Advanced technologies for monitoring and environmental protection from chemical pollutants and radiation burden

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Advanced technologies for monitoring and environmental protection from chemical pollutants and radiation burden (en)
Нове технологије за мониторинг и заштиту животног окружења од штетних хемијских супстанци и радијационог оптерећења (sr)
Nove tehnologije za monitoring i zaštitu životnog okruženja od štetnih hemijskih supstanci i radijacionog opterećenja (sr_RS)
Authors

Publications

Anthropogenic Impact on Erosion Intensity: Case Study of Rural Areas of Pirot and Dimitrovgrad Municipalities, Serbia

Manojlović, Sanja; Antić, Marija; Šantić, Danica; Sibinović, Mikica; Carević, Ivana; Srejić, Tanja

(Basel : MDPI, 2018)

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 .
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17
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17

Soil erosion response to demographic and land use changes in the Nisava river basin, Serbia

Manojlović, Sanja; Antić, Marija; Sibinović, Mikica; Dragićević, Slavoljub; Novković, Ivan

(Parlar Scientific Publications, 2017)

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 .
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Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia)

Dragićević, Slavoljub; Pripuzić, Mirjana; Živković, Nenad; Novković, Ivan; Kostadinov, Stanimir; Langović, Marko; Milojković, Boban; Čvorović, Zoran

(Basel : MDPI, 2017)

TY  - JOUR
AU  - Dragićević, Slavoljub
AU  - Pripuzić, Mirjana
AU  - Živković, Nenad
AU  - Novković, Ivan
AU  - Kostadinov, Stanimir
AU  - Langović, Marko
AU  - Milojković, Boban
AU  - Čvorović, Zoran
PY  - 2017
UR  - https://gery.gef.bg.ac.rs/handle/123456789/817
AB  - The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to perform a reconstruction of the lateral migration of a 15 km length of an active meandering river during the period 1930-2016. River morphological changes were analyzed and quantified from cadastral maps and aerial photographs as well as by geodetic survey and GIS. Hydrological characteristics and extreme hydrological events were evaluated in relation to bank erosion rate. The rate of bank erosion was markedly different from the long-term studied meanders, just like in the short-term period. During the 87 years of observation (from 1930 to 2016), the length of the Kolubara River was enlarged by 3.44 km. The average migration rate of the Kolubara River for monitored meanders in the period 1930-2010 was 1.9 myear(-1), while in the period 2010-2016, the average migration rate was 3.3 myear(-1). The rate of bank erosion was more intensive across the entire short-term period than during the longer period, and the maximum annual rate of bank erosion during the period 2010-2016 varied between 0.3 and 11.5 m. It is very likely that in the period from 2010, frequent discharge variations and rapid change of its extreme values caused more intensive bank erosion. These research results will be valuable for river channel management, engineering (soft and hard engineering), and planning purposes (predicting changes in river channel form) in the Kolubara River Basin.
