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  - 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 .

TY  - JOUR
AU  - Bajat, Branislav
AU  - Pejović, Milutin
AU  - Luković, Jelena
AU  - Manojlović, Predrag
AU  - Ducić, Vladan
AU  - Mustafić, Sanja
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/560
AB  - The appearence of geostatistics and geographical information systems has made it possible to analyze complex spatial patterns of meteorological elements over large areas in the applied climatology. The objective of this study is to use geostatistics to characterize the spatial structure and map the spatial variation of average values of precipitation for a 30-year period in Serbia. New, recently introduced, geostatistical algorithms facilitate utilization of auxiliary variables especially remote sensing data or freely available global datasets. The data from Advanced Spaceborn Thermal Emission and Reflection Radiometer global digital elevation model are incorporated as ancillary variables into spatial prediction of average annual precipitation using geostatistical method known as regression kriging. The R (2) value of 0.842 proves high performance result of the prediction of the proposed method.
PB  - Springer Wien, Wien
T2  - Theoretical and Applied Climatology
T1  - Mapping average annual precipitation in Serbia (1961-1990) by using regression kriging
VL  - 112
IS  - 1-2
SP  - 1
EP  - 13
DO  - 10.1007/s00704-012-0702-2
UR  - https://hdl.handle.net/21.15107/rcub_gery_560
ER  - 

@article{
author = "Bajat, Branislav and Pejović, Milutin and Luković, Jelena and Manojlović, Predrag and Ducić, Vladan and Mustafić, Sanja",
year = "2013",
abstract = "The appearence of geostatistics and geographical information systems has made it possible to analyze complex spatial patterns of meteorological elements over large areas in the applied climatology. The objective of this study is to use geostatistics to characterize the spatial structure and map the spatial variation of average values of precipitation for a 30-year period in Serbia. New, recently introduced, geostatistical algorithms facilitate utilization of auxiliary variables especially remote sensing data or freely available global datasets. The data from Advanced Spaceborn Thermal Emission and Reflection Radiometer global digital elevation model are incorporated as ancillary variables into spatial prediction of average annual precipitation using geostatistical method known as regression kriging. The R (2) value of 0.842 proves high performance result of the prediction of the proposed method.",
publisher = "Springer Wien, Wien",
journal = "Theoretical and Applied Climatology",
title = "Mapping average annual precipitation in Serbia (1961-1990) by using regression kriging",
volume = "112",
number = "1-2",
pages = "1-13",
doi = "10.1007/s00704-012-0702-2",
url = "https://hdl.handle.net/21.15107/rcub_gery_560"
}

Bajat, B., Pejović, M., Luković, J., Manojlović, P., Ducić, V.,& Mustafić, S.. (2013). Mapping average annual precipitation in Serbia (1961-1990) by using regression kriging. in Theoretical and Applied Climatology
Springer Wien, Wien., 112(1-2), 1-13.
https://doi.org/10.1007/s00704-012-0702-2
https://hdl.handle.net/21.15107/rcub_gery_560

Bajat B, Pejović M, Luković J, Manojlović P, Ducić V, Mustafić S. Mapping average annual precipitation in Serbia (1961-1990) by using regression kriging. in Theoretical and Applied Climatology. 2013;112(1-2):1-13.
doi:10.1007/s00704-012-0702-2
https://hdl.handle.net/21.15107/rcub_gery_560 .

Bajat, Branislav, Pejović, Milutin, Luković, Jelena, Manojlović, Predrag, Ducić, Vladan, Mustafić, Sanja, "Mapping average annual precipitation in Serbia (1961-1990) by using regression kriging" in Theoretical and Applied Climatology, 112, no. 1-2 (2013):1-13,
https://doi.org/10.1007/s00704-012-0702-2 .,
https://hdl.handle.net/21.15107/rcub_gery_560 .

TY  - CHAP
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Milošević, Marko V.
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/595
AB  - In the last decade several major floods have been registered on the territory of Serbia. The floods that affected the Nišava River Basin in spring 2010 have been the most severe in the last 50 years. During 2010 daily measurements of suspended sediment were carried out at the last hydrologic profile of Niš along the river. In the study period, mean annual specific runoff was 12.3 L s-1 km-2 and mean annual suspended load concentration was 0.1272 g L-1. A maximum mean monthly concentration of suspended load of 0.3806 g L-1 was recorded in May, when the mean monthly specific runoff was 24 L s-1 km2, and minimum 0.0118 g L-1 in September (2.7 L s-1 km-2). Total suspended load transport was 475,792.2 t (specific yield, 122.9 t km-2 year-1). The suspended transport over the year was 2.1 times higher than the average for the period of 50 years. Out of total annual sediment, 90.7% was moved in the period February to May. On a monthly level, the highest transport was observed in May (31% of the annual transport).
PB  - Springer Netherlands
T2  - Geomorphological Impacts of Extreme Weather: Case Studies From Central and Eastern Europe
T1  - Extreme erosion rates in the Nišava River Basin (eastern Serbia) in 2010
SP  - 171
EP  - 187
DO  - 10.1007/978-94-007-6301-2_11
UR  - https://hdl.handle.net/21.15107/rcub_gery_595
ER  - 

@inbook{
author = "Mustafić, Sanja and Manojlović, Predrag and Milošević, Marko V.",
year = "2013",
abstract = "In the last decade several major floods have been registered on the territory of Serbia. The floods that affected the Nišava River Basin in spring 2010 have been the most severe in the last 50 years. During 2010 daily measurements of suspended sediment were carried out at the last hydrologic profile of Niš along the river. In the study period, mean annual specific runoff was 12.3 L s-1 km-2 and mean annual suspended load concentration was 0.1272 g L-1. A maximum mean monthly concentration of suspended load of 0.3806 g L-1 was recorded in May, when the mean monthly specific runoff was 24 L s-1 km2, and minimum 0.0118 g L-1 in September (2.7 L s-1 km-2). Total suspended load transport was 475,792.2 t (specific yield, 122.9 t km-2 year-1). The suspended transport over the year was 2.1 times higher than the average for the period of 50 years. Out of total annual sediment, 90.7% was moved in the period February to May. On a monthly level, the highest transport was observed in May (31% of the annual transport).",
publisher = "Springer Netherlands",
journal = "Geomorphological Impacts of Extreme Weather: Case Studies From Central and Eastern Europe",
booktitle = "Extreme erosion rates in the Nišava River Basin (eastern Serbia) in 2010",
pages = "171-187",
doi = "10.1007/978-94-007-6301-2_11",
url = "https://hdl.handle.net/21.15107/rcub_gery_595"
}

Mustafić, S., Manojlović, P.,& Milošević, M. V.. (2013). Extreme erosion rates in the Nišava River Basin (eastern Serbia) in 2010. in Geomorphological Impacts of Extreme Weather: Case Studies From Central and Eastern Europe
Springer Netherlands., 171-187.
https://doi.org/10.1007/978-94-007-6301-2_11
https://hdl.handle.net/21.15107/rcub_gery_595

Mustafić S, Manojlović P, Milošević MV. Extreme erosion rates in the Nišava River Basin (eastern Serbia) in 2010. in Geomorphological Impacts of Extreme Weather: Case Studies From Central and Eastern Europe. 2013;:171-187.
doi:10.1007/978-94-007-6301-2_11
https://hdl.handle.net/21.15107/rcub_gery_595 .

Mustafić, Sanja, Manojlović, Predrag, Milošević, Marko V., "Extreme erosion rates in the Nišava River Basin (eastern Serbia) in 2010" in Geomorphological Impacts of Extreme Weather: Case Studies From Central and Eastern Europe (2013):171-187,
https://doi.org/10.1007/978-94-007-6301-2_11 .,
https://hdl.handle.net/21.15107/rcub_gery_595 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Kostić, Predrag
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/586
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Dynamics of suspended sediment load in the upper part of the Rasina River Basin in 2010
VL  - 93
IS  - 4
SP  - 23
EP  - 40
DO  - 10.2298/GSGD1304023M
UR  - https://hdl.handle.net/21.15107/rcub_gery_586
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Kostić, Predrag",
year = "2013",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Dynamics of suspended sediment load in the upper part of the Rasina River Basin in 2010",
volume = "93",
number = "4",
pages = "23-40",
doi = "10.2298/GSGD1304023M",
url = "https://hdl.handle.net/21.15107/rcub_gery_586"
}

Mustafić, S., Manojlović, P.,& Kostić, P.. (2013). Dynamics of suspended sediment load in the upper part of the Rasina River Basin in 2010. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 93(4), 23-40.
https://doi.org/10.2298/GSGD1304023M
https://hdl.handle.net/21.15107/rcub_gery_586

Mustafić S, Manojlović P, Kostić P. Dynamics of suspended sediment load in the upper part of the Rasina River Basin in 2010. in Glasnik Srpskog geografskog društva. 2013;93(4):23-40.
doi:10.2298/GSGD1304023M
https://hdl.handle.net/21.15107/rcub_gery_586 .

