlović, Sanja and Sibinović, Mikica and Srejić, Tanja",
year = "2021",
abstract = "Eksploatacija geoloških resursa je oduvek imala značajnu ulogu u razvoju društva.
Širom sveta, pa i na teritoriji Srbije, rudarstvo ima dugu tradiciju i predstavlja važnu privrednu delatnost. Savremenom društvu su neophodni resursi mineralnih sirovina, a samim tim i
rudarska industrija, jer proizvodi dobijeni ovom delatnošću poboljšavaju kvalitet života i omogućavaju društveni rast. Podizanjem ekološke svesti i usvajanjem novih zakonskih regulativa,
gotovo sve rudarske kompanije usvajaju rigoroznu politiku i procedure zbog potrebe održivosti.
U razvijenim zemljama rudarska aktivnost je sada usko regulisana, a uticaji na životnu sredinu
se sve više kontrolišu. Obavezan deo plana zatvaranja rudnika predstavlja svakako rekultivacija
zemljišta, odnosno vraćanje zemljišta na kom se odvijala eksploatacija mineralnih sirovina u
prirodno ili ekonomski upotrebljivo stanje sa ciljem ublažavanja posledica rudarske aktivnosti
na životnu sredinu. Sastavni je deo zakonskih regulativa i procene uticaja na životnu sredinu u
mnogim zemljama.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac",
title = "Značaj geoloških resursa i uticaj njihove eksploatacije na životnu sredinu",
pages = "219-224",
url = "https://hdl.handle.net/21.15107/rcub_gery_1290"
}

Carević, I., Batoćanin, N., Manojlović, S., Sibinović, M.,& Srejić, T.. (2021). Značaj geoloških resursa i uticaj njihove eksploatacije na životnu sredinu. in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac
Beograd : Asocijacija prostornih planera Srbije., 219-224.
https://hdl.handle.net/21.15107/rcub_gery_1290

Carević I, Batoćanin N, Manojlović S, Sibinović M, Srejić T. Značaj geoloških resursa i uticaj njihove eksploatacije na životnu sredinu. in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac. 2021;:219-224.
https://hdl.handle.net/21.15107/rcub_gery_1290 .

Carević, Ivana, Batoćanin, Natalija, Manojlović, Sanja, Sibinović, Mikica, Srejić, Tanja, "Značaj geoloških resursa i uticaj njihove eksploatacije na životnu sredinu" in Zbornik radova Jedanaestog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Vršac (2021):219-224,
https://hdl.handle.net/21.15107/rcub_gery_1290 .

TY  - JOUR
AU  - Carević, Ivana
AU  - Sibinović, Mikica
AU  - Manojlović, Sanja
AU  - Batoćanin, Natalija
AU  - Petrović, Aleksandar S.
AU  - Srejić, Tanja
PY  - 2021
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1114
AB  - One of the biggest problems of environmental protection in Serbia is landfills. It is often a case that the economic interests are predominant in the landfill sitting; thus, most landfills are not located according to standards. This study shows that detailed geological data assets combined with geographical modeling represents a reliable way to define and locate the landfill site. Geological evaluation is discussed in detail with regard to bedrock lithology, quaternary geology, geological structure, hydrogeology, surface runoff patterns, and topography. An approach combining geographical modeling and geology is presented for determining the sites suitable for landfill selection with respect to their geologic favorability. As opposed to numerous research papers on this topic, in the methodological procedure, special importance is devoted to the analysis of the geological criteria. In this way, it is significantly easier to determine the landfill area with the best characteristics due to geological structure and lithology which unequivocally and precisely indicates inadequate territories for candidate sites. The multicriteria decision analysis (MCDA) is based on geological criteria upgraded with road (primary, residential, secondary, and tertiary), settlements network, railway, airport, infrastructure, land use, hypsometry aquifer, wetland, and surface water. The score values are divided into four classes, i.e., restricted areas, suitable but avoid, suitable, and most suitable. Combining geographical modeling with geology led to the recognition of two locations to be most favorable for landfill site located in the most suitable area, which represents 25.3% of the study area.
PB  - Basel : MDPI
T2  - Sustainability
T1  - Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia
VL  - 13
IS  - 14
SP  - 7810
DO  - 10.3390/su13147810
UR  - https://hdl.handle.net/21.15107/rcub_gery_1114
ER  - 

@article{
author = "Carević, Ivana and Sibinović, Mikica and Manojlović, Sanja and Batoćanin, Natalija and Petrović, Aleksandar S. and Srejić, Tanja",
year = "2021",
abstract = "One of the biggest problems of environmental protection in Serbia is landfills. It is often a case that the economic interests are predominant in the landfill sitting; thus, most landfills are not located according to standards. This study shows that detailed geological data assets combined with geographical modeling represents a reliable way to define and locate the landfill site. Geological evaluation is discussed in detail with regard to bedrock lithology, quaternary geology, geological structure, hydrogeology, surface runoff patterns, and topography. An approach combining geographical modeling and geology is presented for determining the sites suitable for landfill selection with respect to their geologic favorability. As opposed to numerous research papers on this topic, in the methodological procedure, special importance is devoted to the analysis of the geological criteria. In this way, it is significantly easier to determine the landfill area with the best characteristics due to geological structure and lithology which unequivocally and precisely indicates inadequate territories for candidate sites. The multicriteria decision analysis (MCDA) is based on geological criteria upgraded with road (primary, residential, secondary, and tertiary), settlements network, railway, airport, infrastructure, land use, hypsometry aquifer, wetland, and surface water. The score values are divided into four classes, i.e., restricted areas, suitable but avoid, suitable, and most suitable. Combining geographical modeling with geology led to the recognition of two locations to be most favorable for landfill site located in the most suitable area, which represents 25.3% of the study area.",
publisher = "Basel : MDPI",
journal = "Sustainability",
title = "Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia",
volume = "13",
number = "14",
pages = "7810",
doi = "10.3390/su13147810",
url = "https://hdl.handle.net/21.15107/rcub_gery_1114"
}

Carević, I., Sibinović, M., Manojlović, S., Batoćanin, N., Petrović, A. S.,& Srejić, T.. (2021). Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia. in Sustainability
Basel : MDPI., 13(14), 7810.
https://doi.org/10.3390/su13147810
https://hdl.handle.net/21.15107/rcub_gery_1114

Carević I, Sibinović M, Manojlović S, Batoćanin N, Petrović AS, Srejić T. Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia. in Sustainability. 2021;13(14):7810.
doi:10.3390/su13147810
https://hdl.handle.net/21.15107/rcub_gery_1114 .

Carević, Ivana, Sibinović, Mikica, Manojlović, Sanja, Batoćanin, Natalija, Petrović, Aleksandar S., Srejić, Tanja, "Geological Approach for Landfill Site Selection: A Case Study of Vršac Municipality, Serbia" in Sustainability, 13, no. 14 (2021):7810,
https://doi.org/10.3390/su13147810 .,
https://hdl.handle.net/21.15107/rcub_gery_1114 .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Sibinović, Mikica
AU  - Srejić, Tanja
AU  - Hadud, Abosa
AU  - Sabri, Ibrahim
PY  - 2021
UR  - https://gery.gef.bg.ac.rs/handle/123456789/1083
AB  - This study expounds the dynamic relationships among agricultural land-use change, rural population migration, and sediment transport. The variability of suspended sediment load was detected by Mann-Kendall and Pettitt tests. From 1961 to 2007, the annual trend in suspended sediment concentration and sediment load demonstrated significant reduction (alpha = 0.001), with decreasing rates of 0.0144 g/L/y and 84.7 t/y, respectively. An abrupt change-point was detected in 1984 for the sediment load (p = 0.0001). The double-mass curve method and regression analysis of sediment load versus precipitation were used to quantify the effects of climate change and human activities on sediment load variations. The changes in sediment load were predominantly impacted by human activities (89%), while precipitation explained 11% of the reduction in suspended sediment. An important land-use change recorded in the Juzna Morava river basin comprised the abandonment of agricultural lands due to depopulation processes, as well as economic and social changes, which was followed by significant impacts on soil erosion and sediment transport. Land abandonment was most pronounced in marginal mountain or semi-mountainous areas, where agriculture was until recent decades traditional or semi-traditional. The results of the correlation matrix were significant at the p  lt  0.05 level, demonstrating that the decrease of rural population, agricultural land, and arable land were directly related to the decline of suspended sediment. High correlation coefficients were found between anthropogenic indicators and sediment parameters, ranging from 0.94 to 0.97.
PB  - Basel : MDPI
T2  - Sustainability
T1  - Agriculture Land Use Change and Demographic Change in Response to Decline Suspended Sediment in Juzna Morava River Basin (Serbia)
VL  - 13
IS  - 6
DO  - 10.3390/su13063130
UR  - https://hdl.handle.net/21.15107/rcub_gery_1083
ER  - 

