TY  - JOUR
AU  - Anđelković, Aleksandar
AU  - Đeković, Vojislav
AU  - Janić, Milorad
AU  - Spalević, Velibor
AU  - Đukanović, Gordana
AU  - Nikolić, Vesna
PY  - 2020
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/1097
AB  - In this paper, floods that occurred as a result of a cyclone were analysed. The cyclone generated rainfalls of high intensity. The flood wave on the river Belica was reconstructed by recording high water levels. Through subsequent recordings of the flow profile morphology, watercourse, and riverbed reach, the dimensions of the riverbed were defined. The total station TOPCON 3100M was used as a surveying instrument. Based on the registered traces of high waters and a combined method and application of Hec-Ras software, the flow capacity of the riverbed was determined, and meter readings on the flow profile of the watercourse were registered.
PB  - Scibulcom Ltd.
T2  - Journal of Environmental Protection and Ecology
T1  - Floods on the river Belica at Jagodina, Serbia in 2014
EP  - 316
IS  - 1
SP  - 308
VL  - 21
UR  - conv_1988
ER  - 

@article{
author = "Anđelković, Aleksandar and Đeković, Vojislav and Janić, Milorad and Spalević, Velibor and Đukanović, Gordana and Nikolić, Vesna",
year = "2020",
abstract = "In this paper, floods that occurred as a result of a cyclone were analysed. The cyclone generated rainfalls of high intensity. The flood wave on the river Belica was reconstructed by recording high water levels. Through subsequent recordings of the flow profile morphology, watercourse, and riverbed reach, the dimensions of the riverbed were defined. The total station TOPCON 3100M was used as a surveying instrument. Based on the registered traces of high waters and a combined method and application of Hec-Ras software, the flow capacity of the riverbed was determined, and meter readings on the flow profile of the watercourse were registered.",
publisher = "Scibulcom Ltd.",
journal = "Journal of Environmental Protection and Ecology",
title = "Floods on the river Belica at Jagodina, Serbia in 2014",
pages = "316-308",
number = "1",
volume = "21",
url = "conv_1988"
}

Anđelković, A., Đeković, V., Janić, M., Spalević, V., Đukanović, G.,& Nikolić, V.. (2020). Floods on the river Belica at Jagodina, Serbia in 2014. in Journal of Environmental Protection and Ecology
Scibulcom Ltd.., 21(1), 308-316.
conv_1988

Anđelković A, Đeković V, Janić M, Spalević V, Đukanović G, Nikolić V. Floods on the river Belica at Jagodina, Serbia in 2014. in Journal of Environmental Protection and Ecology. 2020;21(1):308-316.
conv_1988 .

Anđelković, Aleksandar, Đeković, Vojislav, Janić, Milorad, Spalević, Velibor, Đukanović, Gordana, Nikolić, Vesna, "Floods on the river Belica at Jagodina, Serbia in 2014" in Journal of Environmental Protection and Ecology, 21, no. 1 (2020):308-316,
conv_1988 .

TY  - JOUR
AU  - Anđelković, Aleksandar
AU  - Ristić, Ratko
AU  - Janić, Milorad
AU  - Đeković, Vojislav
AU  - Živanović, Nikola
AU  - Spalević, Velibor
PY  - 2017
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/835
AB  - Soil erosion is a natural process, occurring over geological time and is essential for soil formation. The concerns about erosion are related to accelerated erosion, where the natural rate is significantly increased by human activity. Soil erosion by water is one of the greatest environmental challenges facing the Globe, being equally challenging problem for the countries of the Balkan Peninsula, changing the quantity and quality of their water resources, reducing at the same time availability and use of fresh water. Most natural watercourses are approximately balanced with respect to sediment inflow and outflow. The dam construction dramatically alters this balance since the increased flow depth and decreased flow velocity of a reservoir, reduces the sediment transport capacity and causes settling. Reservoir sedimentation is a complex process that varies with watershed sediment production, rate of transportation, and mode of deposition. The importance of watershed management in relation to the sediment management has increased, as the number of dams and their ages increase. The paper presents the research of the sediments siltation intensity of the accumulation Duboki Potok in the Barajevska River Basin in Serbia, in the period from 1991 to 2015. The survey data are based on the origin of sediment accumulation and change of the accumulation storage subsequent to the sedimentation within the section of the accumulation. The research comprised the recording of the configuration of the bottom of the lake and determination of the current state of storage capacity, using the echo-sonar 'Garmin Echo-200' and the GPS receiver 'Topcon GMS-2' for the recording of the positions. The used equipment and the measuring method show promising results. The post-processing, once the measurement is transferred into the computer-graphic environment, will simplify further monitoring of the siltation of the studied accumulation.
PB  - Scibulcom Ltd.
T2  - Journal of Environmental Protection and Ecology
T1  - Genesis of sediments and siltation of the accumulation 'Duboki Potok' of the Barajevska river basin, Serbia
EP  - 1745
IS  - 4
SP  - 1735
VL  - 18
UR  - conv_2059
ER  - 

