Đokić, Ivan

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Altitudinal zonation of runoff in the Rasina River Basin

Manojlović, Predrag; Srejić, Milan; Đokić, Ivan; Mustafić, Sanja; Dobrosavljević, Tanja

(Beograd : Srpsko geografsko društvo, 2013)

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 .