@article{
author = "Manojlović, Sanja and Sibinović, Mikica and Srejić, Tanja and Hadud, Abosa and Sabri, Ibrahim",
year = "2021",
abstract = "This study expounds the dynamic relationships among agricultural land-use change, rural population migration, and sediment transport. The variability of suspended sediment load was detected by Mann-Kendall and Pettitt tests. From 1961 to 2007, the annual trend in suspended sediment concentration and sediment load demonstrated significant reduction (alpha = 0.001), with decreasing rates of 0.0144 g/L/y and 84.7 t/y, respectively. An abrupt change-point was detected in 1984 for the sediment load (p = 0.0001). The double-mass curve method and regression analysis of sediment load versus precipitation were used to quantify the effects of climate change and human activities on sediment load variations. The changes in sediment load were predominantly impacted by human activities (89%), while precipitation explained 11% of the reduction in suspended sediment. An important land-use change recorded in the Juzna Morava river basin comprised the abandonment of agricultural lands due to depopulation processes, as well as economic and social changes, which was followed by significant impacts on soil erosion and sediment transport. Land abandonment was most pronounced in marginal mountain or semi-mountainous areas, where agriculture was until recent decades traditional or semi-traditional. The results of the correlation matrix were significant at the p  lt  0.05 level, demonstrating that the decrease of rural population, agricultural land, and arable land were directly related to the decline of suspended sediment. High correlation coefficients were found between anthropogenic indicators and sediment parameters, ranging from 0.94 to 0.97.",
publisher = "Basel : MDPI",
journal = "Sustainability",
title = "Agriculture Land Use Change and Demographic Change in Response to Decline Suspended Sediment in Juzna Morava River Basin (Serbia)",
volume = "13",
number = "6",
doi = "10.3390/su13063130",
url = "https://hdl.handle.net/21.15107/rcub_gery_1083"
}

Manojlović, S., Sibinović, M., Srejić, T., Hadud, A.,& Sabri, I.. (2021). Agriculture Land Use Change and Demographic Change in Response to Decline Suspended Sediment in Juzna Morava River Basin (Serbia). in Sustainability
Basel : MDPI., 13(6).
https://doi.org/10.3390/su13063130
https://hdl.handle.net/21.15107/rcub_gery_1083

Manojlović S, Sibinović M, Srejić T, Hadud A, Sabri I. Agriculture Land Use Change and Demographic Change in Response to Decline Suspended Sediment in Juzna Morava River Basin (Serbia). in Sustainability. 2021;13(6).
doi:10.3390/su13063130
https://hdl.handle.net/21.15107/rcub_gery_1083 .

Manojlović, Sanja, Sibinović, Mikica, Srejić, Tanja, Hadud, Abosa, Sabri, Ibrahim, "Agriculture Land Use Change and Demographic Change in Response to Decline Suspended Sediment in Juzna Morava River Basin (Serbia)" in Sustainability, 13, no. 6 (2021),
https://doi.org/10.3390/su13063130 .,
https://hdl.handle.net/21.15107/rcub_gery_1083 .

TY  - CONF
AU  - Carević, Ivana
AU  - Sibinović, Mikica
AU  - Manojlović, Sanja
AU  - Batoćanin, Natalija
PY  - 2019
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1653
AB  - "Tupižnička ledenica" predstavlja krašku jamu sa interesantnim mikroklimatskim obeležjima i zadržavanjem snega i leda u većem delu godine. Jama je formirana u prekristalisalim neritskim bankovitim i masivnim donjokrednim krečnjacima (fosiloferni biomikriti) koji pripadaju mudstone mikrofaciji. Kao takva, “Tupižnička ledenica” predstavlja važan relikt koji oslikava značajne momente u razvoju Zemljine kore na teritoriji opštine Knjaževac. Početkom 2019. godine je dobila status Spomenik prirode i svrstana je u I kategoriju zaštićenog područja nacionalnog, odnosno izuzetnog značaja. Mogućnost ostvarivanja turističke ponude opštine Knjaževac na bazi prezentacije jedinstvenih prirodnih vrednosti “Tupižničke ledenice” predstavlja jedan od potencijala ove opštine. Osnovna ograničenja za efikasniju zaštitu “Tupižničke ledenice” mogu da se jave usled nepoštovanja režima zaštite zaštićenog prirodnog dobra, nedovoljne dostupnosti zbog nekvalitetne mreže puteva kao i nedovoljne integracije geonasleđa u turističku prezentaciju.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Desetog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Palić-Subotica
T1  - Spomenik prirode "Tupižnička ledenica": status i značaj u prostornom planiranju opštine Knjaževac
SP  - 297
EP  - 302
UR  - https://hdl.handle.net/21.15107/rcub_gery_1653
ER  - 

@conference{
author = "Carević, Ivana and Sibinović, Mikica and Manojlović, Sanja and Batoćanin, Natalija",
year = "2019",
abstract = ""Tupižnička ledenica" predstavlja krašku jamu sa interesantnim mikroklimatskim obeležjima i zadržavanjem snega i leda u većem delu godine. Jama je formirana u prekristalisalim neritskim bankovitim i masivnim donjokrednim krečnjacima (fosiloferni biomikriti) koji pripadaju mudstone mikrofaciji. Kao takva, “Tupižnička ledenica” predstavlja važan relikt koji oslikava značajne momente u razvoju Zemljine kore na teritoriji opštine Knjaževac. Početkom 2019. godine je dobila status Spomenik prirode i svrstana je u I kategoriju zaštićenog područja nacionalnog, odnosno izuzetnog značaja. Mogućnost ostvarivanja turističke ponude opštine Knjaževac na bazi prezentacije jedinstvenih prirodnih vrednosti “Tupižničke ledenice” predstavlja jedan od potencijala ove opštine. Osnovna ograničenja za efikasniju zaštitu “Tupižničke ledenice” mogu da se jave usled nepoštovanja režima zaštite zaštićenog prirodnog dobra, nedovoljne dostupnosti zbog nekvalitetne mreže puteva kao i nedovoljne integracije geonasleđa u turističku prezentaciju.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Desetog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Palić-Subotica",
title = "Spomenik prirode "Tupižnička ledenica": status i značaj u prostornom planiranju opštine Knjaževac",
pages = "297-302",
url = "https://hdl.handle.net/21.15107/rcub_gery_1653"
}

Carević, I., Sibinović, M., Manojlović, S.,& Batoćanin, N.. (2019). Spomenik prirode "Tupižnička ledenica": status i značaj u prostornom planiranju opštine Knjaževac. in Zbornik radova Desetog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Palić-Subotica
Beograd : Asocijacija prostornih planera Srbije., 297-302.
https://hdl.handle.net/21.15107/rcub_gery_1653

Carević I, Sibinović M, Manojlović S, Batoćanin N. Spomenik prirode "Tupižnička ledenica": status i značaj u prostornom planiranju opštine Knjaževac. in Zbornik radova Desetog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Palić-Subotica. 2019;:297-302.
https://hdl.handle.net/21.15107/rcub_gery_1653 .

