TY  - JOUR
AU  - Đukić, Vesna
AU  - Mihailović, Vladislava
PY  - 2012
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/456
AB  - Evapotranspiracija je jedan od najznačajnijih procesa unutar hidrološkog ciklusa, čija pouzdana procena je od suštinske važnosti pri planiranju i upravljanju zemljišnim i vodnim resursima i, od čije veličine direktno zavise potrebe biljaka za vodom. U radu je izvršeno poređenje proračunatih vrednosti referentne evapotranspiracije primenom metode FAO Blaney-Criddle-a, FAO Radijacione metode, metode FAO Penmana i FAO 56 Penman-Montejeve metode sa rezultatima lizimetarskih merenja u Košutnjaku tokom vegetacionih sezona u 2004., 2005. i 2006. godini. Pokazano je da se primenom FAO 56 Penman-Montejeve jednačine dobijaju rezultati najpribližniji rezultatima lizimetarskih merenja, zbog čega se preporučuje primena ove metode pri oceni referentne evapotranspiracije.
AB  - Evapotranspiration is one of the most important processes within the hydrological cycle whose reliable assessment is essential in the planning and managing of land and water resources. Besides that, the water needs of plants depend directly on the size of evapotranspiration. This paper presents a comparison of reference evapotranspiration values calculated using the FAO Blaney-Criddle method, the FAO Radiation methods, the FAO Penman and the FAO 56 Penman-Monteith method with the results of measurements of evapotranspiration at the meteorological station in Košutnjak during the growing seasons of 2004, 2005 and 2006. It is shown that the application of the FAO 56 Penman-Monteith equation provides the calculated values of evapotranspiration that are closest to the results of measurement and it is recommended to apply this method for the estimation of reference evapotranspiration.
PB  - Univerzitet u Beogradu - Šumarski fakultet, Beograd
T2  - Glasnik Šumarskog fakulteta
T1  - Kritička analiza savremenih metoda za proračun referentne evapotranspiracije
T1  - Critical analysis of the contemporary methods for estimating reference evapotranspiration
EP  - 70
IS  - 106
SP  - 57
DO  - 10.2298/GSF1206057D
UR  - conv_369
ER  - 

@article{
author = "Đukić, Vesna and Mihailović, Vladislava",
year = "2012",
abstract = "Evapotranspiracija je jedan od najznačajnijih procesa unutar hidrološkog ciklusa, čija pouzdana procena je od suštinske važnosti pri planiranju i upravljanju zemljišnim i vodnim resursima i, od čije veličine direktno zavise potrebe biljaka za vodom. U radu je izvršeno poređenje proračunatih vrednosti referentne evapotranspiracije primenom metode FAO Blaney-Criddle-a, FAO Radijacione metode, metode FAO Penmana i FAO 56 Penman-Montejeve metode sa rezultatima lizimetarskih merenja u Košutnjaku tokom vegetacionih sezona u 2004., 2005. i 2006. godini. Pokazano je da se primenom FAO 56 Penman-Montejeve jednačine dobijaju rezultati najpribližniji rezultatima lizimetarskih merenja, zbog čega se preporučuje primena ove metode pri oceni referentne evapotranspiracije., Evapotranspiration is one of the most important processes within the hydrological cycle whose reliable assessment is essential in the planning and managing of land and water resources. Besides that, the water needs of plants depend directly on the size of evapotranspiration. This paper presents a comparison of reference evapotranspiration values calculated using the FAO Blaney-Criddle method, the FAO Radiation methods, the FAO Penman and the FAO 56 Penman-Monteith method with the results of measurements of evapotranspiration at the meteorological station in Košutnjak during the growing seasons of 2004, 2005 and 2006. It is shown that the application of the FAO 56 Penman-Monteith equation provides the calculated values of evapotranspiration that are closest to the results of measurement and it is recommended to apply this method for the estimation of reference evapotranspiration.",
publisher = "Univerzitet u Beogradu - Šumarski fakultet, Beograd",
journal = "Glasnik Šumarskog fakulteta",
title = "Kritička analiza savremenih metoda za proračun referentne evapotranspiracije, Critical analysis of the contemporary methods for estimating reference evapotranspiration",
pages = "70-57",
number = "106",
doi = "10.2298/GSF1206057D",
url = "conv_369"
}

Đukić, V.,& Mihailović, V.. (2012). Kritička analiza savremenih metoda za proračun referentne evapotranspiracije. in Glasnik Šumarskog fakulteta
Univerzitet u Beogradu - Šumarski fakultet, Beograd.(106), 57-70.
https://doi.org/10.2298/GSF1206057D
conv_369

Đukić V, Mihailović V. Kritička analiza savremenih metoda za proračun referentne evapotranspiracije. in Glasnik Šumarskog fakulteta. 2012;(106):57-70.
doi:10.2298/GSF1206057D
conv_369 .