Mustafić, Sanja, Manojlović, Predrag, Kostić, Predrag, "Dynamics of suspended sediment load in the upper part of the Rasina River Basin in 2010" in Glasnik Srpskog geografskog društva, 93, no. 4 (2013):23-40,
https://doi.org/10.2298/GSGD1304023M .,
https://hdl.handle.net/21.15107/rcub_gery_586 .

TY  - JOUR
AU  - Manojlović, Predrag
AU  - Srejić, Milan
AU  - Đokić, Ivan
AU  - Mustafić, Sanja
AU  - Dobrosavljević, Tanja
PY  - 2013
UR  - https://gery.gef.bg.ac.rs/handle/123456789/552
AB  - The Rasina River Basin is located on the territory of Central Serbia. The aim of this paper is to determine the amount and spatial distribution of water resources, that is, to establish the participation of altitudinal zones in the formation of the total runoff in the Rasina River Basin area upstream from the 'Ćelije' reservoir. In terms of methodology, determination of water volume is based on four separated petrological-hydrological complexes. Average weighted specific runoff in a given territory is 9 l/s/km2. Metamorphites and magmatites are in the first place per participation in the total water runoff of 42.8 %. The second place belongs to sedimentary rocks that make 39.6 % of the total runoff . Unbound sediments participate in the total runoff value with 10.5 % and limestone with 7.1%.
AB  - Sliv reke Rasine nalazi na teritoriji centralne Srbije. Cilj ovog rada je da se na prostoru sliva Rasine uzvodno od akumulacije 'Ćelije' utvrdi količina i prostorna distribucija vodnih kapaciteta, odnosno da se ustanovi učešće visinskih zona u formiranju ukupnog oticaja. U metodološkom smislu utvrđivanje vodnosti bazirano je preko četiri izdvojena petrološko-hidrološka kompleksa. Prosečni ponderisani specifični oticaj na datoj teritoriji iznosi 9 l/s/km2. Na prvom mestu po učešću u ukupnom oticanju voda 42,8 %, imaju metamorfiti i magmatiti. Drugo mesto pripada sedimentnim stenama koje sa 39,6 % čine deo ukupnog oticaja. Nevezani sedimenti učestvuju u ukupnoj vrednosti oticaja sa 10,5 %, a krečnjaci sa 7,1%.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Altitudinal zonation of runoff in the Rasina River Basin
T1  - Visinsko zoniranje voda u slivu Rasine
VL  - 93
IS  - 2
SP  - 41
EP  - 54
DO  - 10.2298/GSGD1302041M
UR  - https://hdl.handle.net/21.15107/rcub_gery_552
ER  - 

@article{
author = "Manojlović, Predrag and Srejić, Milan and Đokić, Ivan and Mustafić, Sanja and Dobrosavljević, Tanja",
year = "2013",
abstract = "The Rasina River Basin is located on the territory of Central Serbia. The aim of this paper is to determine the amount and spatial distribution of water resources, that is, to establish the participation of altitudinal zones in the formation of the total runoff in the Rasina River Basin area upstream from the 'Ćelije' reservoir. In terms of methodology, determination of water volume is based on four separated petrological-hydrological complexes. Average weighted specific runoff in a given territory is 9 l/s/km2. Metamorphites and magmatites are in the first place per participation in the total water runoff of 42.8 %. The second place belongs to sedimentary rocks that make 39.6 % of the total runoff . Unbound sediments participate in the total runoff value with 10.5 % and limestone with 7.1%., Sliv reke Rasine nalazi na teritoriji centralne Srbije. Cilj ovog rada je da se na prostoru sliva Rasine uzvodno od akumulacije 'Ćelije' utvrdi količina i prostorna distribucija vodnih kapaciteta, odnosno da se ustanovi učešće visinskih zona u formiranju ukupnog oticaja. U metodološkom smislu utvrđivanje vodnosti bazirano je preko četiri izdvojena petrološko-hidrološka kompleksa. Prosečni ponderisani specifični oticaj na datoj teritoriji iznosi 9 l/s/km2. Na prvom mestu po učešću u ukupnom oticanju voda 42,8 %, imaju metamorfiti i magmatiti. Drugo mesto pripada sedimentnim stenama koje sa 39,6 % čine deo ukupnog oticaja. Nevezani sedimenti učestvuju u ukupnoj vrednosti oticaja sa 10,5 %, a krečnjaci sa 7,1%.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Altitudinal zonation of runoff in the Rasina River Basin, Visinsko zoniranje voda u slivu Rasine",
volume = "93",
number = "2",
pages = "41-54",
doi = "10.2298/GSGD1302041M",
url = "https://hdl.handle.net/21.15107/rcub_gery_552"
}

Manojlović, P., Srejić, M., Đokić, I., Mustafić, S.,& Dobrosavljević, T.. (2013). Altitudinal zonation of runoff in the Rasina River Basin. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 93(2), 41-54.
https://doi.org/10.2298/GSGD1302041M
https://hdl.handle.net/21.15107/rcub_gery_552

Manojlović P, Srejić M, Đokić I, Mustafić S, Dobrosavljević T. Altitudinal zonation of runoff in the Rasina River Basin. in Glasnik Srpskog geografskog društva. 2013;93(2):41-54.
doi:10.2298/GSGD1302041M
https://hdl.handle.net/21.15107/rcub_gery_552 .

Manojlović, Predrag, Srejić, Milan, Đokić, Ivan, Mustafić, Sanja, Dobrosavljević, Tanja, "Altitudinal zonation of runoff in the Rasina River Basin" in Glasnik Srpskog geografskog društva, 93, no. 2 (2013):41-54,
https://doi.org/10.2298/GSGD1302041M .,
https://hdl.handle.net/21.15107/rcub_gery_552 .

TY  - JOUR
AU  - Manojlović, Predrag
AU  - Mustafić, Sanja
AU  - Mladenović, Ben
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/474
AB  - In the hydrological year of 2001/2002, the water samples in the Mlava Basin were analyzed. On its most downstream hydrometric profile, to the Bratinac profile, the water samples were taken every 5 days for TDS an d every day for concentration suspend sediment. It was found that during the analyzed period, the transport of chemically dissolved maters was 2 times higher than the silt deposit transport.
AB  - U hidrološkoj 2001/2002. godini analizirani su uzorci vode u slivu Mlave na hidrološkom profilu Bratinac Na njenom najnizvodnijem hidrološkom profilu, do profila Bratinac, uzorci vode uzimani su na svakih 5 dana za utvrđivanje rastvorenih mineralnih materija i svakodnevno za utvrđivanje koncentracije slita. Utvrđeno je da je tokom analiziranog perioda pronos hemijski rastvorenih materija bio 2 puta veći od pronosa silta.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Chemical and mechanical water erosion ratio in the Mlava River basin
T1  - Odnos hemijske i mehaničke vodne erozije u slivu Mlave
VL  - 92
IS  - 1
SP  - 27
EP  - 46
DO  - 10.2298/GSGD1201027M
UR  - https://hdl.handle.net/21.15107/rcub_gery_474
ER  - 

@article{
author = "Manojlović, Predrag and Mustafić, Sanja and Mladenović, Ben",
year = "2012",
abstract = "In the hydrological year of 2001/2002, the water samples in the Mlava Basin were analyzed. On its most downstream hydrometric profile, to the Bratinac profile, the water samples were taken every 5 days for TDS an d every day for concentration suspend sediment. It was found that during the analyzed period, the transport of chemically dissolved maters was 2 times higher than the silt deposit transport., U hidrološkoj 2001/2002. godini analizirani su uzorci vode u slivu Mlave na hidrološkom profilu Bratinac Na njenom najnizvodnijem hidrološkom profilu, do profila Bratinac, uzorci vode uzimani su na svakih 5 dana za utvrđivanje rastvorenih mineralnih materija i svakodnevno za utvrđivanje koncentracije slita. Utvrđeno je da je tokom analiziranog perioda pronos hemijski rastvorenih materija bio 2 puta veći od pronosa silta.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Chemical and mechanical water erosion ratio in the Mlava River basin, Odnos hemijske i mehaničke vodne erozije u slivu Mlave",
volume = "92",
number = "1",
pages = "27-46",
doi = "10.2298/GSGD1201027M",
url = "https://hdl.handle.net/21.15107/rcub_gery_474"
}

Manojlović, P., Mustafić, S.,& Mladenović, B.. (2012). Chemical and mechanical water erosion ratio in the Mlava River basin. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 92(1), 27-46.
https://doi.org/10.2298/GSGD1201027M
https://hdl.handle.net/21.15107/rcub_gery_474

Manojlović P, Mustafić S, Mladenović B. Chemical and mechanical water erosion ratio in the Mlava River basin. in Glasnik Srpskog geografskog društva. 2012;92(1):27-46.
doi:10.2298/GSGD1201027M
https://hdl.handle.net/21.15107/rcub_gery_474 .

Manojlović, Predrag, Mustafić, Sanja, Mladenović, Ben, "Chemical and mechanical water erosion ratio in the Mlava River basin" in Glasnik Srpskog geografskog društva, 92, no. 1 (2012):27-46,
https://doi.org/10.2298/GSGD1201027M .,
https://hdl.handle.net/21.15107/rcub_gery_474 .