Carević, Ivana, Sibinović, Mikica, Manojlović, Sanja, Batoćanin, Natalija, "Spomenik prirode "Tupižnička ledenica": status i značaj u prostornom planiranju opštine Knjaževac" in Zbornik radova Desetog naučno-stručnog skupa sa međunarodnim učešćem "Planska i normativna zaštita prostora i životne sredine", Palić-Subotica (2019):297-302,
https://hdl.handle.net/21.15107/rcub_gery_1653 .

TY  - CONF
AU  - Manojlović, Sanja
AU  - Dobrosavljević, Tanja
AU  - Gocić, Milena
AU  - Milošević, Marko V.
AU  - Manojlović, Predrag
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/888
AB  - Global climate change and changes caused by human activity have had a considerable impact on river systems. Recent studies have observed different trends of water discharge and sediment transport for the largest rivers in the world. This paper deals with the trend analysis of suspended sediment load (Qs) at the most downstream hydrological station of the Juzna Morava (Mojsinje). The data, which were obtained from the Republic Hydrometeorological Service of Serbia (RHSS), included daily values of water discharge (Q) and suspended sediment concentration (SSC) for the time period 1958-2007. The trend of sediment load was determined using the non-parametric Mann-Kendall test, while the Pettitt test was used to establish the transition year. The results show that the average perennial suspended sediment load for the given time period was 2.47x10(6) t (160.5 t/km(2)/yr), ranging from 0.04x10(6) t (2.6 t/km(2)/yr) to 9.85x10(6) t (640.3 t/km(2)/yr). The average decrease in sediment yield was 5.15 t/km(2)/yr with high statistical significance of 0.001. Using the Pettitt test, the year of 1985 was determined as a transition year in suspended sediment load. Suspended sediment load declined by 71% in the period after 1985.
PB  - Catena Verlag, Reiskirchen
C3  - Proceedings of the 3rd Conference of the World Association of Soil and Water Conservation (WASWAC)
T1  - Trend analysis of annual water discharge and sediment load in the Juzna Morava River (Serbia) during 1958-2007
VL  - 45
SP  - 79
EP  - 87
UR  - https://hdl.handle.net/21.15107/rcub_gery_888
ER  - 

@conference{
author = "Manojlović, Sanja and Dobrosavljević, Tanja and Gocić, Milena and Milošević, Marko V. and Manojlović, Predrag",
year = "2018",
abstract = "Global climate change and changes caused by human activity have had a considerable impact on river systems. Recent studies have observed different trends of water discharge and sediment transport for the largest rivers in the world. This paper deals with the trend analysis of suspended sediment load (Qs) at the most downstream hydrological station of the Juzna Morava (Mojsinje). The data, which were obtained from the Republic Hydrometeorological Service of Serbia (RHSS), included daily values of water discharge (Q) and suspended sediment concentration (SSC) for the time period 1958-2007. The trend of sediment load was determined using the non-parametric Mann-Kendall test, while the Pettitt test was used to establish the transition year. The results show that the average perennial suspended sediment load for the given time period was 2.47x10(6) t (160.5 t/km(2)/yr), ranging from 0.04x10(6) t (2.6 t/km(2)/yr) to 9.85x10(6) t (640.3 t/km(2)/yr). The average decrease in sediment yield was 5.15 t/km(2)/yr with high statistical significance of 0.001. Using the Pettitt test, the year of 1985 was determined as a transition year in suspended sediment load. Suspended sediment load declined by 71% in the period after 1985.",
publisher = "Catena Verlag, Reiskirchen",
journal = "Proceedings of the 3rd Conference of the World Association of Soil and Water Conservation (WASWAC)",
title = "Trend analysis of annual water discharge and sediment load in the Juzna Morava River (Serbia) during 1958-2007",
volume = "45",
pages = "79-87",
url = "https://hdl.handle.net/21.15107/rcub_gery_888"
}

Manojlović, S., Dobrosavljević, T., Gocić, M., Milošević, M. V.,& Manojlović, P.. (2018). Trend analysis of annual water discharge and sediment load in the Juzna Morava River (Serbia) during 1958-2007. in Proceedings of the 3rd Conference of the World Association of Soil and Water Conservation (WASWAC)
Catena Verlag, Reiskirchen., 45, 79-87.
https://hdl.handle.net/21.15107/rcub_gery_888

Manojlović S, Dobrosavljević T, Gocić M, Milošević MV, Manojlović P. Trend analysis of annual water discharge and sediment load in the Juzna Morava River (Serbia) during 1958-2007. in Proceedings of the 3rd Conference of the World Association of Soil and Water Conservation (WASWAC). 2018;45:79-87.
https://hdl.handle.net/21.15107/rcub_gery_888 .

Manojlović, Sanja, Dobrosavljević, Tanja, Gocić, Milena, Milošević, Marko V., Manojlović, Predrag, "Trend analysis of annual water discharge and sediment load in the Juzna Morava River (Serbia) during 1958-2007" in Proceedings of the 3rd Conference of the World Association of Soil and Water Conservation (WASWAC), 45 (2018):79-87,
https://hdl.handle.net/21.15107/rcub_gery_888 .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Antić, Marija
AU  - Šantić, Danica
AU  - Sibinović, Mikica
AU  - Carević, Ivana
AU  - Srejić, Tanja
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/947
AB  - In many Eastern European countries, the standard of living increased as a result of the process of industrialization in the second half of the 20th Century. Consequently, the population in rural areas with small-scale farming decreased due to the availability of employment elsewhere. This directly impacted soil erosion (and thereby sustainability of the land), but the degree and direction are not well known. This study investigates two municipalities within Serbia, their change in population and its impact on land use changes and soil erosion. The standard of living increased after the industrialization process in the 1960s within these municipalities. The erosion potential model is used to calculate gross annual erosion. The changes related to population and arable land in rural settlements are analyzed according to proportional spatial changes. The results show an overall decrease of erosion intensity in the study area. In addition, two basic findings are derived: first, the highest level of human impact on soil is in rural settlements at the lowest elevation zones, where erosion intensity shows the least amount of decrease; and, second, the most intensive depopulation process, recorded in higher elevation zones, indicates a rapid decrease of erosion intensity.
PB  - Basel : MDPI
T2  - Sustainability
T1  - Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia
VL  - 10
IS  - 3
DO  - 10.3390/su10030826
UR  - https://hdl.handle.net/21.15107/rcub_gery_947
ER  - 

@article{
author = "Manojlović, Sanja and Antić, Marija and Šantić, Danica and Sibinović, Mikica and Carević, Ivana and Srejić, Tanja",
year = "2018",
abstract = "In many Eastern European countries, the standard of living increased as a result of the process of industrialization in the second half of the 20th Century. Consequently, the population in rural areas with small-scale farming decreased due to the availability of employment elsewhere. This directly impacted soil erosion (and thereby sustainability of the land), but the degree and direction are not well known. This study investigates two municipalities within Serbia, their change in population and its impact on land use changes and soil erosion. The standard of living increased after the industrialization process in the 1960s within these municipalities. The erosion potential model is used to calculate gross annual erosion. The changes related to population and arable land in rural settlements are analyzed according to proportional spatial changes. The results show an overall decrease of erosion intensity in the study area. In addition, two basic findings are derived: first, the highest level of human impact on soil is in rural settlements at the lowest elevation zones, where erosion intensity shows the least amount of decrease; and, second, the most intensive depopulation process, recorded in higher elevation zones, indicates a rapid decrease of erosion intensity.",
publisher = "Basel : MDPI",
journal = "Sustainability",
title = "Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia",
volume = "10",
number = "3",
doi = "10.3390/su10030826",
url = "https://hdl.handle.net/21.15107/rcub_gery_947"
}

Manojlović, S., Antić, M., Šantić, D., Sibinović, M., Carević, I.,& Srejić, T.. (2018). Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia. in Sustainability
Basel : MDPI., 10(3).
https://doi.org/10.3390/su10030826
https://hdl.handle.net/21.15107/rcub_gery_947

Manojlović S, Antić M, Šantić D, Sibinović M, Carević I, Srejić T. Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia. in Sustainability. 2018;10(3).
doi:10.3390/su10030826
https://hdl.handle.net/21.15107/rcub_gery_947 .