@article{
author = "Anđelković, Aleksandar and Ristić, Ratko and Janić, Milorad and Đeković, Vojislav and Živanović, Nikola and Spalević, Velibor",
year = "2017",
abstract = "Soil erosion is a natural process, occurring over geological time and is essential for soil formation. The concerns about erosion are related to accelerated erosion, where the natural rate is significantly increased by human activity. Soil erosion by water is one of the greatest environmental challenges facing the Globe, being equally challenging problem for the countries of the Balkan Peninsula, changing the quantity and quality of their water resources, reducing at the same time availability and use of fresh water. Most natural watercourses are approximately balanced with respect to sediment inflow and outflow. The dam construction dramatically alters this balance since the increased flow depth and decreased flow velocity of a reservoir, reduces the sediment transport capacity and causes settling. Reservoir sedimentation is a complex process that varies with watershed sediment production, rate of transportation, and mode of deposition. The importance of watershed management in relation to the sediment management has increased, as the number of dams and their ages increase. The paper presents the research of the sediments siltation intensity of the accumulation Duboki Potok in the Barajevska River Basin in Serbia, in the period from 1991 to 2015. The survey data are based on the origin of sediment accumulation and change of the accumulation storage subsequent to the sedimentation within the section of the accumulation. The research comprised the recording of the configuration of the bottom of the lake and determination of the current state of storage capacity, using the echo-sonar 'Garmin Echo-200' and the GPS receiver 'Topcon GMS-2' for the recording of the positions. The used equipment and the measuring method show promising results. The post-processing, once the measurement is transferred into the computer-graphic environment, will simplify further monitoring of the siltation of the studied accumulation.",
publisher = "Scibulcom Ltd.",
journal = "Journal of Environmental Protection and Ecology",
title = "Genesis of sediments and siltation of the accumulation 'Duboki Potok' of the Barajevska river basin, Serbia",
pages = "1745-1735",
number = "4",
volume = "18",
url = "conv_2059"
}

Anđelković, A., Ristić, R., Janić, M., Đeković, V., Živanović, N.,& Spalević, V.. (2017). Genesis of sediments and siltation of the accumulation 'Duboki Potok' of the Barajevska river basin, Serbia. in Journal of Environmental Protection and Ecology
Scibulcom Ltd.., 18(4), 1735-1745.
conv_2059

Anđelković A, Ristić R, Janić M, Đeković V, Živanović N, Spalević V. Genesis of sediments and siltation of the accumulation 'Duboki Potok' of the Barajevska river basin, Serbia. in Journal of Environmental Protection and Ecology. 2017;18(4):1735-1745.
conv_2059 .

Anđelković, Aleksandar, Ristić, Ratko, Janić, Milorad, Đeković, Vojislav, Živanović, Nikola, Spalević, Velibor, "Genesis of sediments and siltation of the accumulation 'Duboki Potok' of the Barajevska river basin, Serbia" in Journal of Environmental Protection and Ecology, 18, no. 4 (2017):1735-1745,
conv_2059 .

TY  - JOUR
AU  - Vujacić, D.
AU  - Barović, G.
AU  - Đeković, Vojislav
AU  - Anđelković, Aleksandar
AU  - Khaledidarvishan, A.
AU  - Gholami, L.
AU  - Jovanović, M.
AU  - Spalević, Velibor
PY  - 2017
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/828
AB  - Sediment is a final result of erosion playing an important role in sustainable development of water resource system, controlling riverine hydrology, morphology, ecology, and water quality. A comprehensive approach estimating sediment yield from a watershed is needed to develop proper measures for mitigating sediment disasters and assessing downstream impacts. The researchers are using qualitative and quantitative methods for describing erosion through field observations and laboratory experiments. Indirect valuations of the erosion processes have been carried out using suspended sediment yield data of rivers or by assessing the sediments deposited in reservoirs. Modelling in ungauged basins has been considered as one of the main challenges in hydrological sciences. The objective of this research was to simulate responses of erosion processes in the Sheremetski Potok calculating sediment yield by using the models 'River Basin' and 'Surface and Distance'. Our findings pointed out a low potential of soil erosion risk, although in the river basin prevails very steep slopes (average river basin decline, Isr, 43.42%). With 2058 m(3) yr(-1) of sediment yield, and an area-specific sediment yield of 298 m(3) km(-2) yr(-1), the studied basin belongs to the Montenegrin basins with low sediment discharge. The model outcomes were validated through measurements at the Potpec reservoir.
PB  - Scibulcom Ltd.
T2  - Journal of Environmental Protection and Ecology
T1  - Calculation of sediment yield using the 'river basin' and 'surface and distance' models: a case study of the Sheremetski potok watershed, Montenegro
EP  - 1201
IS  - 3
SP  - 1193
VL  - 18
UR  - conv_2064
ER  - 