TY  - JOUR
AU  - Manojlović, Predrag
PY  - 2012
UR  - https://gery.gef.bg.ac.rs/handle/123456789/528
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Ph.D. Radislav Tošić: Basin of the Drenova reservoir: Erosion processes and siltation, Geographical society of the Republic of Srpska, Banja Luka, 2012
T1  - Dr Radislav Tošić: Sliv akumulacije drenova - erozioni procesi i zasipanje akumulacije, Geografsko društvo Republike Srpske, Banja Luka, 2012
VL  - 92
IS  - 1
SP  - 203
EP  - 204
UR  - https://hdl.handle.net/21.15107/rcub_gery_528
ER  - 

@article{
author = "Manojlović, Predrag",
year = "2012",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Ph.D. Radislav Tošić: Basin of the Drenova reservoir: Erosion processes and siltation, Geographical society of the Republic of Srpska, Banja Luka, 2012, Dr Radislav Tošić: Sliv akumulacije drenova - erozioni procesi i zasipanje akumulacije, Geografsko društvo Republike Srpske, Banja Luka, 2012",
volume = "92",
number = "1",
pages = "203-204",
url = "https://hdl.handle.net/21.15107/rcub_gery_528"
}

Manojlović, P.. (2012). Ph.D. Radislav Tošić: Basin of the Drenova reservoir: Erosion processes and siltation, Geographical society of the Republic of Srpska, Banja Luka, 2012. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 92(1), 203-204.
https://hdl.handle.net/21.15107/rcub_gery_528

Manojlović P. Ph.D. Radislav Tošić: Basin of the Drenova reservoir: Erosion processes and siltation, Geographical society of the Republic of Srpska, Banja Luka, 2012. in Glasnik Srpskog geografskog društva. 2012;92(1):203-204.
https://hdl.handle.net/21.15107/rcub_gery_528 .

Manojlović, Predrag, "Ph.D. Radislav Tošić: Basin of the Drenova reservoir: Erosion processes and siltation, Geographical society of the Republic of Srpska, Banja Luka, 2012" in Glasnik Srpskog geografskog društva, 92, no. 1 (2012):203-204,
https://hdl.handle.net/21.15107/rcub_gery_528 .

TY  - JOUR
AU  - Luković, Jelena
AU  - Manojlović, Predrag
AU  - Mustafić, Sanja
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/342
AB  - In this paper connection between temperature changes and North Atlantic oscillation (NAO) has been investigated in the period from 1979 until 2006. Satellite temperature data from UAHMSU were investigated in relation to North Atlantic Oscillation index on the Earth, in Europe and in Serbia. Statistically insignificant correlation coefficient has been obtained for the area of Serbia. The analysis of periodicity of 2.8±0.5 year is in accordance with that one obtained by Landschieidt (2001). However, in order to give final conclusion regarding to climate change more parameters should be analyzed.
AB  - U radu je istraživana veza između temperature vazduha i Severno atlantske oscilacije (NAO) u svetu , u periodu od 1979. do 2006. godine. Ispitivana je veza između satelitskih podataka temperature vazduha UAHMSU i NAO indeksa na prostoru Srbije (17.5-22.5°E i 42.5-47.5°N ), u Evropi (10-45°E i 35-70°N) i svetu po pojasevima od po 10° geografske širine. Uočen je statistički nesignifikantan koeficijent korelacije za prostor Srbije. Analiza elementarne periodičnosti je pokazala da u posmatranom periodu prosečna dužina osnovne periode za MSU od približno 2.8±0.5 godina, odgovara periodičnosti varijanse NAO, koju je dao Landschieidt (2001). Ipak, u isticanju mogućih uzroka savremenih kolebanja klime trebalo bi istovremeno analizirati više parametara cirkulacije atmosfere.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Temperature changes on the Earth and in Serbia and North Atlantic oscillation (NAO)
T1  - Promene temperature vazduha u svetu i Srbiji i Severno atlantska oscilacija (NAO)
VL  - 90
IS  - 1
SP  - 123
EP  - 133
UR  - https://hdl.handle.net/21.15107/rcub_gery_342
ER  - 

@article{
author = "Luković, Jelena and Manojlović, Predrag and Mustafić, Sanja",
year = "2010",
abstract = "In this paper connection between temperature changes and North Atlantic oscillation (NAO) has been investigated in the period from 1979 until 2006. Satellite temperature data from UAHMSU were investigated in relation to North Atlantic Oscillation index on the Earth, in Europe and in Serbia. Statistically insignificant correlation coefficient has been obtained for the area of Serbia. The analysis of periodicity of 2.8±0.5 year is in accordance with that one obtained by Landschieidt (2001). However, in order to give final conclusion regarding to climate change more parameters should be analyzed., U radu je istraživana veza između temperature vazduha i Severno atlantske oscilacije (NAO) u svetu , u periodu od 1979. do 2006. godine. Ispitivana je veza između satelitskih podataka temperature vazduha UAHMSU i NAO indeksa na prostoru Srbije (17.5-22.5°E i 42.5-47.5°N ), u Evropi (10-45°E i 35-70°N) i svetu po pojasevima od po 10° geografske širine. Uočen je statistički nesignifikantan koeficijent korelacije za prostor Srbije. Analiza elementarne periodičnosti je pokazala da u posmatranom periodu prosečna dužina osnovne periode za MSU od približno 2.8±0.5 godina, odgovara periodičnosti varijanse NAO, koju je dao Landschieidt (2001). Ipak, u isticanju mogućih uzroka savremenih kolebanja klime trebalo bi istovremeno analizirati više parametara cirkulacije atmosfere.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Temperature changes on the Earth and in Serbia and North Atlantic oscillation (NAO), Promene temperature vazduha u svetu i Srbiji i Severno atlantska oscilacija (NAO)",
volume = "90",
number = "1",
pages = "123-133",
url = "https://hdl.handle.net/21.15107/rcub_gery_342"
}

Luković, J., Manojlović, P.,& Mustafić, S.. (2010). Temperature changes on the Earth and in Serbia and North Atlantic oscillation (NAO). in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(1), 123-133.
https://hdl.handle.net/21.15107/rcub_gery_342

Luković J, Manojlović P, Mustafić S. Temperature changes on the Earth and in Serbia and North Atlantic oscillation (NAO). in Glasnik Srpskog geografskog društva. 2010;90(1):123-133.
https://hdl.handle.net/21.15107/rcub_gery_342 .

Luković, Jelena, Manojlović, Predrag, Mustafić, Sanja, "Temperature changes on the Earth and in Serbia and North Atlantic oscillation (NAO)" in Glasnik Srpskog geografskog društva, 90, no. 1 (2010):123-133,
https://hdl.handle.net/21.15107/rcub_gery_342 .

TY  - JOUR
AU  - Manojlović, Predrag
AU  - Nikolić, Milena
AU  - Mustafić, Sanja
AU  - Luković, Jelena
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/335
AB  - The mineralization of water and its content in Crvena River so far have not been studied. Water sampling was conducted from April 2008 - May 2009. Total mineralization is relatively low, which is consistent with the dominant lithological structure (Permian red sandstone). Dry residue contains Ca2+ ion, with the increased participation of SiO2. During the observational period it is clearly expressed seasonal effect. It is reflected not in the direct but the indirect impact. Based on the ratio of individual ions a model is determined for estimation of water flow at the confluence of the Crvena River in Nisava River. It could be applied to other drainage basins that have not been studied so far.
AB  - Mineralizacija voda i njena struktura u slivu Crvene reke do sada nije bila predmet istraživanja. Uzorkovanja voda vršena su u periodu april 2008.- maj 2009. godina. Ukupna mineralizacija je relativno niska, što je u skladu sa preovlađujućim petrološkim sastavom (permski crveni peščari). U strukturi suvog ostatka dominira Ca2+ jon, uz povećano učešće SiO2. U toku osmatranog perioda postoji jasno izražen sezonski uticaj. On se ogleda ne u njegovom direktnom, već u posrednom uticaju, preko vodnosti, aktivnosti vegetacije i aktiomiceta. Na osnovu odnosa pojedinih jona utvrđen je model procene proticaja na ušću Crvene reke u Nišavu. On bi se, sa izvesnim korekcijama, mogao primeniti i na drugim hidrološki neizučenim slivovima.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Seasonal variability of Crvena river water mineralization
T1  - Sezonska varijabilnost mineralizacije voda u slivu Crvene reke
VL  - 90
IS  - 4
SP  - 9
EP  - 27
UR  - https://hdl.handle.net/21.15107/rcub_gery_335
ER  - 