Manojlović, Sanja, Antić, Marija, Šantić, Danica, Sibinović, Mikica, Carević, Ivana, Srejić, Tanja, "Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia" in Sustainability, 10, no. 3 (2018),
https://doi.org/10.3390/su10030826 .,
https://hdl.handle.net/21.15107/rcub_gery_947 .

TY  - JOUR
AU  - Anđelković, Goran
AU  - Jovanović, Slavoljub
AU  - Manojlović, Sanja
AU  - Samardžić, Ivan
AU  - Živković, Ljiljana
AU  - Šabić, Dejan
AU  - Gatarić, Dragica
AU  - Džinović, Milanka
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/944
AB  - Considering recent weather events in Serbia (especially the floods in 2014), a need has arisen for research that would help in identifying extreme weather phenomena. Therefore, the aim of this paper is to determine the thresholds above which intense precipitation can be considered as extreme precipitation events in Serbia. In this study, we determined the frequency of precipitation occurring at an intensity above the threshold of an extreme phenomenon (1961-2015), as well as the frequency of precipitation occurring at or above the absolute daily maximum in the reference period (1961-1990). The study sample included daily rainfall observations from 28 stations from the national meteorological network in Serbia. Applying a decile method, all the stations recording precipitation above the threshold of dangerous phenomena on the same day are classified into the corresponding decile. The threshold value was determined as the average value of the extreme annual precipitation in the analyzed period. The cases that are due to the high prevalence listed in the last decile are considered extreme. The results showed that the critical number of observation points above which an event is considered extreme precipitation event is 6.21, and a warning of the danger could be ensured only in the case of neighboring stations in the network. The threshold of extreme precipitation events for the individual stations ranges up to 130 mm. The obtained results might be used to mitigate the effects of extreme precipitation events in Serbia in the future.
PB  - Basel : MDPI
T2  - Atmosphere
T1  - Extreme Precipitation Events in Serbia: Defining the Threshold Criteria for Emergency Preparedness
VL  - 9
IS  - 5
DO  - 10.3390/atmos9050188
UR  - https://hdl.handle.net/21.15107/rcub_gery_944
ER  - 

@article{
author = "Anđelković, Goran and Jovanović, Slavoljub and Manojlović, Sanja and Samardžić, Ivan and Živković, Ljiljana and Šabić, Dejan and Gatarić, Dragica and Džinović, Milanka",
year = "2018",
abstract = "Considering recent weather events in Serbia (especially the floods in 2014), a need has arisen for research that would help in identifying extreme weather phenomena. Therefore, the aim of this paper is to determine the thresholds above which intense precipitation can be considered as extreme precipitation events in Serbia. In this study, we determined the frequency of precipitation occurring at an intensity above the threshold of an extreme phenomenon (1961-2015), as well as the frequency of precipitation occurring at or above the absolute daily maximum in the reference period (1961-1990). The study sample included daily rainfall observations from 28 stations from the national meteorological network in Serbia. Applying a decile method, all the stations recording precipitation above the threshold of dangerous phenomena on the same day are classified into the corresponding decile. The threshold value was determined as the average value of the extreme annual precipitation in the analyzed period. The cases that are due to the high prevalence listed in the last decile are considered extreme. The results showed that the critical number of observation points above which an event is considered extreme precipitation event is 6.21, and a warning of the danger could be ensured only in the case of neighboring stations in the network. The threshold of extreme precipitation events for the individual stations ranges up to 130 mm. The obtained results might be used to mitigate the effects of extreme precipitation events in Serbia in the future.",
publisher = "Basel : MDPI",
journal = "Atmosphere",
title = "Extreme Precipitation Events in Serbia: Defining the Threshold Criteria for Emergency Preparedness",
volume = "9",
number = "5",
doi = "10.3390/atmos9050188",
url = "https://hdl.handle.net/21.15107/rcub_gery_944"
}

Anđelković, G., Jovanović, S., Manojlović, S., Samardžić, I., Živković, L., Šabić, D., Gatarić, D.,& Džinović, M.. (2018). Extreme Precipitation Events in Serbia: Defining the Threshold Criteria for Emergency Preparedness. in Atmosphere
Basel : MDPI., 9(5).
https://doi.org/10.3390/atmos9050188
https://hdl.handle.net/21.15107/rcub_gery_944

Anđelković G, Jovanović S, Manojlović S, Samardžić I, Živković L, Šabić D, Gatarić D, Džinović M. Extreme Precipitation Events in Serbia: Defining the Threshold Criteria for Emergency Preparedness. in Atmosphere. 2018;9(5).
doi:10.3390/atmos9050188
https://hdl.handle.net/21.15107/rcub_gery_944 .

Anđelković, Goran, Jovanović, Slavoljub, Manojlović, Sanja, Samardžić, Ivan, Živković, Ljiljana, Šabić, Dejan, Gatarić, Dragica, Džinović, Milanka, "Extreme Precipitation Events in Serbia: Defining the Threshold Criteria for Emergency Preparedness" in Atmosphere, 9, no. 5 (2018),
https://doi.org/10.3390/atmos9050188 .,
https://hdl.handle.net/21.15107/rcub_gery_944 .

TY  - JOUR
AU  - Tošić, Radislav
AU  - Lovrić, Novica
AU  - Dragićević, Slavoljub
AU  - Manojlović, Sanja
PY  - 2018
UR  - https://gery.gef.bg.ac.rs/handle/123456789/941
AB  - Torrential floods are the most frequent natural hazard events in Bosnia and Herzegovina. The increase of intensive rains in Bosnia and Herzegovina over last years, as a consequence of the climate changes, has triggered many torrential floods, which have generated a lot of damages and losses of human lives. This study was focused on development of torrential susceptibility model using GMM Method and GIS in the Vrbas river basin as an attempt to create a new methodological approach which can be used on other river basins in Bosnia and Herzegovina. First, a total of 174 torrential basins were identified in the Vrbas river basin, as a base for creating an inventory map, which was a base map for the assessment of torrential floods susceptibility. The GIS Matrix Method and six influencing factors were used for generation of Torrential Flood Susceptibility Model. Based on the obtained values of Torrential Flood Susceptibility Model for the Vrbas river basin, 45.52% of the study area is within strong and very strong susceptibility category. The Torrential Flood Susceptibility Model was validated using a "degree of fit" method. Validation indicators of the TFSM show that the 80.04% are in the category of strong and very strong susceptibility, while only 4.37% are in the category of very low and low susceptibility. This fact suggests that used methodology based on GMM method and used influencing factors enable delimitation of the area with high and very high susceptibility to torrential floods into the Vrbas basin. Therefore, used methodological approach represents a good base for future research, and it has potential for the practical use and should be tested in other river basins in Bosnia and Herzegovina.
PB  - Baia Mare : North University of Baia Mare
T2  - Carpathian Journal of Earth and Environmental Sciences
T1  - Assessment of torrential flood susceptibility using GIS matrix method: case study - Vrbas river basin (B&H)
VL  - 13
IS  - 2
SP  - 369
EP  - 382
DO  - 10.26471/cjees/2018/013/032
UR  - https://hdl.handle.net/21.15107/rcub_gery_941
ER  - 