@article{
author = "Vujacić, D. and Barović, G. and Đeković, Vojislav and Anđelković, Aleksandar and Khaledidarvishan, A. and Gholami, L. and Jovanović, M. and Spalević, Velibor",
year = "2017",
abstract = "Sediment is a final result of erosion playing an important role in sustainable development of water resource system, controlling riverine hydrology, morphology, ecology, and water quality. A comprehensive approach estimating sediment yield from a watershed is needed to develop proper measures for mitigating sediment disasters and assessing downstream impacts. The researchers are using qualitative and quantitative methods for describing erosion through field observations and laboratory experiments. Indirect valuations of the erosion processes have been carried out using suspended sediment yield data of rivers or by assessing the sediments deposited in reservoirs. Modelling in ungauged basins has been considered as one of the main challenges in hydrological sciences. The objective of this research was to simulate responses of erosion processes in the Sheremetski Potok calculating sediment yield by using the models 'River Basin' and 'Surface and Distance'. Our findings pointed out a low potential of soil erosion risk, although in the river basin prevails very steep slopes (average river basin decline, Isr, 43.42%). With 2058 m(3) yr(-1) of sediment yield, and an area-specific sediment yield of 298 m(3) km(-2) yr(-1), the studied basin belongs to the Montenegrin basins with low sediment discharge. The model outcomes were validated through measurements at the Potpec reservoir.",
publisher = "Scibulcom Ltd.",
journal = "Journal of Environmental Protection and Ecology",
title = "Calculation of sediment yield using the 'river basin' and 'surface and distance' models: a case study of the Sheremetski potok watershed, Montenegro",
pages = "1201-1193",
number = "3",
volume = "18",
url = "conv_2064"
}

Vujacić, D., Barović, G., Đeković, V., Anđelković, A., Khaledidarvishan, A., Gholami, L., Jovanović, M.,& Spalević, V.. (2017). Calculation of sediment yield using the 'river basin' and 'surface and distance' models: a case study of the Sheremetski potok watershed, Montenegro. in Journal of Environmental Protection and Ecology
Scibulcom Ltd.., 18(3), 1193-1201.
conv_2064

Vujacić D, Barović G, Đeković V, Anđelković A, Khaledidarvishan A, Gholami L, Jovanović M, Spalević V. Calculation of sediment yield using the 'river basin' and 'surface and distance' models: a case study of the Sheremetski potok watershed, Montenegro. in Journal of Environmental Protection and Ecology. 2017;18(3):1193-1201.
conv_2064 .

Vujacić, D., Barović, G., Đeković, Vojislav, Anđelković, Aleksandar, Khaledidarvishan, A., Gholami, L., Jovanović, M., Spalević, Velibor, "Calculation of sediment yield using the 'river basin' and 'surface and distance' models: a case study of the Sheremetski potok watershed, Montenegro" in Journal of Environmental Protection and Ecology, 18, no. 3 (2017):1193-1201,
conv_2064 .

TY  - JOUR
AU  - Đeković, Vojislav
AU  - Milošević, N.
AU  - Anđelković, Aleksandar
AU  - Đurović, N.
AU  - Barović, G.
AU  - Vujacić, D.
AU  - Spalević, Velibor
PY  - 2016
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/790
AB  - The formation of a river channel stream profile in natural conditions is a long process that lasts for hundreds of years. Research at experimental sections of streams is necessary to discover the initial phases of river beds morphological development. In order to achieve this, this study focused on the period after regulatory earth works. From this initial period, the earthy regulated channel is left to the natural processes of morphological formation. This paper presents the research on morphological changes in the Pestan River (H min, 44 degrees 26'08.4" N 20 degrees 15'23.2" E) from 1978 to 2013, after the regulatory works. One of the possible reasons for permanent morphological changes is reaching the balance between transport and disposition of river sediment, and transport capacity of the stream. The experimental stream reach is located upstream from the mouth of the Pestan into the Kolubara. The goal of the research was to determine the causes of steady morphological changes of the regulated channel, from the initial phase, after the regulatory works, until today.
PB  - Scibulcom Ltd.
T2  - Journal of Environmental Protection and Ecology
T1  - Channel morphology changes in the river Pestan, Serbia
EP  - 1213
IS  - 3
SP  - 1203
VL  - 17
UR  - conv_2124
ER  - 