@article{
author = "Manojlović, Predrag and Nikolić, Milena and Mustafić, Sanja and Luković, Jelena",
year = "2010",
abstract = "The mineralization of water and its content in Crvena River so far have not been studied. Water sampling was conducted from April 2008 - May 2009. Total mineralization is relatively low, which is consistent with the dominant lithological structure (Permian red sandstone). Dry residue contains Ca2+ ion, with the increased participation of SiO2. During the observational period it is clearly expressed seasonal effect. It is reflected not in the direct but the indirect impact. Based on the ratio of individual ions a model is determined for estimation of water flow at the confluence of the Crvena River in Nisava River. It could be applied to other drainage basins that have not been studied so far., Mineralizacija voda i njena struktura u slivu Crvene reke do sada nije bila predmet istraživanja. Uzorkovanja voda vršena su u periodu april 2008.- maj 2009. godina. Ukupna mineralizacija je relativno niska, što je u skladu sa preovlađujućim petrološkim sastavom (permski crveni peščari). U strukturi suvog ostatka dominira Ca2+ jon, uz povećano učešće SiO2. U toku osmatranog perioda postoji jasno izražen sezonski uticaj. On se ogleda ne u njegovom direktnom, već u posrednom uticaju, preko vodnosti, aktivnosti vegetacije i aktiomiceta. Na osnovu odnosa pojedinih jona utvrđen je model procene proticaja na ušću Crvene reke u Nišavu. On bi se, sa izvesnim korekcijama, mogao primeniti i na drugim hidrološki neizučenim slivovima.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Seasonal variability of Crvena river water mineralization, Sezonska varijabilnost mineralizacije voda u slivu Crvene reke",
volume = "90",
number = "4",
pages = "9-27",
url = "https://hdl.handle.net/21.15107/rcub_gery_335"
}

Manojlović, P., Nikolić, M., Mustafić, S.,& Luković, J.. (2010). Seasonal variability of Crvena river water mineralization. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(4), 9-27.
https://hdl.handle.net/21.15107/rcub_gery_335

Manojlović P, Nikolić M, Mustafić S, Luković J. Seasonal variability of Crvena river water mineralization. in Glasnik Srpskog geografskog društva. 2010;90(4):9-27.
https://hdl.handle.net/21.15107/rcub_gery_335 .

Manojlović, Predrag, Nikolić, Milena, Mustafić, Sanja, Luković, Jelena, "Seasonal variability of Crvena river water mineralization" in Glasnik Srpskog geografskog društva, 90, no. 4 (2010):9-27,
https://hdl.handle.net/21.15107/rcub_gery_335 .

TY  - JOUR
AU  - Milošević, Marko V.
AU  - Manojlović, Predrag
AU  - Mustafić, Sanja
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/375
AB  - The influence of anthropogenic factor on the landslide genesis is analyzed in this paper. Buildings, traffic, water supply and electro infrastructure are introduced in natural landscape as the result of human, living and economic activities in space. The conditions and processes which these objects can cause on the relation object-relief, and therefore initiate the occurrence of landslides, are the change of morphometric characteristics and the modifications of the water balance of slope. The zone with both qualitative and quantitative transformations of relief represents interactive zone in which the influence of man as a genetic factor or modifier of this colluvial process can be observed. .
AB  - U radu je analiziran uticaj antropogenog faktora na genezu klizišta. Kao proizvod ljudskih životnih i privrednih aktivnosti u prostoru dolazi do introdukovanja građevinskih objekata, saobraćajne, vodovodne i elektro infrastrukture u prirodni pejsaž. Uslove i procese koje ovi objekti mogu da izazovu na relaciji objekat-reljef, i da time iniciraju pojavu klizišta, je izmena morfometrijskih karakteristika i izmena vodnog bilansa padine. Zona u kojoj je došlo do kvalitativne i kvantitativne transformacije reljefa predstavlja interaktivnu zonu u kojoj se može sagledati uticaj čoveka kao genetskog faktora ili modifikatora ovog koluvijalnog procesa. .
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Some aspects of anthropogenic influences on the landslide genesis on the territory of municipality of Jagodina
T1  - Neki aspekti antropogenog uticaja na genezu klizišta na teritoriji grada Jagodine
VL  - 90
IS  - 2
SP  - 139
EP  - 149
UR  - https://hdl.handle.net/21.15107/rcub_gery_375
ER  - 

@article{
author = "Milošević, Marko V. and Manojlović, Predrag and Mustafić, Sanja",
year = "2010",
abstract = "The influence of anthropogenic factor on the landslide genesis is analyzed in this paper. Buildings, traffic, water supply and electro infrastructure are introduced in natural landscape as the result of human, living and economic activities in space. The conditions and processes which these objects can cause on the relation object-relief, and therefore initiate the occurrence of landslides, are the change of morphometric characteristics and the modifications of the water balance of slope. The zone with both qualitative and quantitative transformations of relief represents interactive zone in which the influence of man as a genetic factor or modifier of this colluvial process can be observed. ., U radu je analiziran uticaj antropogenog faktora na genezu klizišta. Kao proizvod ljudskih životnih i privrednih aktivnosti u prostoru dolazi do introdukovanja građevinskih objekata, saobraćajne, vodovodne i elektro infrastrukture u prirodni pejsaž. Uslove i procese koje ovi objekti mogu da izazovu na relaciji objekat-reljef, i da time iniciraju pojavu klizišta, je izmena morfometrijskih karakteristika i izmena vodnog bilansa padine. Zona u kojoj je došlo do kvalitativne i kvantitativne transformacije reljefa predstavlja interaktivnu zonu u kojoj se može sagledati uticaj čoveka kao genetskog faktora ili modifikatora ovog koluvijalnog procesa. .",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Some aspects of anthropogenic influences on the landslide genesis on the territory of municipality of Jagodina, Neki aspekti antropogenog uticaja na genezu klizišta na teritoriji grada Jagodine",
volume = "90",
number = "2",
pages = "139-149",
url = "https://hdl.handle.net/21.15107/rcub_gery_375"
}

Milošević, M. V., Manojlović, P.,& Mustafić, S.. (2010). Some aspects of anthropogenic influences on the landslide genesis on the territory of municipality of Jagodina. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(2), 139-149.
https://hdl.handle.net/21.15107/rcub_gery_375

Milošević MV, Manojlović P, Mustafić S. Some aspects of anthropogenic influences on the landslide genesis on the territory of municipality of Jagodina. in Glasnik Srpskog geografskog društva. 2010;90(2):139-149.
https://hdl.handle.net/21.15107/rcub_gery_375 .

Milošević, Marko V., Manojlović, Predrag, Mustafić, Sanja, "Some aspects of anthropogenic influences on the landslide genesis on the territory of municipality of Jagodina" in Glasnik Srpskog geografskog društva, 90, no. 2 (2010):139-149,
https://hdl.handle.net/21.15107/rcub_gery_375 .

TY  - JOUR
AU  - Manojlović, Predrag
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/374
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Slavoljub Dragićević, Dejan Filipović: Prirodni uslovi i nepogode u planiranju i zaštiti prostora, Geografski fakultet, Beograd, 2009
VL  - 90
IS  - 4
SP  - 180
EP  - 181
UR  - https://hdl.handle.net/21.15107/rcub_gery_374
ER  - 

@article{
author = "Manojlović, Predrag",
year = "2010",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Slavoljub Dragićević, Dejan Filipović: Prirodni uslovi i nepogode u planiranju i zaštiti prostora, Geografski fakultet, Beograd, 2009",
volume = "90",
number = "4",
pages = "180-181",
url = "https://hdl.handle.net/21.15107/rcub_gery_374"
}

Manojlović, P.. (2010). Slavoljub Dragićević, Dejan Filipović: Prirodni uslovi i nepogode u planiranju i zaštiti prostora, Geografski fakultet, Beograd, 2009. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(4), 180-181.
https://hdl.handle.net/21.15107/rcub_gery_374

Manojlović P. Slavoljub Dragićević, Dejan Filipović: Prirodni uslovi i nepogode u planiranju i zaštiti prostora, Geografski fakultet, Beograd, 2009. in Glasnik Srpskog geografskog društva. 2010;90(4):180-181.
https://hdl.handle.net/21.15107/rcub_gery_374 .

Manojlović, Predrag, "Slavoljub Dragićević, Dejan Filipović: Prirodni uslovi i nepogode u planiranju i zaštiti prostora, Geografski fakultet, Beograd, 2009" in Glasnik Srpskog geografskog društva, 90, no. 4 (2010):180-181,
https://hdl.handle.net/21.15107/rcub_gery_374 .

TY  - JOUR
AU  - Manojlović, Predrag
PY  - 2010
UR  - https://gery.gef.bg.ac.rs/handle/123456789/371
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Nenad Živković: Prosečni godišnji i sezonski oticaji reka u Srbiji, Geografski fakultet, Beograd, 2009
VL  - 90
IS  - 4
SP  - 180
EP  - 180
UR  - https://hdl.handle.net/21.15107/rcub_gery_371
ER  - 

@article{
author = "Manojlović, Predrag",
year = "2010",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Nenad Živković: Prosečni godišnji i sezonski oticaji reka u Srbiji, Geografski fakultet, Beograd, 2009",
volume = "90",
number = "4",
pages = "180-180",
url = "https://hdl.handle.net/21.15107/rcub_gery_371"
}

Manojlović, P.. (2010). Nenad Živković: Prosečni godišnji i sezonski oticaji reka u Srbiji, Geografski fakultet, Beograd, 2009. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 90(4), 180-180.
https://hdl.handle.net/21.15107/rcub_gery_371

Manojlović P. Nenad Živković: Prosečni godišnji i sezonski oticaji reka u Srbiji, Geografski fakultet, Beograd, 2009. in Glasnik Srpskog geografskog društva. 2010;90(4):180-180.
https://hdl.handle.net/21.15107/rcub_gery_371 .