@article{
author = "Tošić, Radislav and Lovrić, Novica and Dragićević, Slavoljub and Manojlović, Sanja",
year = "2018",
abstract = "Torrential floods are the most frequent natural hazard events in Bosnia and Herzegovina. The increase of intensive rains in Bosnia and Herzegovina over last years, as a consequence of the climate changes, has triggered many torrential floods, which have generated a lot of damages and losses of human lives. This study was focused on development of torrential susceptibility model using GMM Method and GIS in the Vrbas river basin as an attempt to create a new methodological approach which can be used on other river basins in Bosnia and Herzegovina. First, a total of 174 torrential basins were identified in the Vrbas river basin, as a base for creating an inventory map, which was a base map for the assessment of torrential floods susceptibility. The GIS Matrix Method and six influencing factors were used for generation of Torrential Flood Susceptibility Model. Based on the obtained values of Torrential Flood Susceptibility Model for the Vrbas river basin, 45.52% of the study area is within strong and very strong susceptibility category. The Torrential Flood Susceptibility Model was validated using a "degree of fit" method. Validation indicators of the TFSM show that the 80.04% are in the category of strong and very strong susceptibility, while only 4.37% are in the category of very low and low susceptibility. This fact suggests that used methodology based on GMM method and used influencing factors enable delimitation of the area with high and very high susceptibility to torrential floods into the Vrbas basin. Therefore, used methodological approach represents a good base for future research, and it has potential for the practical use and should be tested in other river basins in Bosnia and Herzegovina.",
publisher = "Baia Mare : North University of Baia Mare",
journal = "Carpathian Journal of Earth and Environmental Sciences",
title = "Assessment of torrential flood susceptibility using GIS matrix method: case study - Vrbas river basin (B&H)",
volume = "13",
number = "2",
pages = "369-382",
doi = "10.26471/cjees/2018/013/032",
url = "https://hdl.handle.net/21.15107/rcub_gery_941"
}

Tošić, R., Lovrić, N., Dragićević, S.,& Manojlović, S.. (2018). Assessment of torrential flood susceptibility using GIS matrix method: case study - Vrbas river basin (B&H). in Carpathian Journal of Earth and Environmental Sciences
Baia Mare : North University of Baia Mare., 13(2), 369-382.
https://doi.org/10.26471/cjees/2018/013/032
https://hdl.handle.net/21.15107/rcub_gery_941

Tošić R, Lovrić N, Dragićević S, Manojlović S. Assessment of torrential flood susceptibility using GIS matrix method: case study - Vrbas river basin (B&H). in Carpathian Journal of Earth and Environmental Sciences. 2018;13(2):369-382.
doi:10.26471/cjees/2018/013/032
https://hdl.handle.net/21.15107/rcub_gery_941 .

Tošić, Radislav, Lovrić, Novica, Dragićević, Slavoljub, Manojlović, Sanja, "Assessment of torrential flood susceptibility using GIS matrix method: case study - Vrbas river basin (B&H)" in Carpathian Journal of Earth and Environmental Sciences, 13, no. 2 (2018):369-382,
https://doi.org/10.26471/cjees/2018/013/032 .,
https://hdl.handle.net/21.15107/rcub_gery_941 .

TY  - JOUR
AU  - Manojlović, Sanja
AU  - Antić, Marija
AU  - Sibinović, Mikica
AU  - Dragićević, Slavoljub
AU  - Novković, Ivan
PY  - 2017
UR  - https://gery.gef.bg.ac.rs/handle/123456789/811
AB  - In this paper the relationship between demographic and land use changes and their impact on the intensity of erosion processes in the Nisava River basin is examined by using quantitative typology. For the purposes of quantifying the erosion intensity changes, the erosion potential model (EPM) was used to calculate the annual gross erosion and spatial distribution of soil erosion in study area. The value of the erosion coefficient was reduced from Z(1) = 0.443 in 1971 to Z(2) = 0.356 in 2011. Specific annual gross erosion in the Nisava River basin was 765.3 m(3)/km(2)/year in 1971 while in 2011 it was 533.3 m(3)/km(2)/year. Therefore, due to changes in intensity of erosion processes the specific annual gross erosion in study area was decreased for 232.3 m(3)/km(2)/year. In 40-year period, there were no significant changes in natural conditions, so the anthropogenic influences were responsible for the reduced erosion intensity. Research results indicate three types of population and land use changes with different scale and intensity of erosion process: progressive type with favourable demographic potentials, huge land use transformation and intensive process of soil erosion; stagnant type with advanced agricultural and demographic dimension which imposed pressures to the environment and soil erosion; regressive type and dominant regressive sub-type with depopulation and deagrarization have significant decereasing effect on soil erosion. These results are basis for all integral soil and water management projects, forest ecosystems and environmental protection, spatial planning, agriculture and other human activities.
PB  - Parlar Scientific Publications
T2  - Fresenius Environmental Bulletin
T1  - Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia
VL  - 26
IS  - 12
SP  - 7547
EP  - 7560
UR  - https://hdl.handle.net/21.15107/rcub_gery_811
ER  - 

@article{
author = "Manojlović, Sanja and Antić, Marija and Sibinović, Mikica and Dragićević, Slavoljub and Novković, Ivan",
year = "2017",
abstract = "In this paper the relationship between demographic and land use changes and their impact on the intensity of erosion processes in the Nisava River basin is examined by using quantitative typology. For the purposes of quantifying the erosion intensity changes, the erosion potential model (EPM) was used to calculate the annual gross erosion and spatial distribution of soil erosion in study area. The value of the erosion coefficient was reduced from Z(1) = 0.443 in 1971 to Z(2) = 0.356 in 2011. Specific annual gross erosion in the Nisava River basin was 765.3 m(3)/km(2)/year in 1971 while in 2011 it was 533.3 m(3)/km(2)/year. Therefore, due to changes in intensity of erosion processes the specific annual gross erosion in study area was decreased for 232.3 m(3)/km(2)/year. In 40-year period, there were no significant changes in natural conditions, so the anthropogenic influences were responsible for the reduced erosion intensity. Research results indicate three types of population and land use changes with different scale and intensity of erosion process: progressive type with favourable demographic potentials, huge land use transformation and intensive process of soil erosion; stagnant type with advanced agricultural and demographic dimension which imposed pressures to the environment and soil erosion; regressive type and dominant regressive sub-type with depopulation and deagrarization have significant decereasing effect on soil erosion. These results are basis for all integral soil and water management projects, forest ecosystems and environmental protection, spatial planning, agriculture and other human activities.",
publisher = "Parlar Scientific Publications",
journal = "Fresenius Environmental Bulletin",
title = "Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia",
volume = "26",
number = "12",
pages = "7547-7560",
url = "https://hdl.handle.net/21.15107/rcub_gery_811"
}

Manojlović, S., Antić, M., Sibinović, M., Dragićević, S.,& Novković, I.. (2017). Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia. in Fresenius Environmental Bulletin
Parlar Scientific Publications., 26(12), 7547-7560.
https://hdl.handle.net/21.15107/rcub_gery_811

Manojlović S, Antić M, Sibinović M, Dragićević S, Novković I. Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia. in Fresenius Environmental Bulletin. 2017;26(12):7547-7560.
https://hdl.handle.net/21.15107/rcub_gery_811 .

Manojlović, Sanja, Antić, Marija, Sibinović, Mikica, Dragićević, Slavoljub, Novković, Ivan, "Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia" in Fresenius Environmental Bulletin, 26, no. 12 (2017):7547-7560,
https://hdl.handle.net/21.15107/rcub_gery_811 .