PB  - Basel : MDPI
T2  - Water
T1  - Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia)
VL  - 9
IS  - 10
DO  - 10.3390/w9100748
UR  - https://hdl.handle.net/21.15107/rcub_gery_817
ER  - 
@article{
author = "Dragićević, Slavoljub and Pripuzić, Mirjana and Živković, Nenad and Novković, Ivan and Kostadinov, Stanimir and Langović, Marko and Milojković, Boban and Čvorović, Zoran",
year = "2017",
abstract = "The fluvial process is characterized by an intense meandering riverbed. The aim of this study was to perform a reconstruction of the lateral migration of a 15 km length of an active meandering river during the period 1930-2016. River morphological changes were analyzed and quantified from cadastral maps and aerial photographs as well as by geodetic survey and GIS. Hydrological characteristics and extreme hydrological events were evaluated in relation to bank erosion rate. The rate of bank erosion was markedly different from the long-term studied meanders, just like in the short-term period. During the 87 years of observation (from 1930 to 2016), the length of the Kolubara River was enlarged by 3.44 km. The average migration rate of the Kolubara River for monitored meanders in the period 1930-2010 was 1.9 myear(-1), while in the period 2010-2016, the average migration rate was 3.3 myear(-1). The rate of bank erosion was more intensive across the entire short-term period than during the longer period, and the maximum annual rate of bank erosion during the period 2010-2016 varied between 0.3 and 11.5 m. It is very likely that in the period from 2010, frequent discharge variations and rapid change of its extreme values caused more intensive bank erosion. These research results will be valuable for river channel management, engineering (soft and hard engineering), and planning purposes (predicting changes in river channel form) in the Kolubara River Basin.",
publisher = "Basel : MDPI",
journal = "Water",
title = "Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia)",
volume = "9",
number = "10",
doi = "10.3390/w9100748",
url = "https://hdl.handle.net/21.15107/rcub_gery_817"
}
Dragićević, S., Pripuzić, M., Živković, N., Novković, I., Kostadinov, S., Langović, M., Milojković, B.,& Čvorović, Z.. (2017). Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia). in Water
Basel : MDPI., 9(10).
https://doi.org/10.3390/w9100748
https://hdl.handle.net/21.15107/rcub_gery_817
Dragićević S, Pripuzić M, Živković N, Novković I, Kostadinov S, Langović M, Milojković B, Čvorović Z. Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia). in Water. 2017;9(10).
doi:10.3390/w9100748
https://hdl.handle.net/21.15107/rcub_gery_817 .
Dragićević, Slavoljub, Pripuzić, Mirjana, Živković, Nenad, Novković, Ivan, Kostadinov, Stanimir, Langović, Marko, Milojković, Boban, Čvorović, Zoran, "Spatial and Temporal Variability of Bank Erosion during the Period 1930-2016: Case StudyKolubara River Basin (Serbia)" in Water, 9, no. 10 (2017),
https://doi.org/10.3390/w9100748 .,
https://hdl.handle.net/21.15107/rcub_gery_817 .
1
19
10
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Torrential flood prevention in the Kolubara river basin