Manojlović, Predrag, "Nenad Živković: Prosečni godišnji i sezonski oticaji reka u Srbiji, Geografski fakultet, Beograd, 2009" in Glasnik Srpskog geografskog društva, 90, no. 4 (2010):180-180,
https://hdl.handle.net/21.15107/rcub_gery_371 .

TY  - JOUR
AU  - Luković, Jelena
AU  - Manojlović, Predrag
AU  - Mustafić, Sanja
PY  - 2009
UR  - https://gery.gef.bg.ac.rs/handle/123456789/311
AB  - In this paper the air temperature changes have been investigated on the base of satellite measurement, in the period from 1979 until 2006. The analysis has shown that there is no temperature amplification with altitude. Data for Serbia have shown negative trend of temperature in the last 20 years of the investigated period. Although it is not statistically significant, the sign is not in accordance with the increasing CO2 concentration. This may mean that the sign of satellite temperature doesn't support hypothesis about domination of anthropogenic greenhouse effects. .
AB  - U radu je analizirana promena temperature vazduha u Srbiji i svetu, na osnovu podataka satelitskih osmatranja, u periodu od 1979. do 2006. godine. Analiza trenda je pokazala da nema amplifikacije trenda porasta temperature sa visinom. Analiza za Srbiju pokazala je u poslednjih 20 godina u posmatranom periodu od 1987. do 2006. godine negativan, trend temperature vazduha. Iako statistički nesignifikantan, znak trenda nije saglasan sa rastućom koncentracijom antropogenog SO2. To bi značilo da znak promena satelitskih temperatura vazduha u posmatranom periodu nije u skladu sa očekivanim, u uslovima dominacije antropogenog efekta staklene bašte.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Temperature changes in Serbia and worldwide according to satellite data
T1  - Promene temperature vazduha na osnovu satelitskih osmatranja u Srbiji i svetu
VL  - 89
IS  - 3
SP  - 177
EP  - 189
UR  - https://hdl.handle.net/21.15107/rcub_gery_311
ER  - 

@article{
author = "Luković, Jelena and Manojlović, Predrag and Mustafić, Sanja",
year = "2009",
abstract = "In this paper the air temperature changes have been investigated on the base of satellite measurement, in the period from 1979 until 2006. The analysis has shown that there is no temperature amplification with altitude. Data for Serbia have shown negative trend of temperature in the last 20 years of the investigated period. Although it is not statistically significant, the sign is not in accordance with the increasing CO2 concentration. This may mean that the sign of satellite temperature doesn't support hypothesis about domination of anthropogenic greenhouse effects. ., U radu je analizirana promena temperature vazduha u Srbiji i svetu, na osnovu podataka satelitskih osmatranja, u periodu od 1979. do 2006. godine. Analiza trenda je pokazala da nema amplifikacije trenda porasta temperature sa visinom. Analiza za Srbiju pokazala je u poslednjih 20 godina u posmatranom periodu od 1987. do 2006. godine negativan, trend temperature vazduha. Iako statistički nesignifikantan, znak trenda nije saglasan sa rastućom koncentracijom antropogenog SO2. To bi značilo da znak promena satelitskih temperatura vazduha u posmatranom periodu nije u skladu sa očekivanim, u uslovima dominacije antropogenog efekta staklene bašte.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Temperature changes in Serbia and worldwide according to satellite data, Promene temperature vazduha na osnovu satelitskih osmatranja u Srbiji i svetu",
volume = "89",
number = "3",
pages = "177-189",
url = "https://hdl.handle.net/21.15107/rcub_gery_311"
}

Luković, J., Manojlović, P.,& Mustafić, S.. (2009). Temperature changes in Serbia and worldwide according to satellite data. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 89(3), 177-189.
https://hdl.handle.net/21.15107/rcub_gery_311

Luković J, Manojlović P, Mustafić S. Temperature changes in Serbia and worldwide according to satellite data. in Glasnik Srpskog geografskog društva. 2009;89(3):177-189.
https://hdl.handle.net/21.15107/rcub_gery_311 .

Luković, Jelena, Manojlović, Predrag, Mustafić, Sanja, "Temperature changes in Serbia and worldwide according to satellite data" in Glasnik Srpskog geografskog društva, 89, no. 3 (2009):177-189,
https://hdl.handle.net/21.15107/rcub_gery_311 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Milinčić, Miroljub
PY  - 2009
UR  - https://gery.gef.bg.ac.rs/handle/123456789/308
AB  - The drainage basin is spatially and functionally clearly defined and relevant hydrologic, geomorphologic and ecologic landscape totality. Therefore, it mostly represents basic geo-spatial unit of generation, monitoring, and studying numerous physical-geographical and geo-ecologic occurrences and processes. One of the most important components of geo-space, on the level of basin, is manifested through the state and quality of surface waters. So, the acceptance of systematic approach in studying mineralization of the surface waters would contribute to the deeper understanding of the process in complex systematic surroundings which drainage basin represents. The Visočica Drainage Basin was chosen as proving ground of this kind of the research approach for several reasons. The highest specific runoff on the territory of Eastern Serbia, heterogeneous geologic structure of terrain, almost complete absence of the influence of the anthropogenic factor on the state of the environment, as well as the existence of water accumulation enabled perception of the values of dissolved mineral substances of surface waters as landscape-ecologic component of geo-space.
AB  - Sliv je prostorno i funkcionalno, jasno definisana i relevantna hidrološka, geomorfološka i ekološka predeona celina. Zato on najčešće predstavlja osnovnu geoprostornu jedinicu generisanja, praćenja i proučavanja mnogobrojnih fizičko-geografskih i geo-ekoloških pojava i procesa. Jedna od najznačajnijih komponenti geoprostora na nivou sliva manifestuje se kroz stanje i kvalitet površinskih voda. S toga bi prihvatanje sistemskog pristupa u proučavanju mineralizacije površinskih voda potpomoglo dublje razumevanje procesa u složenom sistemskom okruženju kakav je sliv. Kao poligon takve vrste istraživačkog pristupa sliv Visočice odabran je iz nekoliko razloga. Najviši specifični oticaji na prostoru istočne Srbije, heterogen geološki sastav terena, skoro potpuno odsustvo uticaja antropogenog faktora na stanje životne sredine, kao i postojanje vodne akumulacije Zavoj omogućilo je sagledavanje vrednosti rastvorenih mineralnih materija površinskih voda kao predeono-ekološke komponente geoprostora.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Mineralization of the surface waters in the Visočica drainage basin: Supplement for the landscape-ecologic analysis
T1  - Mineralizacija površinskih voda u slivu Visočice - prilog za predeono-ekološku analizu
VL  - 89
IS  - 4
SP  - 141
EP  - 160
UR  - https://hdl.handle.net/21.15107/rcub_gery_308
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Milinčić, Miroljub",
year = "2009",
abstract = "The drainage basin is spatially and functionally clearly defined and relevant hydrologic, geomorphologic and ecologic landscape totality. Therefore, it mostly represents basic geo-spatial unit of generation, monitoring, and studying numerous physical-geographical and geo-ecologic occurrences and processes. One of the most important components of geo-space, on the level of basin, is manifested through the state and quality of surface waters. So, the acceptance of systematic approach in studying mineralization of the surface waters would contribute to the deeper understanding of the process in complex systematic surroundings which drainage basin represents. The Visočica Drainage Basin was chosen as proving ground of this kind of the research approach for several reasons. The highest specific runoff on the territory of Eastern Serbia, heterogeneous geologic structure of terrain, almost complete absence of the influence of the anthropogenic factor on the state of the environment, as well as the existence of water accumulation enabled perception of the values of dissolved mineral substances of surface waters as landscape-ecologic component of geo-space., Sliv je prostorno i funkcionalno, jasno definisana i relevantna hidrološka, geomorfološka i ekološka predeona celina. Zato on najčešće predstavlja osnovnu geoprostornu jedinicu generisanja, praćenja i proučavanja mnogobrojnih fizičko-geografskih i geo-ekoloških pojava i procesa. Jedna od najznačajnijih komponenti geoprostora na nivou sliva manifestuje se kroz stanje i kvalitet površinskih voda. S toga bi prihvatanje sistemskog pristupa u proučavanju mineralizacije površinskih voda potpomoglo dublje razumevanje procesa u složenom sistemskom okruženju kakav je sliv. Kao poligon takve vrste istraživačkog pristupa sliv Visočice odabran je iz nekoliko razloga. Najviši specifični oticaji na prostoru istočne Srbije, heterogen geološki sastav terena, skoro potpuno odsustvo uticaja antropogenog faktora na stanje životne sredine, kao i postojanje vodne akumulacije Zavoj omogućilo je sagledavanje vrednosti rastvorenih mineralnih materija površinskih voda kao predeono-ekološke komponente geoprostora.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Mineralization of the surface waters in the Visočica drainage basin: Supplement for the landscape-ecologic analysis, Mineralizacija površinskih voda u slivu Visočice - prilog za predeono-ekološku analizu",
volume = "89",
number = "4",
pages = "141-160",
url = "https://hdl.handle.net/21.15107/rcub_gery_308"
}

Mustafić, S., Manojlović, P.,& Milinčić, M.. (2009). Mineralization of the surface waters in the Visočica drainage basin: Supplement for the landscape-ecologic analysis. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 89(4), 141-160.
https://hdl.handle.net/21.15107/rcub_gery_308

Mustafić S, Manojlović P, Milinčić M. Mineralization of the surface waters in the Visočica drainage basin: Supplement for the landscape-ecologic analysis. in Glasnik Srpskog geografskog društva. 2009;89(4):141-160.
https://hdl.handle.net/21.15107/rcub_gery_308 .