TY  - JOUR
AU  - Langović, Marko
AU  - Manojlović, Sanja
AU  - Čvorović, Zoran
PY  - 2017
UR  - https://gery.gef.bg.ac.rs/handle/123456789/810
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Trends of mean annual river discharges in the Zapadna Morava river basin
VL  - 97
IS  - 2
SP  - 19
EP  - 45
DO  - 10.2298/GSGD1702019L
UR  - https://hdl.handle.net/21.15107/rcub_gery_810
ER  - 

@article{
author = "Langović, Marko and Manojlović, Sanja and Čvorović, Zoran",
year = "2017",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Trends of mean annual river discharges in the Zapadna Morava river basin",
volume = "97",
number = "2",
pages = "19-45",
doi = "10.2298/GSGD1702019L",
url = "https://hdl.handle.net/21.15107/rcub_gery_810"
}

Langović, M., Manojlović, S.,& Čvorović, Z.. (2017). Trends of mean annual river discharges in the Zapadna Morava river basin. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 97(2), 19-45.
https://doi.org/10.2298/GSGD1702019L
https://hdl.handle.net/21.15107/rcub_gery_810

Langović M, Manojlović S, Čvorović Z. Trends of mean annual river discharges in the Zapadna Morava river basin. in Glasnik Srpskog geografskog društva. 2017;97(2):19-45.
doi:10.2298/GSGD1702019L
https://hdl.handle.net/21.15107/rcub_gery_810 .

Langović, Marko, Manojlović, Sanja, Čvorović, Zoran, "Trends of mean annual river discharges in the Zapadna Morava river basin" in Glasnik Srpskog geografskog društva, 97, no. 2 (2017):19-45,
https://doi.org/10.2298/GSGD1702019L .,
https://hdl.handle.net/21.15107/rcub_gery_810 .

TY  - CONF
AU  - Dobrosavljević, Tanja
AU  - Manojlović, Sanja
AU  - Gocić, Milena
AU  - Srejić, Milan
PY  - 2016
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1289
AB  - Održivo korišćenje resursa lokalne sredine je moguće samo uz identifikaciju glavnih faktora njihove degradacije. Jedan od glavnih faktora degradacije celokupne životne sredine je erozija i transport nanosa. Rad se bavi procesom mehaničke vodne erozije u slivu Crnice sa stanovišta njegove prostorno-vremenske varijabilnosti. Empirijski metod Gavrilović, u kombinaciji sa savremenim programskim paketima i teledetekcionim metodama, omogućio je precizno utvrđivanje uticaja glavnih fizičko-geografskih faktora na proces erozije u slivu. Rezultati istraživanja su pokazali da je u periodu 1971-2011. godine došlo do smanjenja erozije za 13%. Sklop fizičko-geografskih i antropogenih faktora je doveo do specifične prostorne raspodele produkcije nanosa u slivu Crnice. Karte produkcije nanosa u slivu Crnice za 1971. i 2011. godinu, mogu biti osnova za rešavanje ključnih problema grada Paraćina i njegove okoline.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Šestog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Vršac
T1  - Mehanička vodna erozija u slivu Crnice
SP  - 445
EP  - 452
UR  - https://hdl.handle.net/21.15107/rcub_gery_1289
ER  - 

@conference{
author = "Dobrosavljević, Tanja and Manojlović, Sanja and Gocić, Milena and Srejić, Milan",
year = "2016",
abstract = "Održivo korišćenje resursa lokalne sredine je moguće samo uz identifikaciju glavnih faktora njihove degradacije. Jedan od glavnih faktora degradacije celokupne životne sredine je erozija i transport nanosa. Rad se bavi procesom mehaničke vodne erozije u slivu Crnice sa stanovišta njegove prostorno-vremenske varijabilnosti. Empirijski metod Gavrilović, u kombinaciji sa savremenim programskim paketima i teledetekcionim metodama, omogućio je precizno utvrđivanje uticaja glavnih fizičko-geografskih faktora na proces erozije u slivu. Rezultati istraživanja su pokazali da je u periodu 1971-2011. godine došlo do smanjenja erozije za 13%. Sklop fizičko-geografskih i antropogenih faktora je doveo do specifične prostorne raspodele produkcije nanosa u slivu Crnice. Karte produkcije nanosa u slivu Crnice za 1971. i 2011. godinu, mogu biti osnova za rešavanje ključnih problema grada Paraćina i njegove okoline.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Šestog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Vršac",
title = "Mehanička vodna erozija u slivu Crnice",
pages = "445-452",
url = "https://hdl.handle.net/21.15107/rcub_gery_1289"
}

Dobrosavljević, T., Manojlović, S., Gocić, M.,& Srejić, M.. (2016). Mehanička vodna erozija u slivu Crnice. in Zbornik radova Šestog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Vršac
Beograd : Asocijacija prostornih planera Srbije., 445-452.
https://hdl.handle.net/21.15107/rcub_gery_1289

Dobrosavljević T, Manojlović S, Gocić M, Srejić M. Mehanička vodna erozija u slivu Crnice. in Zbornik radova Šestog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Vršac. 2016;:445-452.
https://hdl.handle.net/21.15107/rcub_gery_1289 .

Dobrosavljević, Tanja, Manojlović, Sanja, Gocić, Milena, Srejić, Milan, "Mehanička vodna erozija u slivu Crnice" in Zbornik radova Šestog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Vršac (2016):445-452,
https://hdl.handle.net/21.15107/rcub_gery_1289 .

TY  - CONF
AU  - Mustafić, Sanja
AU  - Dobrosavljević, Tanja
AU  - Luković, Jelena
AU  - Manojlović, Predrag
AU  - Milošević, Marko
PY  - 2015
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1382
AB  - Soil erosion as well as sedimentation and transportation processes are complex in Serbia. The processes of erosion are
widely distributed and determined by quite favorable natural conditions. Examination of suspended sediment load transport in
Serbia is very popular recently. Frequent extreme meteorological and hydrological conditions imply permanent loss of land. In this
study, the inter-annual sediment load is examined in the Morava River Basin. Suspended load (Qs) monitoring was carried out by
Met office at 16 profiles. Identified trends were obtained using the nonparametric Mann-Kendall test. Average transport of
suspended sediment within the Morava drainage basin is ranged from 15.1 to 160.5 t/km2/year. The results of the Mann-Kendall
test showed different trends. Six stations identified a negative trend significant at 0.001, at three stations significance at 0.1, while
four stations didn’t reveal any significant result. The average negative trend in suspended sediment load is ranged from 0.03 to 7.6
t/km2/year. On the other hand, on three stations a positive trend is identified. The differences can be attributed to the impact of
climate change as well as anthropogenic factors. Increasing rainfall trend may have an impact on suspended sediment load on
specific stations. On the other hand, extensive years of erosion control measures, as well as the depopulation of rural settlements
in some parts of the basin led to reduced intensity of the erosion as well as suspended sediment load transportation.
PB  - Budapest : Hungarian Geographical society
PB  - Association of Geographical societies in Europe
C3  - Congers programme and Abstract of the Fifth EUGEO Congress on the Geography of Europe, Budapest
T1  - Suspended Sediment Transport in Serbian River
SP  - 177
UR  - https://hdl.handle.net/21.15107/rcub_gery_1382
ER  - 

@conference{
author = "Mustafić, Sanja and Dobrosavljević, Tanja and Luković, Jelena and Manojlović, Predrag and Milošević, Marko",
year = "2015",
abstract = "Soil erosion as well as sedimentation and transportation processes are complex in Serbia. The processes of erosion are
widely distributed and determined by quite favorable natural conditions. Examination of suspended sediment load transport in
Serbia is very popular recently. Frequent extreme meteorological and hydrological conditions imply permanent loss of land. In this
study, the inter-annual sediment load is examined in the Morava River Basin. Suspended load (Qs) monitoring was carried out by
Met office at 16 profiles. Identified trends were obtained using the nonparametric Mann-Kendall test. Average transport of
suspended sediment within the Morava drainage basin is ranged from 15.1 to 160.5 t/km2/year. The results of the Mann-Kendall
test showed different trends. Six stations identified a negative trend significant at 0.001, at three stations significance at 0.1, while
four stations didn’t reveal any significant result. The average negative trend in suspended sediment load is ranged from 0.03 to 7.6
t/km2/year. On the other hand, on three stations a positive trend is identified. The differences can be attributed to the impact of
climate change as well as anthropogenic factors. Increasing rainfall trend may have an impact on suspended sediment load on
specific stations. On the other hand, extensive years of erosion control measures, as well as the depopulation of rural settlements
in some parts of the basin led to reduced intensity of the erosion as well as suspended sediment load transportation.",
publisher = "Budapest : Hungarian Geographical society, Association of Geographical societies in Europe",
journal = "Congers programme and Abstract of the Fifth EUGEO Congress on the Geography of Europe, Budapest",
title = "Suspended Sediment Transport in Serbian River",
pages = "177",
url = "https://hdl.handle.net/21.15107/rcub_gery_1382"
}