Kostadinov, Stanimir; Dragićević, Slavoljub; Stefanović, Tomislav; Novković, Ivan; Petrović, Ana M.

(Science Press, Beijing, 2017)

TY  - JOUR
AU  - Kostadinov, Stanimir
AU  - Dragićević, Slavoljub
AU  - Stefanović, Tomislav
AU  - Novković, Ivan
AU  - Petrović, Ana M.
PY  - 2017
UR  - https://gery.gef.bg.ac.rs/handle/123456789/816
AB  - One of the most vulnerable parts to natural hazards in Serbia is Kolubara river basin. In the past, during the period from 1929 to 2013, 121 torrential flood events in the Kolubara river basin were recorded which show that this territory is extremely vulnerable to the torrential floods. The extreme event which occurred in May 2014 causing the catastrophic material damages and casualties was the latest and historical flood. The analysis of natural conditions in the Kolubara basin uniformly showed that this area is predisposed to a greater number of torrential floods due to its geomorphological, hydrological and land use properties. Torrential floods are closely related to the intensity and spatial distribution of erosive processes in the upper part of the Kolubara basin. The estimation of soil erosion potential is generally achieved by Erosion Potential Model (EPM). For the purposes of determining the degree of torrential properties in various water streams in the Kolubara basin, the calculation of susceptibility to torrential floods was assessed by Flash Flood Potential Index (FFPI). More than half of the basin area (57.2%) is located within the category of very weak and weak erosion (Z(sr) = 0.35), but the category of medium erosion is geospatially very common. Such a distribution of medium erosion category provides conditions for generating, i.e. production of sediment which would boost torrential properties of water streams. After the classification of the obtained FFPI values it was determined that 25% of the Kolubara basin is very susceptible to torrents and this data should be seriously taken into consideration. Based on the analyses, the best and most successful manner of defence is prevention which consists of the integrated river basin management system (integrated torrent control system) so that technical works in hydrographic networks of torrents and biological and biotechnical works on the slope of the basin would be the best solution. Permanent control of erosive and torrential processes in the river basin will be not only important for flood control but it can also protect the existing and future water reservoirs and retentions from siltation with erosion sediment which is of great significance to the water management, agriculture, energy sector, and the entire society.
PB  - Science Press, Beijing
T2  - Journal of Mountain Science
T1  - Torrential flood prevention in the Kolubara river basin
VL  - 14
IS  - 11
SP  - 2230
EP  - 2245
DO  - 10.1007/s11629-017-4575-9
UR  - https://hdl.handle.net/21.15107/rcub_gery_816
ER  - 
@article{
author = "Kostadinov, Stanimir and Dragićević, Slavoljub and Stefanović, Tomislav and Novković, Ivan and Petrović, Ana M.",
year = "2017",
abstract = "One of the most vulnerable parts to natural hazards in Serbia is Kolubara river basin. In the past, during the period from 1929 to 2013, 121 torrential flood events in the Kolubara river basin were recorded which show that this territory is extremely vulnerable to the torrential floods. The extreme event which occurred in May 2014 causing the catastrophic material damages and casualties was the latest and historical flood. The analysis of natural conditions in the Kolubara basin uniformly showed that this area is predisposed to a greater number of torrential floods due to its geomorphological, hydrological and land use properties. Torrential floods are closely related to the intensity and spatial distribution of erosive processes in the upper part of the Kolubara basin. The estimation of soil erosion potential is generally achieved by Erosion Potential Model (EPM). For the purposes of determining the degree of torrential properties in various water streams in the Kolubara basin, the calculation of susceptibility to torrential floods was assessed by Flash Flood Potential Index (FFPI). More than half of the basin area (57.2%) is located within the category of very weak and weak erosion (Z(sr) = 0.35), but the category of medium erosion is geospatially very common. Such a distribution of medium erosion category provides conditions for generating, i.e. production of sediment which would boost torrential properties of water streams. After the classification of the obtained FFPI values it was determined that 25% of the Kolubara basin is very susceptible to torrents and this data should be seriously taken into consideration. Based on the analyses, the best and most successful manner of defence is prevention which consists of the integrated river basin management system (integrated torrent control system) so that technical works in hydrographic networks of torrents and biological and biotechnical works on the slope of the basin would be the best solution. Permanent control of erosive and torrential processes in the river basin will be not only important for flood control but it can also protect the existing and future water reservoirs and retentions from siltation with erosion sediment which is of great significance to the water management, agriculture, energy sector, and the entire society.",
publisher = "Science Press, Beijing",
journal = "Journal of Mountain Science",
title = "Torrential flood prevention in the Kolubara river basin",
volume = "14",
number = "11",
pages = "2230-2245",
doi = "10.1007/s11629-017-4575-9",
url = "https://hdl.handle.net/21.15107/rcub_gery_816"
}
Kostadinov, S., Dragićević, S., Stefanović, T., Novković, I.,& Petrović, A. M.. (2017). Torrential flood prevention in the Kolubara river basin. in Journal of Mountain Science
Science Press, Beijing., 14(11), 2230-2245.
https://doi.org/10.1007/s11629-017-4575-9
https://hdl.handle.net/21.15107/rcub_gery_816
Kostadinov S, Dragićević S, Stefanović T, Novković I, Petrović AM. Torrential flood prevention in the Kolubara river basin. in Journal of Mountain Science. 2017;14(11):2230-2245.
doi:10.1007/s11629-017-4575-9
https://hdl.handle.net/21.15107/rcub_gery_816 .
Kostadinov, Stanimir, Dragićević, Slavoljub, Stefanović, Tomislav, Novković, Ivan, Petrović, Ana M., "Torrential flood prevention in the Kolubara river basin" in Journal of Mountain Science, 14, no. 11 (2017):2230-2245,
https://doi.org/10.1007/s11629-017-4575-9 .,
https://hdl.handle.net/21.15107/rcub_gery_816 .
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