Mustafić, Sanja, Manojlović, Predrag, Milinčić, Miroljub, "Mineralization of the surface waters in the Visočica drainage basin: Supplement for the landscape-ecologic analysis" in Glasnik Srpskog geografskog društva, 89, no. 4 (2009):141-160,
https://hdl.handle.net/21.15107/rcub_gery_308 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Kostadinov, Stanimir
AU  - Manojlović, Predrag
PY  - 2008
UR  - https://gery.gef.bg.ac.rs/handle/123456789/249
AB  - In this paper land erosion has been investigated from its temporal and spatial variability point of view. The aim of the application of contemporary soft wares and satellite observations was to create an adequate data base which allows faster and more adequate possibility for monitoring the intensity of erosive processes, as well as meaningful decision for application of different ways of anti erosive techniques of the most dangerous areas. Geomorphologic mapping of erosive processes using plane and satellite images has allowed rational planning of field observations and, at the other side very detailed establishing of the intensity of previous erosion. A new approach applied in this paper during data processing of all relevant parameters influencing erosion is based on using of software Geomedia 5.2 (Intergraph).
AB  - Rad tretira proces erozije zemljišta sa stanovišta njegove prostorno-vremenske varijabilnosti. Primena savremenih programskih paketa i satelitskih osmatranja ima za cilj formiranje adekvatne baze podataka, koja omogućava bržu i adekvatniju mogućnost praćenja stanja i intenziteta erozivnih procesa, a samim tim i svrsishodniju odluku o primeni različitih vidova anterozivnih mera zaštite najugroženijih prostora. Geomorfološko kartiranje erozivnih procesa putem avionskih i satelitskih snimaka omogućilo je, s jedne strane, racionalno planiranje terenskih opseravcija, a sa druge strane veoma detaljno utvrđivanje intenziteta erozije u prošlosti. Novi pristup primenjen u ovom radu prilikom obrade svih relevantnih parametara koji utiču na proces erozije, zasniva se na korišćenju programskog paketa Geomedia 5.2 (Intergraf).
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Risk of artificial lake 'Zavoj' to processes of erosion: Methodological, knowing and protecting aspect
T1  - Ugroženost akumulacije 'Zavoj' erozivnim procesima - metodološki, saznajni i zaštitni aspekt
VL  - 88
IS  - 1
SP  - 29
EP  - 42
UR  - https://hdl.handle.net/21.15107/rcub_gery_249
ER  - 

@article{
author = "Mustafić, Sanja and Kostadinov, Stanimir and Manojlović, Predrag",
year = "2008",
abstract = "In this paper land erosion has been investigated from its temporal and spatial variability point of view. The aim of the application of contemporary soft wares and satellite observations was to create an adequate data base which allows faster and more adequate possibility for monitoring the intensity of erosive processes, as well as meaningful decision for application of different ways of anti erosive techniques of the most dangerous areas. Geomorphologic mapping of erosive processes using plane and satellite images has allowed rational planning of field observations and, at the other side very detailed establishing of the intensity of previous erosion. A new approach applied in this paper during data processing of all relevant parameters influencing erosion is based on using of software Geomedia 5.2 (Intergraph)., Rad tretira proces erozije zemljišta sa stanovišta njegove prostorno-vremenske varijabilnosti. Primena savremenih programskih paketa i satelitskih osmatranja ima za cilj formiranje adekvatne baze podataka, koja omogućava bržu i adekvatniju mogućnost praćenja stanja i intenziteta erozivnih procesa, a samim tim i svrsishodniju odluku o primeni različitih vidova anterozivnih mera zaštite najugroženijih prostora. Geomorfološko kartiranje erozivnih procesa putem avionskih i satelitskih snimaka omogućilo je, s jedne strane, racionalno planiranje terenskih opseravcija, a sa druge strane veoma detaljno utvrđivanje intenziteta erozije u prošlosti. Novi pristup primenjen u ovom radu prilikom obrade svih relevantnih parametara koji utiču na proces erozije, zasniva se na korišćenju programskog paketa Geomedia 5.2 (Intergraf).",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Risk of artificial lake 'Zavoj' to processes of erosion: Methodological, knowing and protecting aspect, Ugroženost akumulacije 'Zavoj' erozivnim procesima - metodološki, saznajni i zaštitni aspekt",
volume = "88",
number = "1",
pages = "29-42",
url = "https://hdl.handle.net/21.15107/rcub_gery_249"
}

Mustafić, S., Kostadinov, S.,& Manojlović, P.. (2008). Risk of artificial lake 'Zavoj' to processes of erosion: Methodological, knowing and protecting aspect. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 88(1), 29-42.
https://hdl.handle.net/21.15107/rcub_gery_249

Mustafić S, Kostadinov S, Manojlović P. Risk of artificial lake 'Zavoj' to processes of erosion: Methodological, knowing and protecting aspect. in Glasnik Srpskog geografskog društva. 2008;88(1):29-42.
https://hdl.handle.net/21.15107/rcub_gery_249 .

Mustafić, Sanja, Kostadinov, Stanimir, Manojlović, Predrag, "Risk of artificial lake 'Zavoj' to processes of erosion: Methodological, knowing and protecting aspect" in Glasnik Srpskog geografskog društva, 88, no. 1 (2008):29-42,
https://hdl.handle.net/21.15107/rcub_gery_249 .

TY  - JOUR
AU  - Mustafić, Sanja
AU  - Manojlović, Predrag
AU  - Dragićević, Slavoljub
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/242
AB  - Modern geomorphologic investigations of condition and change of the intensity of erosive process should be based on application of remote sensing methods which are based on processing of aerial and satellite photographs. Using of these methods is very important because it enables good possibilities for realizing regional relations of the investigated phenomenon, as well as the estimate of spatial and temporal variability of all physical-geographical and anthropogenic factors influencing given process. Realizing process of land erosion, on the whole, is only possible by creating universal data base, as well as by using of appropriate software, more exactly by establishing uniform information system. Geographical information system, as the most effective one, the most complex and the most integral system of information about the space enables unification as well as analytical and synthetically processing of all data.
AB  - Geografski informacioni sistemi pružaju nam širok raspon mogućnosti analize i sinteze, koje se mogu upotrebljavati na različite načine. Analitičke mogućnosti ovako formirane baze podataka organizovane su tako da se svaka vrsta analize jednog parametra može izvesti ili zasebno ili u kombinaciji sa drugima parametrima. Mogućnosti sinteze su višestruke, a najadekvatnije su predstavljene vizelizacijom različitih vrsta digitalnih podatka, kao i mogućnošću iznalaženja i primene različitih vrsta modela. Može se zaključiti da sa rastućim potrebama geomorfologa, uspostavljanjem novih pitanja i hipoteza, računarsko- softverska analiza i modelovanje u geomorfologiji predstavljaju nezaobilazan pravac istraživanja.
PB  - Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"
T2  - Zbornik radova Geografskog instituta "Jovan Cvijić", SANU
T1  - Application of remote sensing methods and GIS in erosive process investigations
T1  - Primena teledetekcionih metoda i GIS-a u istraživanjima erozivnih procesa
IS  - 57
SP  - 465
EP  - 473
UR  - https://hdl.handle.net/21.15107/rcub_gery_242
ER  - 