Mustafić, S., Dobrosavljević, T., Luković, J., Manojlović, P.,& Milošević, M.. (2015). Suspended Sediment Transport in Serbian River. in Congers programme and Abstract of the Fifth EUGEO Congress on the Geography of Europe, Budapest
Budapest : Hungarian Geographical society., 177.
https://hdl.handle.net/21.15107/rcub_gery_1382

Mustafić S, Dobrosavljević T, Luković J, Manojlović P, Milošević M. Suspended Sediment Transport in Serbian River. in Congers programme and Abstract of the Fifth EUGEO Congress on the Geography of Europe, Budapest. 2015;:177.
https://hdl.handle.net/21.15107/rcub_gery_1382 .

Mustafić, Sanja, Dobrosavljević, Tanja, Luković, Jelena, Manojlović, Predrag, Milošević, Marko, "Suspended Sediment Transport in Serbian River" in Congers programme and Abstract of the Fifth EUGEO Congress on the Geography of Europe, Budapest (2015):177,
https://hdl.handle.net/21.15107/rcub_gery_1382 .

TY  - CONF
AU  - Mustafić, Sanja
AU  - Nikolić, Milena
AU  - Manojlović, Predrag
AU  - Dobrosavljević, Tanja
PY  - 2014
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1401
AB  - Kao globalni fenomen erozija zemljišta predstavlja važan faktor kauzalnih veza između prirodne sredine s jedne strane, i demografskih, ekonomskih i ekoloških aspekata razvoja određenog prostora sa druge strane. Osnovni karakter procesa erozije zemljišta je isti, ali intenzitet procesa je različit i zavisi od karakteristika navedenih faktora koji na datom prostoru deluju. Shodno tome, nameće se potreba proučavanja interaktivnog i multikolinearnog delovanja prirodne sredine i ljudske aktivnosti na isti. Geografska proučavanja ove problematike predstavljaju polaznu osnovu konkretizacije kauzalnih odnosa sredine u kojoj procesi erozije u većoj ili manjoj meri deluju. Na taj način geografski pristup definiše determinaciju uzroka stanja, ali i potencijalnih posledica, koje proces erozije zemljišta, izazvan prirodnim i antropogenim faktorima, inplicira na stanje i kvalitet životne sredine. Geografski pristup predstavljen je kroz četiri osnovna polazišta, a to su: kvantifikacija intenziteta mehaničke i hemijske vodne erozije; prostorno-vremenska distribucija intenziteta erozije; utvrđivanje trenda promene intenziteta erozivnog procesa; determinacija dominantnih geografskih faktora koji utiču na intenzitet erozije zemljišta.
PB  - Beograd : Asocijacija prostornih planera Srbije
PB  - Beograd : Univerzitet u Beogradu - Geografski fakultet
C3  - Zbornik radova Petog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Beograd
T1  - Integrisani geograski pristup proučavanja erozije zemljišta
SP  - 315
EP  - 320
UR  - https://hdl.handle.net/21.15107/rcub_gery_1401
ER  - 

@conference{
author = "Mustafić, Sanja and Nikolić, Milena and Manojlović, Predrag and Dobrosavljević, Tanja",
year = "2014",
abstract = "Kao globalni fenomen erozija zemljišta predstavlja važan faktor kauzalnih veza između prirodne sredine s jedne strane, i demografskih, ekonomskih i ekoloških aspekata razvoja određenog prostora sa druge strane. Osnovni karakter procesa erozije zemljišta je isti, ali intenzitet procesa je različit i zavisi od karakteristika navedenih faktora koji na datom prostoru deluju. Shodno tome, nameće se potreba proučavanja interaktivnog i multikolinearnog delovanja prirodne sredine i ljudske aktivnosti na isti. Geografska proučavanja ove problematike predstavljaju polaznu osnovu konkretizacije kauzalnih odnosa sredine u kojoj procesi erozije u većoj ili manjoj meri deluju. Na taj način geografski pristup definiše determinaciju uzroka stanja, ali i potencijalnih posledica, koje proces erozije zemljišta, izazvan prirodnim i antropogenim faktorima, inplicira na stanje i kvalitet životne sredine. Geografski pristup predstavljen je kroz četiri osnovna polazišta, a to su: kvantifikacija intenziteta mehaničke i hemijske vodne erozije; prostorno-vremenska distribucija intenziteta erozije; utvrđivanje trenda promene intenziteta erozivnog procesa; determinacija dominantnih geografskih faktora koji utiču na intenzitet erozije zemljišta.",
publisher = "Beograd : Asocijacija prostornih planera Srbije, Beograd : Univerzitet u Beogradu - Geografski fakultet",
journal = "Zbornik radova Petog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Beograd",
title = "Integrisani geograski pristup proučavanja erozije zemljišta",
pages = "315-320",
url = "https://hdl.handle.net/21.15107/rcub_gery_1401"
}

Mustafić, S., Nikolić, M., Manojlović, P.,& Dobrosavljević, T.. (2014). Integrisani geograski pristup proučavanja erozije zemljišta. in Zbornik radova Petog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Beograd
Beograd : Asocijacija prostornih planera Srbije., 315-320.
https://hdl.handle.net/21.15107/rcub_gery_1401

Mustafić S, Nikolić M, Manojlović P, Dobrosavljević T. Integrisani geograski pristup proučavanja erozije zemljišta. in Zbornik radova Petog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Beograd. 2014;:315-320.
https://hdl.handle.net/21.15107/rcub_gery_1401 .

Mustafić, Sanja, Nikolić, Milena, Manojlović, Predrag, Dobrosavljević, Tanja, "Integrisani geograski pristup proučavanja erozije zemljišta" in Zbornik radova Petog naučno-stručnog skupa sa međunarodnim učešćem "Lokalna samouprava u planiranju i uređenju prostora i naselja", Beograd (2014):315-320,
https://hdl.handle.net/21.15107/rcub_gery_1401 .

TY  - CONF
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Nikolić, Milena
AU  - Dobrosavljević, Tanja
PY  - 2014
UR  - http://gery.gef.bg.ac.rs/handle/123456789/1400
AB  - The paper is concerned with identifying changes in the time series of discharge (Q), suspended sediment concentration (SSC) and sediment load (Qs) of the Velika Morva River. The catchment area on farthest hydrological profile Ljubičevski most on Velika Morava River is approximately 35496 km2. In this profile were carried out daily measurements of flow and concentration of silt in the period 1967 to 2007. Average perennial transport of suspended sediment is 2,57*106
 t (72,4 t/km2/y) and ranged from 0,17*106 t (4,8 t/km2/y) to 10,02*106 t (282,2 t/km2/y). Trends determined for Q, SSC and Qs are statistically obtained using the non-parametric Mann-Kendall test. Results of Mann-Kendall test show that Q has a slight declining trend of annual values which do not show statistical significance. Decline in trendline SSC and Qs is a significant at a level of 0.01. Calculating the standardized regression coefficients, it was found that the relative impact of SSC on sediment load is 3.1 time higher than the impact of discharge. For the period 1967-2007 the average dicrease in sediment load at the mouth of the Velika Morava was 3,1 t/km2/y. Decrease in suspended sediment concentrations in recent period can be explained by changes in land use, negative demographic development trends (depopulation of rural areas), carrying out conservation works in the catchment and hydro-technical works in the river bed of the Velika Morava river.
PB  - Belgrade : University of Belgrade - Faculty of Geography
PB  - Novi Sad : University of Novi Sad - Faculty of Sciences, Department of Geography, Tourism and Hotel Management
C3  - Book of abstract of the Third Romanian-Bulgarian-Hungarian-Serbian Conference: Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube, Srebrno Jezero
T1  - Temporal variation of suspended sediment load in the Velika Morava River at the mouth of the Danube River for the period 1967-2007
SP  - 26
UR  - https://hdl.handle.net/21.15107/rcub_gery_1400
ER  - 