@article{
author = "Đeković, Vojislav and Milošević, N. and Anđelković, Aleksandar and Đurović, N. and Barović, G. and Vujacić, D. and Spalević, Velibor",
year = "2016",
abstract = "The formation of a river channel stream profile in natural conditions is a long process that lasts for hundreds of years. Research at experimental sections of streams is necessary to discover the initial phases of river beds morphological development. In order to achieve this, this study focused on the period after regulatory earth works. From this initial period, the earthy regulated channel is left to the natural processes of morphological formation. This paper presents the research on morphological changes in the Pestan River (H min, 44 degrees 26'08.4" N 20 degrees 15'23.2" E) from 1978 to 2013, after the regulatory works. One of the possible reasons for permanent morphological changes is reaching the balance between transport and disposition of river sediment, and transport capacity of the stream. The experimental stream reach is located upstream from the mouth of the Pestan into the Kolubara. The goal of the research was to determine the causes of steady morphological changes of the regulated channel, from the initial phase, after the regulatory works, until today.",
publisher = "Scibulcom Ltd.",
journal = "Journal of Environmental Protection and Ecology",
title = "Channel morphology changes in the river Pestan, Serbia",
pages = "1213-1203",
number = "3",
volume = "17",
url = "conv_2124"
}

Đeković, V., Milošević, N., Anđelković, A., Đurović, N., Barović, G., Vujacić, D.,& Spalević, V.. (2016). Channel morphology changes in the river Pestan, Serbia. in Journal of Environmental Protection and Ecology
Scibulcom Ltd.., 17(3), 1203-1213.
conv_2124

Đeković V, Milošević N, Anđelković A, Đurović N, Barović G, Vujacić D, Spalević V. Channel morphology changes in the river Pestan, Serbia. in Journal of Environmental Protection and Ecology. 2016;17(3):1203-1213.
conv_2124 .

Đeković, Vojislav, Milošević, N., Anđelković, Aleksandar, Đurović, N., Barović, G., Vujacić, D., Spalević, Velibor, "Channel morphology changes in the river Pestan, Serbia" in Journal of Environmental Protection and Ecology, 17, no. 3 (2016):1203-1213,
conv_2124 .

TY  - JOUR
AU  - Anđelković, Aleksandar
AU  - Ristić, Ratko
AU  - Janić, Milorad
AU  - Đeković, Vojislav
AU  - Živanović, Nikola
AU  - Spalević, Velibor
PY  - 2015
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/695
AB  - Soil erosion is a natural process, occurring over geological time and is essential for soil formation. The concerns about erosion are related to accelerated erosion, where the natural rate is significantly increased by human activity. Soil erosion by water is one of the greatest environmental challenges facing the Globe, being equally challenging problem for the countries of the Balkan Peninsula, changing the quantity and quality of their water resources, reducing at the same time availability and use of fresh water. Most natural watercourses are approximately balanced with respect to sediment inflow and outflow. The dam construction dramatically alters this balance since the increased flow depth and decreased flow velocity of a reservoir, reduces the sediment transport capacity and causes settling. Reservoir sedimentation is a complex process that varies with watershed sediment production, rate of transportation, and mode of deposition. The importance of watershed management in relation to the sediment management has increased, as the number of dams and their ages increase. The paper presents the research of the sediments siltation intensity of the accumulation Duboki Potok in the Barajevska River Basin in Serbia, in the period from 1991 to 2015. The survey data are based on the origin of sediment accumulation and change of the accumulation storage subsequent to the sedimentation within the section of the accumulation. The research comprised the recording of the configuration of the bottom of the lake and determination of the current state of storage capacity, using the echo-sonar ‘Garmin Echo-200’ and the GPS receiver ‘Topcon GMS-2’ for the recording of the positions. The used equipment and the measuring method show promising results. The post-processing, once the measurement is transferred into the computer-graphic environment, will simplify further monitoring of the siltation of the studied accumulation.
PB  - Gebruder Borntraeger Verlagsbuchhandlung
T2  - European Journal of Mineralogy
T1  - Genesis of sediments and siltation of the accumulation ⇘duboki potok⇔ of the barajevska river basin, serbia
EP  - 1745
IS  - 2
SP  - 1735
VL  - 27
UR  - conv_2075
ER  - 