@article{
author = "Mustafić, Sanja and Manojlović, Predrag and Dragićević, Slavoljub",
year = "2007",
abstract = "Modern geomorphologic investigations of condition and change of the intensity of erosive process should be based on application of remote sensing methods which are based on processing of aerial and satellite photographs. Using of these methods is very important because it enables good possibilities for realizing regional relations of the investigated phenomenon, as well as the estimate of spatial and temporal variability of all physical-geographical and anthropogenic factors influencing given process. Realizing process of land erosion, on the whole, is only possible by creating universal data base, as well as by using of appropriate software, more exactly by establishing uniform information system. Geographical information system, as the most effective one, the most complex and the most integral system of information about the space enables unification as well as analytical and synthetically processing of all data., Geografski informacioni sistemi pružaju nam širok raspon mogućnosti analize i sinteze, koje se mogu upotrebljavati na različite načine. Analitičke mogućnosti ovako formirane baze podataka organizovane su tako da se svaka vrsta analize jednog parametra može izvesti ili zasebno ili u kombinaciji sa drugima parametrima. Mogućnosti sinteze su višestruke, a najadekvatnije su predstavljene vizelizacijom različitih vrsta digitalnih podatka, kao i mogućnošću iznalaženja i primene različitih vrsta modela. Može se zaključiti da sa rastućim potrebama geomorfologa, uspostavljanjem novih pitanja i hipoteza, računarsko- softverska analiza i modelovanje u geomorfologiji predstavljaju nezaobilazan pravac istraživanja.",
publisher = "Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić"",
journal = "Zbornik radova Geografskog instituta "Jovan Cvijić", SANU",
title = "Application of remote sensing methods and GIS in erosive process investigations, Primena teledetekcionih metoda i GIS-a u istraživanjima erozivnih procesa",
number = "57",
pages = "465-473",
url = "https://hdl.handle.net/21.15107/rcub_gery_242"
}

Mustafić, S., Manojlović, P.,& Dragićević, S.. (2007). Application of remote sensing methods and GIS in erosive process investigations. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU
Beograd : Srpska akademija nauka i umetnosti SANU - Geografski institut "Jovan Cvijić".(57), 465-473.
https://hdl.handle.net/21.15107/rcub_gery_242

Mustafić S, Manojlović P, Dragićević S. Application of remote sensing methods and GIS in erosive process investigations. in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU. 2007;(57):465-473.
https://hdl.handle.net/21.15107/rcub_gery_242 .

Mustafić, Sanja, Manojlović, Predrag, Dragićević, Slavoljub, "Application of remote sensing methods and GIS in erosive process investigations" in Zbornik radova Geografskog instituta "Jovan Cvijić", SANU, no. 57 (2007):465-473,
https://hdl.handle.net/21.15107/rcub_gery_242 .

TY  - JOUR
AU  - Dragićević, Slavoljub
AU  - Manojlović, Predrag
AU  - Nikolić, Jugoslav
PY  - 2007
UR  - https://gery.gef.bg.ac.rs/handle/123456789/219
AB  - Recent methodology of sampling and establishing silt deposit concentration in Serbian rivers is associated to numerous deficiencies. Daily concentrations of this type of river deposit on the most of the hydrological gauges were obtained on the base of only one measurement, which takes into consideration the matter of representative ness of those samples. Taking the samples of deposit in one point on the profile is little bit problematic because of dispersion of the obtained results. Very important matter is the question of choice of the sampling location. This analyses of data may lead to serious spots in calculating total carried deposit. From the above mentioned reasons, we decided to take precise measurements of silt deposit concentration as well as to establish methodological spots of measurements. The results of these measurements are analyzed and presented in this paper.
AB  - Dosadašnja metodologija uzimanja uzoraka i utvrđivanja koncentracija suspendovanog nanosa na našim rekama karakteriše se brojnim nedostatcima. Dnevne koncentracije ovog tipa rečnog nanosa na najvećem broju hidroloških stanica dobijene su na osnovu samo jednog merenja čime se postavlja pitanje reprezentativnosti takvih uzoraka. Zahvatanje uzoraka nanosa u jednoj tački profila veoma je problematično zbog velikog stepena rasipanja dobijenih rezultata, a postavlja se i pitanje pravilnog izbora lokacija za obavljanje merenja. Ovakva vrsta podataka može dovesti do ozbiljnih pogrešaka u izračunavanju sumarnog pronosa nanosa. Iz navedenih razloga, pristupilo se ideji sprovođenja preciznijih merenja koncentracija suspendovanog nanosa i utvrđivanju metodološke greške postojećih merenja. Rezultati merenja analizirani su i prikazani u ovom radu.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Methodological spot of establishing silt deposit concentration in Serbian rivers
T1  - Metodološka greška utvrđivanja koncentracije suspendovanog nanosa na našim rekama
VL  - 87
IS  - 1
SP  - 15
EP  - 22
UR  - https://hdl.handle.net/21.15107/rcub_gery_219
ER  - 

@article{
author = "Dragićević, Slavoljub and Manojlović, Predrag and Nikolić, Jugoslav",
year = "2007",
abstract = "Recent methodology of sampling and establishing silt deposit concentration in Serbian rivers is associated to numerous deficiencies. Daily concentrations of this type of river deposit on the most of the hydrological gauges were obtained on the base of only one measurement, which takes into consideration the matter of representative ness of those samples. Taking the samples of deposit in one point on the profile is little bit problematic because of dispersion of the obtained results. Very important matter is the question of choice of the sampling location. This analyses of data may lead to serious spots in calculating total carried deposit. From the above mentioned reasons, we decided to take precise measurements of silt deposit concentration as well as to establish methodological spots of measurements. The results of these measurements are analyzed and presented in this paper., Dosadašnja metodologija uzimanja uzoraka i utvrđivanja koncentracija suspendovanog nanosa na našim rekama karakteriše se brojnim nedostatcima. Dnevne koncentracije ovog tipa rečnog nanosa na najvećem broju hidroloških stanica dobijene su na osnovu samo jednog merenja čime se postavlja pitanje reprezentativnosti takvih uzoraka. Zahvatanje uzoraka nanosa u jednoj tački profila veoma je problematično zbog velikog stepena rasipanja dobijenih rezultata, a postavlja se i pitanje pravilnog izbora lokacija za obavljanje merenja. Ovakva vrsta podataka može dovesti do ozbiljnih pogrešaka u izračunavanju sumarnog pronosa nanosa. Iz navedenih razloga, pristupilo se ideji sprovođenja preciznijih merenja koncentracija suspendovanog nanosa i utvrđivanju metodološke greške postojećih merenja. Rezultati merenja analizirani su i prikazani u ovom radu.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Methodological spot of establishing silt deposit concentration in Serbian rivers, Metodološka greška utvrđivanja koncentracije suspendovanog nanosa na našim rekama",
volume = "87",
number = "1",
pages = "15-22",
url = "https://hdl.handle.net/21.15107/rcub_gery_219"
}

Dragićević, S., Manojlović, P.,& Nikolić, J.. (2007). Methodological spot of establishing silt deposit concentration in Serbian rivers. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 87(1), 15-22.
https://hdl.handle.net/21.15107/rcub_gery_219

Dragićević S, Manojlović P, Nikolić J. Methodological spot of establishing silt deposit concentration in Serbian rivers. in Glasnik Srpskog geografskog društva. 2007;87(1):15-22.
https://hdl.handle.net/21.15107/rcub_gery_219 .

Dragićević, Slavoljub, Manojlović, Predrag, Nikolić, Jugoslav, "Methodological spot of establishing silt deposit concentration in Serbian rivers" in Glasnik Srpskog geografskog društva, 87, no. 1 (2007):15-22,
https://hdl.handle.net/21.15107/rcub_gery_219 .

TY  - JOUR
AU  - Manojlović, Predrag
AU  - Damnjanović-Rakić, Milica
PY  - 2006
UR  - https://gery.gef.bg.ac.rs/handle/123456789/169
AB  - How big is the influence of climatic factor on the intensity of rocks dissolving (limestone) in Serbia? Previous investigations of rivers water chemistry changes have shown it insignificance. This investigation shows significant collective influence of climatic elements contained in "seasonal factor".
AB  - Koliki je uticaj klimatskog faktora na intenzitet rastvaranja stena (krečnjaka) u Srbiji. Dosadašnjim istraživanjima promene hemizma vode rečnih tokova zaključeno je da je on minoran. Ovim istraživanjima uočen je značajan upliv zbirnog uticaja klimatskih elemenata sadržanih u "sezonskom faktoru".
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - The influence of seasonal factor on chemical dissolving of limestone variability in Svrljiška valley
T1  - Uticaj sezonskog faktora na varijabilnost hemijskog rastvaranja krečnjaka u Svrljiškoj kotlini
VL  - 86
IS  - 2
SP  - 29
EP  - 36
UR  - https://hdl.handle.net/21.15107/rcub_gery_169
ER  - 

@article{
author = "Manojlović, Predrag and Damnjanović-Rakić, Milica",
year = "2006",
abstract = "How big is the influence of climatic factor on the intensity of rocks dissolving (limestone) in Serbia? Previous investigations of rivers water chemistry changes have shown it insignificance. This investigation shows significant collective influence of climatic elements contained in "seasonal factor"., Koliki je uticaj klimatskog faktora na intenzitet rastvaranja stena (krečnjaka) u Srbiji. Dosadašnjim istraživanjima promene hemizma vode rečnih tokova zaključeno je da je on minoran. Ovim istraživanjima uočen je značajan upliv zbirnog uticaja klimatskih elemenata sadržanih u "sezonskom faktoru".",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "The influence of seasonal factor on chemical dissolving of limestone variability in Svrljiška valley, Uticaj sezonskog faktora na varijabilnost hemijskog rastvaranja krečnjaka u Svrljiškoj kotlini",
volume = "86",
number = "2",
pages = "29-36",
url = "https://hdl.handle.net/21.15107/rcub_gery_169"
}

Manojlović, P.,& Damnjanović-Rakić, M.. (2006). The influence of seasonal factor on chemical dissolving of limestone variability in Svrljiška valley. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 86(2), 29-36.
https://hdl.handle.net/21.15107/rcub_gery_169

Manojlović P, Damnjanović-Rakić M. The influence of seasonal factor on chemical dissolving of limestone variability in Svrljiška valley. in Glasnik Srpskog geografskog društva. 2006;86(2):29-36.
https://hdl.handle.net/21.15107/rcub_gery_169 .