@conference{
author = "Mustafić, Sanja and Manojlović, Predrag and Nikolić, Milena and Dobrosavljević, Tanja",
year = "2014",
abstract = "The paper is concerned with identifying changes in the time series of discharge (Q), suspended sediment concentration (SSC) and sediment load (Qs) of the Velika Morva River. The catchment area on farthest hydrological profile Ljubičevski most on Velika Morava River is approximately 35496 km2. In this profile were carried out daily measurements of flow and concentration of silt in the period 1967 to 2007. Average perennial transport of suspended sediment is 2,57*106
 t (72,4 t/km2/y) and ranged from 0,17*106 t (4,8 t/km2/y) to 10,02*106 t (282,2 t/km2/y). Trends determined for Q, SSC and Qs are statistically obtained using the non-parametric Mann-Kendall test. Results of Mann-Kendall test show that Q has a slight declining trend of annual values which do not show statistical significance. Decline in trendline SSC and Qs is a significant at a level of 0.01. Calculating the standardized regression coefficients, it was found that the relative impact of SSC on sediment load is 3.1 time higher than the impact of discharge. For the period 1967-2007 the average dicrease in sediment load at the mouth of the Velika Morava was 3,1 t/km2/y. Decrease in suspended sediment concentrations in recent period can be explained by changes in land use, negative demographic development trends (depopulation of rural areas), carrying out conservation works in the catchment and hydro-technical works in the river bed of the Velika Morava river.",
publisher = "Belgrade : University of Belgrade - Faculty of Geography, Novi Sad : University of Novi Sad - Faculty of Sciences, Department of Geography, Tourism and Hotel Management",
journal = "Book of abstract of the Third Romanian-Bulgarian-Hungarian-Serbian Conference: Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube, Srebrno Jezero",
title = "Temporal variation of suspended sediment load in the Velika Morava River at the mouth of the Danube River for the period 1967-2007",
pages = "26",
url = "https://hdl.handle.net/21.15107/rcub_gery_1400"
}

Mustafić, S., Manojlović, P., Nikolić, M.,& Dobrosavljević, T.. (2014). Temporal variation of suspended sediment load in the Velika Morava River at the mouth of the Danube River for the period 1967-2007. in Book of abstract of the Third Romanian-Bulgarian-Hungarian-Serbian Conference: Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube, Srebrno Jezero
Belgrade : University of Belgrade - Faculty of Geography., 26.
https://hdl.handle.net/21.15107/rcub_gery_1400

Mustafić S, Manojlović P, Nikolić M, Dobrosavljević T. Temporal variation of suspended sediment load in the Velika Morava River at the mouth of the Danube River for the period 1967-2007. in Book of abstract of the Third Romanian-Bulgarian-Hungarian-Serbian Conference: Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube, Srebrno Jezero. 2014;:26.
https://hdl.handle.net/21.15107/rcub_gery_1400 .

Mustafić, Sanja, Manojlović, Predrag, Nikolić, Milena, Dobrosavljević, Tanja, "Temporal variation of suspended sediment load in the Velika Morava River at the mouth of the Danube River for the period 1967-2007" in Book of abstract of the Third Romanian-Bulgarian-Hungarian-Serbian Conference: Geographical Research and Cross-Border Cooperation within the Lower Basin of the Danube, Srebrno Jezero (2014):26,
https://hdl.handle.net/21.15107/rcub_gery_1400 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Đurović, Predrag
AU  - Dragićević, Slavoljub
AU  - Tošić, Radislav
AU  - Petrović, Aleksandar S.
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/633
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Našim profesorima - Povodom 90 i 80 godina života i rada
VL  - 94
IS  - 4
SP  - 2
EP  - 34
DO  - 10.2298/GSGD1404002M
UR  - https://hdl.handle.net/21.15107/rcub_gery_633
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Đurović, Predrag and Dragićević, Slavoljub and Tošić, Radislav and Petrović, Aleksandar S.",
year = "2014",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Našim profesorima - Povodom 90 i 80 godina života i rada",
volume = "94",
number = "4",
pages = "2-34",
doi = "10.2298/GSGD1404002M",
url = "https://hdl.handle.net/21.15107/rcub_gery_633"
}

Mustafić, S., Manojlović, P., Đurović, P., Dragićević, S., Tošić, R.,& Petrović, A. S.. (2014). Našim profesorima - Povodom 90 i 80 godina života i rada. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 94(4), 2-34.
https://doi.org/10.2298/GSGD1404002M
https://hdl.handle.net/21.15107/rcub_gery_633

Mustafić S, Manojlović P, Đurović P, Dragićević S, Tošić R, Petrović AS. Našim profesorima - Povodom 90 i 80 godina života i rada. in Glasnik Srpskog geografskog društva. 2014;94(4):2-34.
doi:10.2298/GSGD1404002M
https://hdl.handle.net/21.15107/rcub_gery_633 .

Mustafić, Sanja, Manojlović, Predrag, Đurović, Predrag, Dragićević, Slavoljub, Tošić, Radislav, Petrović, Aleksandar S., "Našim profesorima - Povodom 90 i 80 godina života i rada" in Glasnik Srpskog geografskog društva, 94, no. 4 (2014):2-34,
https://doi.org/10.2298/GSGD1404002M .,
https://hdl.handle.net/21.15107/rcub_gery_633 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Nikolić, Milena
AU  - Dobrosavljević, Tanja
PY  - 2014
UR  - https://gery.gef.bg.ac.rs/handle/123456789/630
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Trend of suspended sediment load in the Velika Morava River in the period 1967-2007
VL  - 94
IS  - 4
SP  - 35
EP  - 48
DO  - 10.2298/GSGD140715001M
UR  - https://hdl.handle.net/21.15107/rcub_gery_630
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Nikolić, Milena and Dobrosavljević, Tanja",
year = "2014",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Trend of suspended sediment load in the Velika Morava River in the period 1967-2007",
volume = "94",
number = "4",
pages = "35-48",
doi = "10.2298/GSGD140715001M",
url = "https://hdl.handle.net/21.15107/rcub_gery_630"
}

Mustafić, S., Manojlović, P., Nikolić, M.,& Dobrosavljević, T.. (2014). Trend of suspended sediment load in the Velika Morava River in the period 1967-2007. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 94(4), 35-48.
https://doi.org/10.2298/GSGD140715001M
https://hdl.handle.net/21.15107/rcub_gery_630

Mustafić S, Manojlović P, Nikolić M, Dobrosavljević T. Trend of suspended sediment load in the Velika Morava River in the period 1967-2007. in Glasnik Srpskog geografskog društva. 2014;94(4):35-48.
doi:10.2298/GSGD140715001M
https://hdl.handle.net/21.15107/rcub_gery_630 .

Mustafić, Sanja, Manojlović, Predrag, Nikolić, Milena, Dobrosavljević, Tanja, "Trend of suspended sediment load in the Velika Morava River in the period 1967-2007" in Glasnik Srpskog geografskog društva, 94, no. 4 (2014):35-48,
https://doi.org/10.2298/GSGD140715001M .,
https://hdl.handle.net/21.15107/rcub_gery_630 .