@article{
author = "Anđelković, Aleksandar and Ristić, Ratko and Janić, Milorad and Đeković, Vojislav and Živanović, Nikola and Spalević, Velibor",
year = "2015",
abstract = "Soil erosion is a natural process, occurring over geological time and is essential for soil formation. The concerns about erosion are related to accelerated erosion, where the natural rate is significantly increased by human activity. Soil erosion by water is one of the greatest environmental challenges facing the Globe, being equally challenging problem for the countries of the Balkan Peninsula, changing the quantity and quality of their water resources, reducing at the same time availability and use of fresh water. Most natural watercourses are approximately balanced with respect to sediment inflow and outflow. The dam construction dramatically alters this balance since the increased flow depth and decreased flow velocity of a reservoir, reduces the sediment transport capacity and causes settling. Reservoir sedimentation is a complex process that varies with watershed sediment production, rate of transportation, and mode of deposition. The importance of watershed management in relation to the sediment management has increased, as the number of dams and their ages increase. The paper presents the research of the sediments siltation intensity of the accumulation Duboki Potok in the Barajevska River Basin in Serbia, in the period from 1991 to 2015. The survey data are based on the origin of sediment accumulation and change of the accumulation storage subsequent to the sedimentation within the section of the accumulation. The research comprised the recording of the configuration of the bottom of the lake and determination of the current state of storage capacity, using the echo-sonar ‘Garmin Echo-200’ and the GPS receiver ‘Topcon GMS-2’ for the recording of the positions. The used equipment and the measuring method show promising results. The post-processing, once the measurement is transferred into the computer-graphic environment, will simplify further monitoring of the siltation of the studied accumulation.",
publisher = "Gebruder Borntraeger Verlagsbuchhandlung",
journal = "European Journal of Mineralogy",
title = "Genesis of sediments and siltation of the accumulation ⇘duboki potok⇔ of the barajevska river basin, serbia",
pages = "1745-1735",
number = "2",
volume = "27",
url = "conv_2075"
}

Anđelković, A., Ristić, R., Janić, M., Đeković, V., Živanović, N.,& Spalević, V.. (2015). Genesis of sediments and siltation of the accumulation ⇘duboki potok⇔ of the barajevska river basin, serbia. in European Journal of Mineralogy
Gebruder Borntraeger Verlagsbuchhandlung., 27(2), 1735-1745.
conv_2075

Anđelković A, Ristić R, Janić M, Đeković V, Živanović N, Spalević V. Genesis of sediments and siltation of the accumulation ⇘duboki potok⇔ of the barajevska river basin, serbia. in European Journal of Mineralogy. 2015;27(2):1735-1745.
conv_2075 .

Anđelković, Aleksandar, Ristić, Ratko, Janić, Milorad, Đeković, Vojislav, Živanović, Nikola, Spalević, Velibor, "Genesis of sediments and siltation of the accumulation ⇘duboki potok⇔ of the barajevska river basin, serbia" in European Journal of Mineralogy, 27, no. 2 (2015):1735-1745,
conv_2075 .

TY  - JOUR
AU  - Annys, Klaas
AU  - Frankl, Amaury
AU  - Spalević, Velibor
AU  - Čurović, Milić
AU  - Borota, Dragan
AU  - Nyssen, Jan
PY  - 2014
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/565
AB  - The geomorphological map of the northeastern Durmitor Mountains and the plateau Jezerska Povrs. (1: 10,000, 47 km(2), Montenegro, Dinaric Alps) was prepared from an intensive fieldwork campaign and remote sensing analysis, and was compiled within a GIS. The basic components of the legend are (i) processes/genesis, (ii) materials, (iii) morphometry/morphography, (iv) hydrography, (v) vegetation and (vi) anthropogenic features. The geomorphological setting of the area consists of Mesozoic limestones which are physically deformed by Quaternary glacial and periglacial activity and chemically affected during interglacials. Glacial deposits on the plateau of three middle-to-late Pleistocene glacial phases are intersected by a well-developed network of palaeo meltwater channels. In the mountains, Holocene glacier retreat left behind a series of well-preserved recessional moraines. The map serves as a valuable tool for Quaternary research in the Durmitor Mountains, and also in other mountains of the Western Balkans.
T2  - Journal of Maps
T1  - Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Povrs (Montenegro)
EP  - 611
IS  - 4
SP  - 600
VL  - 10
DO  - 10.1080/17445647.2014.909338
UR  - conv_1116
ER  - 