Manojlović, Predrag, Damnjanović-Rakić, Milica, "The influence of seasonal factor on chemical dissolving of limestone variability in Svrljiška valley" in Glasnik Srpskog geografskog društva, 86, no. 2 (2006):29-36,
https://hdl.handle.net/21.15107/rcub_gery_169 .

TY  - JOUR
AU  - Manojlović, Predrag
AU  - Dragićević, Slavoljub
AU  - Mustafić, Sanja
PY  - 2004
UR  - https://gery.gef.bg.ac.rs/handle/123456789/99
AB  - By using the database that is based on grid system of 1 km2 from Laboratory of physical geography, few quantitative maps have been made. Their researching and analyzing can show global relations on Serbian territory. Their importance overcomes geomorphologic needs, because they could be used for spatial planning, economic needs and environment protection.
AB  - Korišćenjem baze podataka Laboratorije fizičke geografije zasnovane na grid sistemu od 1 km2, urađeno je nekoliko kvantitativnih karata. Njihovim sagledavanjem i analizom mogu se dobiti globalni odnosi na prostoru Srbije. Njihova upotrebna vrednost prevazilazi potrebe geomorfologije, jer se mogu koristiti u prostornom planiranju, potrebama privrede i zaštiti životne sredine.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - The basic morphometric characteristics of Serbian relief
T1  - Osnovne morfometrijske karakteristike reljefa Srbije
VL  - 84
IS  - 2
SP  - 11
EP  - 20
UR  - https://hdl.handle.net/21.15107/rcub_gery_99
ER  - 

@article{
author = "Manojlović, Predrag and Dragićević, Slavoljub and Mustafić, Sanja",
year = "2004",
abstract = "By using the database that is based on grid system of 1 km2 from Laboratory of physical geography, few quantitative maps have been made. Their researching and analyzing can show global relations on Serbian territory. Their importance overcomes geomorphologic needs, because they could be used for spatial planning, economic needs and environment protection., Korišćenjem baze podataka Laboratorije fizičke geografije zasnovane na grid sistemu od 1 km2, urađeno je nekoliko kvantitativnih karata. Njihovim sagledavanjem i analizom mogu se dobiti globalni odnosi na prostoru Srbije. Njihova upotrebna vrednost prevazilazi potrebe geomorfologije, jer se mogu koristiti u prostornom planiranju, potrebama privrede i zaštiti životne sredine.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "The basic morphometric characteristics of Serbian relief, Osnovne morfometrijske karakteristike reljefa Srbije",
volume = "84",
number = "2",
pages = "11-20",
url = "https://hdl.handle.net/21.15107/rcub_gery_99"
}

Manojlović, P., Dragićević, S.,& Mustafić, S.. (2004). The basic morphometric characteristics of Serbian relief. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 84(2), 11-20.
https://hdl.handle.net/21.15107/rcub_gery_99

Manojlović P, Dragićević S, Mustafić S. The basic morphometric characteristics of Serbian relief. in Glasnik Srpskog geografskog društva. 2004;84(2):11-20.
https://hdl.handle.net/21.15107/rcub_gery_99 .

Manojlović, Predrag, Dragićević, Slavoljub, Mustafić, Sanja, "The basic morphometric characteristics of Serbian relief" in Glasnik Srpskog geografskog društva, 84, no. 2 (2004):11-20,
https://hdl.handle.net/21.15107/rcub_gery_99 .

TY  - JOUR
AU  - Dragićević, Slavoljub
AU  - Manojlović, Predrag
AU  - Mustafić, Sanja
PY  - 2003
UR  - https://gery.gef.bg.ac.rs/handle/123456789/68
AB  - Based on the research of the chemical erosion intensity in the upper course of Tamnava, the appearance of its negative value has been found. Further researches, that enclose the lower course, confirmed this fact. This research opened the important question about the causes of this phenomena. Analytical method eliminated all expected causes and led to conclusion that the reason for this should be found by using the more precise research of the mineralization of the precipitations. It was necessary to continue the measuring of the precipitation mineralization in the greater number of locations and in the wider time period, as well as in the different meteorological conditions, and after that to establish the subordination between the amount of precipitations and the entered TDS. Only after these additive researches we could be able to find out the relation between ''entry'' and ''exit'' and to find out the intensity of the chemical erosion in this, and in the other river basins. For now, we are able only to find out the carrying of TDS, as well as the reduction of the chemical evacuation for the non - carbonated part of the basin (corrected value).
AB  - Detaljnim geomorfološkim istraživanjima intenziteta hemijske erozije do nedavno je bio obuhvaćen samo prostor istočne Srbije, tako da ovo istraživanje ima za cilj određivanje iznosa ovog dela rečne erozije i u zapadnim delovima naše zemlje. Na osnovu opsežnih terenskih i laboratorijskih merenja koncentracija najvažnijih makrojona na dva hidrološka profila reke Tamnave i na toj osnovi određivanja vrednosti suvog ostatka, ostvarena je mogućnost izračunavanja intenziteta hemijske erozije u ovom slivu.
PB  - Beograd : Srpsko geografsko društvo
T2  - Glasnik Srpskog geografskog društva
T1  - Contribution to the research of the chemical intensity erosion in the western Serbia
T1  - Prilog određivanju intenziteta hemijske erozije zapadne Srbije
VL  - 83
IS  - 1
SP  - 7
EP  - 14
UR  - https://hdl.handle.net/21.15107/rcub_gery_68
ER  - 

@article{
author = "Dragićević, Slavoljub and Manojlović, Predrag and Mustafić, Sanja",
year = "2003",
abstract = "Based on the research of the chemical erosion intensity in the upper course of Tamnava, the appearance of its negative value has been found. Further researches, that enclose the lower course, confirmed this fact. This research opened the important question about the causes of this phenomena. Analytical method eliminated all expected causes and led to conclusion that the reason for this should be found by using the more precise research of the mineralization of the precipitations. It was necessary to continue the measuring of the precipitation mineralization in the greater number of locations and in the wider time period, as well as in the different meteorological conditions, and after that to establish the subordination between the amount of precipitations and the entered TDS. Only after these additive researches we could be able to find out the relation between ''entry'' and ''exit'' and to find out the intensity of the chemical erosion in this, and in the other river basins. For now, we are able only to find out the carrying of TDS, as well as the reduction of the chemical evacuation for the non - carbonated part of the basin (corrected value)., Detaljnim geomorfološkim istraživanjima intenziteta hemijske erozije do nedavno je bio obuhvaćen samo prostor istočne Srbije, tako da ovo istraživanje ima za cilj određivanje iznosa ovog dela rečne erozije i u zapadnim delovima naše zemlje. Na osnovu opsežnih terenskih i laboratorijskih merenja koncentracija najvažnijih makrojona na dva hidrološka profila reke Tamnave i na toj osnovi određivanja vrednosti suvog ostatka, ostvarena je mogućnost izračunavanja intenziteta hemijske erozije u ovom slivu.",
publisher = "Beograd : Srpsko geografsko društvo",
journal = "Glasnik Srpskog geografskog društva",
title = "Contribution to the research of the chemical intensity erosion in the western Serbia, Prilog određivanju intenziteta hemijske erozije zapadne Srbije",
volume = "83",
number = "1",
pages = "7-14",
url = "https://hdl.handle.net/21.15107/rcub_gery_68"
}

Dragićević, S., Manojlović, P.,& Mustafić, S.. (2003). Contribution to the research of the chemical intensity erosion in the western Serbia. in Glasnik Srpskog geografskog društva
Beograd : Srpsko geografsko društvo., 83(1), 7-14.
https://hdl.handle.net/21.15107/rcub_gery_68

Dragićević S, Manojlović P, Mustafić S. Contribution to the research of the chemical intensity erosion in the western Serbia. in Glasnik Srpskog geografskog društva. 2003;83(1):7-14.
https://hdl.handle.net/21.15107/rcub_gery_68 .

Dragićević, Slavoljub, Manojlović, Predrag, Mustafić, Sanja, "Contribution to the research of the chemical intensity erosion in the western Serbia" in Glasnik Srpskog geografskog društva, 83, no. 1 (2003):7-14,
https://hdl.handle.net/21.15107/rcub_gery_68 .