@article{
author = "Annys, Klaas and Frankl, Amaury and Spalević, Velibor and Čurović, Milić and Borota, Dragan and Nyssen, Jan",
year = "2014",
abstract = "The geomorphological map of the northeastern Durmitor Mountains and the plateau Jezerska Povrs. (1: 10,000, 47 km(2), Montenegro, Dinaric Alps) was prepared from an intensive fieldwork campaign and remote sensing analysis, and was compiled within a GIS. The basic components of the legend are (i) processes/genesis, (ii) materials, (iii) morphometry/morphography, (iv) hydrography, (v) vegetation and (vi) anthropogenic features. The geomorphological setting of the area consists of Mesozoic limestones which are physically deformed by Quaternary glacial and periglacial activity and chemically affected during interglacials. Glacial deposits on the plateau of three middle-to-late Pleistocene glacial phases are intersected by a well-developed network of palaeo meltwater channels. In the mountains, Holocene glacier retreat left behind a series of well-preserved recessional moraines. The map serves as a valuable tool for Quaternary research in the Durmitor Mountains, and also in other mountains of the Western Balkans.",
journal = "Journal of Maps",
title = "Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Povrs (Montenegro)",
pages = "611-600",
number = "4",
volume = "10",
doi = "10.1080/17445647.2014.909338",
url = "conv_1116"
}

Annys, K., Frankl, A., Spalević, V., Čurović, M., Borota, D.,& Nyssen, J.. (2014). Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Povrs (Montenegro). in Journal of Maps, 10(4), 600-611.
https://doi.org/10.1080/17445647.2014.909338
conv_1116

Annys K, Frankl A, Spalević V, Čurović M, Borota D, Nyssen J. Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Povrs (Montenegro). in Journal of Maps. 2014;10(4):600-611.
doi:10.1080/17445647.2014.909338
conv_1116 .

Annys, Klaas, Frankl, Amaury, Spalević, Velibor, Čurović, Milić, Borota, Dragan, Nyssen, Jan, "Geomorphology of the Durmitor Mountains and surrounding plateau Jezerska Povrs (Montenegro)" in Journal of Maps, 10, no. 4 (2014):600-611,
https://doi.org/10.1080/17445647.2014.909338 .,
conv_1116 .

TY  - JOUR
AU  - Čurović, Milić
AU  - Medarević, Milan
AU  - Pantić, Damjan
AU  - Spalević, Velibor
PY  - 2011
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/392
AB  - The aim of this research was to identify characteristics of the three-dominant mixed forests of beech, fir and spruce (Piceeto-Abieti-Fagetum s. lat.) in Montenegro. Basic ecological, structural and production research was first analyzed and evaluated to define the multi-disciplinary character of the forests. Forest types recognizable from these basic characteristics were then defined as follows: (i) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum vaccinetosum s. lat.) on calcocambisol on limestone (Vukodol site): (ii) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum s. lat.) on acid cambisol on an eruptive base (Sula site); (iii) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum typicum s. lat.) on calcocambisol on an eruptive base of virgin forest structure (Biogradska gora). With these results an ecological based forest characterisation is available for forest planning and management.
T2  - Austrian Journal of Forest Science
T1  - Major types of mixed forests of spruce, fir and beech in Montenegro
EP  - 111
IS  - 2
SP  - 93
VL  - 128
UR  - conv_2100
ER  - 

@article{
author = "Čurović, Milić and Medarević, Milan and Pantić, Damjan and Spalević, Velibor",
year = "2011",
abstract = "The aim of this research was to identify characteristics of the three-dominant mixed forests of beech, fir and spruce (Piceeto-Abieti-Fagetum s. lat.) in Montenegro. Basic ecological, structural and production research was first analyzed and evaluated to define the multi-disciplinary character of the forests. Forest types recognizable from these basic characteristics were then defined as follows: (i) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum vaccinetosum s. lat.) on calcocambisol on limestone (Vukodol site): (ii) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum s. lat.) on acid cambisol on an eruptive base (Sula site); (iii) Mixed beech, fir and spruce forest (Piceeto-Abieti-Fagetum typicum s. lat.) on calcocambisol on an eruptive base of virgin forest structure (Biogradska gora). With these results an ecological based forest characterisation is available for forest planning and management.",
journal = "Austrian Journal of Forest Science",
title = "Major types of mixed forests of spruce, fir and beech in Montenegro",
pages = "111-93",
number = "2",
volume = "128",
url = "conv_2100"
}

Čurović, M., Medarević, M., Pantić, D.,& Spalević, V.. (2011). Major types of mixed forests of spruce, fir and beech in Montenegro. in Austrian Journal of Forest Science, 128(2), 93-111.
conv_2100

Čurović M, Medarević M, Pantić D, Spalević V. Major types of mixed forests of spruce, fir and beech in Montenegro. in Austrian Journal of Forest Science. 2011;128(2):93-111.
conv_2100 .

Čurović, Milić, Medarević, Milan, Pantić, Damjan, Spalević, Velibor, "Major types of mixed forests of spruce, fir and beech in Montenegro" in Austrian Journal of Forest Science, 128, no. 2 (2011):93-111,
conv_2100 .

TY  - JOUR
AU  - Čurović, Milić
AU  - Stesević, Danijela
AU  - Medarević, Milan
AU  - Cvjetićanin, Rade
AU  - Pantić, Damjan
AU  - Spalević, Velibor
PY  - 2011
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/406
AB  - Due to their extraordinary diversity and high level of conservation, the forest ecosystems of Biogradska Gora undoubtedly fall under the most significant forest objects. Owing to the lack of anthropogenic impacts, it is an especially interesting and gratifying research subject for different experts and scientists. In order to implement a sufficiently high biodiversity level management, it is necessary to know the structural characteristics of untouched forests. In this paper we focused our attention on monodominant montane beech forests with their ecological and structural characteristics, as a bioecological basis for environmentally friendly planning and sustainable management of these and similar forest ecosystems.
PB  - Srpsko biološko društvo, Beograd, i dr.
T2  - Archives of Biological Sciences
T1  - Ecological and structural characteristics of monodominant montane beech forests in the national park Biogradska gora, Montenegro
EP  - 440
IS  - 2
SP  - 429
VL  - 63
DO  - 10.2298/ABS1102429C
UR  - conv_965
ER  - 

@article{
author = "Čurović, Milić and Stesević, Danijela and Medarević, Milan and Cvjetićanin, Rade and Pantić, Damjan and Spalević, Velibor",
year = "2011",
abstract = "Due to their extraordinary diversity and high level of conservation, the forest ecosystems of Biogradska Gora undoubtedly fall under the most significant forest objects. Owing to the lack of anthropogenic impacts, it is an especially interesting and gratifying research subject for different experts and scientists. In order to implement a sufficiently high biodiversity level management, it is necessary to know the structural characteristics of untouched forests. In this paper we focused our attention on monodominant montane beech forests with their ecological and structural characteristics, as a bioecological basis for environmentally friendly planning and sustainable management of these and similar forest ecosystems.",
publisher = "Srpsko biološko društvo, Beograd, i dr.",
journal = "Archives of Biological Sciences",
title = "Ecological and structural characteristics of monodominant montane beech forests in the national park Biogradska gora, Montenegro",
pages = "440-429",
number = "2",
volume = "63",
doi = "10.2298/ABS1102429C",
url = "conv_965"
}

Čurović, M., Stesević, D., Medarević, M., Cvjetićanin, R., Pantić, D.,& Spalević, V.. (2011). Ecological and structural characteristics of monodominant montane beech forests in the national park Biogradska gora, Montenegro. in Archives of Biological Sciences
Srpsko biološko društvo, Beograd, i dr.., 63(2), 429-440.
https://doi.org/10.2298/ABS1102429C
conv_965

Čurović M, Stesević D, Medarević M, Cvjetićanin R, Pantić D, Spalević V. Ecological and structural characteristics of monodominant montane beech forests in the national park Biogradska gora, Montenegro. in Archives of Biological Sciences. 2011;63(2):429-440.
doi:10.2298/ABS1102429C
conv_965 .

Čurović, Milić, Stesević, Danijela, Medarević, Milan, Cvjetićanin, Rade, Pantić, Damjan, Spalević, Velibor, "Ecological and structural characteristics of monodominant montane beech forests in the national park Biogradska gora, Montenegro" in Archives of Biological Sciences, 63, no. 2 (2011):429-440,
https://doi.org/10.2298/ABS1102429C .,
conv_965 .

TY  - JOUR
AU  - Ristić, Ratko
AU  - Kostadinov, Stanimir
AU  - Malošević, Dragan
AU  - Spalević, Velibor
PY  - 2001
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/92
AB  - Proračun velikih voda određene verovatnoće pojave Qmax(% ), na bujičnim slivovima, obavlja se uglavnom primenom teorije sintetičkog jediničnog hidrograma (proračun vršne ordinate sintetičkog jediničnog hidrograma qmax) i SCS metodologije (za razdvajanje efektivnih Pe od ukupnih padavina Pb). Proračun efektivnih padavina zahteva determinisanje broja krive oticaja CN, koji se određuje na osnovu hidrološke klase zemljišta, opštih hidroloških uslova, a u zavisnosti od načina korišćenja zemljišta. Neodgovarajuća procena hidroloških uslova, pogotovo na teren­ima sa razvijenim erozionim procesima, vodi ka sukcesivnim greškama, na liniji: broj krive oticaja CN→ deficit vlage u zemljištu d→ efektivna kiša Pe→ maksimalan proticaj Qmax. Adekvatna primena procedure, u proceni broja krive oticaja CN, prikazana je na primeru sliva reke Onjeg (sliv Kolubare), do profila Brajkovac.
AB  - Computation of maximal discharge Qmax(%), on torrential catchment areas, is carried out, usually, by synthetic unit hydrograph (maximal ordinate of synthetic unit hydrograph) and SCS method (deriving of effective rainfall Pe from total precipitation Pb). Calculation of effective rainfall is based on determination of runoff curve number CN. Runoff curve number depends on: hydrologic soil group; hydrologic conditions; land use. Erroneous estimations of hydrologic group of soil and hydrologic conditions, especially on the terrain with developed erosion processes, lead to successive errors: runoff curve number CN→ potential maximum retention d→ effective rainfall Pe→ maximal discharge Qmax. Adequate procedure for estimation of runoff curve number CN was applied in the experimental catchments area of river Onjeg (subcatchment of the Kolubara river system), at the profile Brajkovac. .
PB  - Unija bioloških naučnih društava Jugoslavije, Beograd
T2  - Zemljište i biljka
T1  - Erozionistički aspekt u proceni hidrološke klase zemljišta i determinisanja broja krive oticaja CN
T1  - Erosion aspect in estimation of hydrologic soil group and determination of runoff curve number CN
EP  - 174
IS  - 3
SP  - 165
VL  - 50
UR  - conv_663
ER  - 

@article{
author = "Ristić, Ratko and Kostadinov, Stanimir and Malošević, Dragan and Spalević, Velibor",
year = "2001",
abstract = "Proračun velikih voda određene verovatnoće pojave Qmax(% ), na bujičnim slivovima, obavlja se uglavnom primenom teorije sintetičkog jediničnog hidrograma (proračun vršne ordinate sintetičkog jediničnog hidrograma qmax) i SCS metodologije (za razdvajanje efektivnih Pe od ukupnih padavina Pb). Proračun efektivnih padavina zahteva determinisanje broja krive oticaja CN, koji se određuje na osnovu hidrološke klase zemljišta, opštih hidroloških uslova, a u zavisnosti od načina korišćenja zemljišta. Neodgovarajuća procena hidroloških uslova, pogotovo na teren­ima sa razvijenim erozionim procesima, vodi ka sukcesivnim greškama, na liniji: broj krive oticaja CN→ deficit vlage u zemljištu d→ efektivna kiša Pe→ maksimalan proticaj Qmax. Adekvatna primena procedure, u proceni broja krive oticaja CN, prikazana je na primeru sliva reke Onjeg (sliv Kolubare), do profila Brajkovac., Computation of maximal discharge Qmax(%), on torrential catchment areas, is carried out, usually, by synthetic unit hydrograph (maximal ordinate of synthetic unit hydrograph) and SCS method (deriving of effective rainfall Pe from total precipitation Pb). Calculation of effective rainfall is based on determination of runoff curve number CN. Runoff curve number depends on: hydrologic soil group; hydrologic conditions; land use. Erroneous estimations of hydrologic group of soil and hydrologic conditions, especially on the terrain with developed erosion processes, lead to successive errors: runoff curve number CN→ potential maximum retention d→ effective rainfall Pe→ maximal discharge Qmax. Adequate procedure for estimation of runoff curve number CN was applied in the experimental catchments area of river Onjeg (subcatchment of the Kolubara river system), at the profile Brajkovac. .",
publisher = "Unija bioloških naučnih društava Jugoslavije, Beograd",
journal = "Zemljište i biljka",
title = "Erozionistički aspekt u proceni hidrološke klase zemljišta i determinisanja broja krive oticaja CN, Erosion aspect in estimation of hydrologic soil group and determination of runoff curve number CN",
pages = "174-165",
number = "3",
volume = "50",
url = "conv_663"
}

Ristić, R., Kostadinov, S., Malošević, D.,& Spalević, V.. (2001). Erozionistički aspekt u proceni hidrološke klase zemljišta i determinisanja broja krive oticaja CN. in Zemljište i biljka
Unija bioloških naučnih društava Jugoslavije, Beograd., 50(3), 165-174.
conv_663

Ristić R, Kostadinov S, Malošević D, Spalević V. Erozionistički aspekt u proceni hidrološke klase zemljišta i determinisanja broja krive oticaja CN. in Zemljište i biljka. 2001;50(3):165-174.
conv_663 .

Ristić, Ratko, Kostadinov, Stanimir, Malošević, Dragan, Spalević, Velibor, "Erozionistički aspekt u proceni hidrološke klase zemljišta i determinisanja broja krive oticaja CN" in Zemljište i biljka, 50, no. 3 (2001):165-174,
conv_663 .