Đukić, Vesna, Mihailović, Vladislava, "Kritička analiza savremenih metoda za proračun referentne evapotranspiracije" in Glasnik Šumarskog fakulteta, no. 106 (2012):57-70,
https://doi.org/10.2298/GSF1206057D .,
conv_369 .

TY  - JOUR
AU  - Đukić, Vesna
AU  - Mihailović, Vladislava
PY  - 2012
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/420
AB  - U toku suša proticaj na vodotocima je smanjen, i dominira bazni proticaj. Bazni oticaji su karakteristični za malovodne periode i pružaju informacije o raspoloživim vodnim resursima u slivu u toku suše, posebno o osobinama akvifera i retenzionim karakteristikama sliva. Ovaj rad se bavi mogućnošću analize i simulacije komponente baznog oticaja, kao i determinisanjem zakonitosti u njegovim promenama, do kojih se može doći analizom registrovanih hidrograma ukupnog oticaja u dužem vremenskom periodu. Osnova za modeliranje promena baznih oticaja u toku vremena bile su vrednosti baznih oticaja dobijene iz hidrograma ukupnih oticaja primenom grafičke metode lokalnih minimuma. Primenom formiranog modela urađene su simulacije hidrograma baznog oticaja tokom tri karakteristicne godine (kišne -1970., prosečne - 1985. i sušne - 1990) i pokazano je da su odstupanja u odnosu na vrednosti baznih proticaja dobijenih primenom metode lokalnih minimuma u granicama dozvoljenih.
AB  - During the drought the flow in streams is reduced and is dominated by base flow. Baseflows are characteristic of low flow periods and provide information on available water resources in the basin during the drought, particularly on the aquifer and retention basin characteristics. This paper deals with the possibility of analysis and simulation of baseflow, and the determination of the pattern of its changes based on the total registered streamflow hydrograph at the catchment outlet. The basis for modeling the base flow changes in the time were base flow values obtained from the streamflow hydrograph by application of the graphical local minimum method. Applying the simulation model developed in this study, simulations of base flow hydrographs were performed for three characteristic years (1970, 1985, and 1990). It was shown that discrepancies between values of the base flows obtained through application of the local minimum method and the model are within the limits of tolerance.
PB  - Univerzitet u Nišu, Niš
T2  - Facta universitatis - series: Architecture and Civil Engineering
T1  - Analiza režima podzemnih voda na osnovu hidrograma oticaja
T1  - Analysis of groundwater regime on the basis of stream flow hydrograph
EP  - 314
IS  - 3
SP  - 301
VL  - 10
DO  - 10.2298/FUACE1203301D
UR  - conv_586
ER  - 

@article{
author = "Đukić, Vesna and Mihailović, Vladislava",
year = "2012",
abstract = "U toku suša proticaj na vodotocima je smanjen, i dominira bazni proticaj. Bazni oticaji su karakteristični za malovodne periode i pružaju informacije o raspoloživim vodnim resursima u slivu u toku suše, posebno o osobinama akvifera i retenzionim karakteristikama sliva. Ovaj rad se bavi mogućnošću analize i simulacije komponente baznog oticaja, kao i determinisanjem zakonitosti u njegovim promenama, do kojih se može doći analizom registrovanih hidrograma ukupnog oticaja u dužem vremenskom periodu. Osnova za modeliranje promena baznih oticaja u toku vremena bile su vrednosti baznih oticaja dobijene iz hidrograma ukupnih oticaja primenom grafičke metode lokalnih minimuma. Primenom formiranog modela urađene su simulacije hidrograma baznog oticaja tokom tri karakteristicne godine (kišne -1970., prosečne - 1985. i sušne - 1990) i pokazano je da su odstupanja u odnosu na vrednosti baznih proticaja dobijenih primenom metode lokalnih minimuma u granicama dozvoljenih., During the drought the flow in streams is reduced and is dominated by base flow. Baseflows are characteristic of low flow periods and provide information on available water resources in the basin during the drought, particularly on the aquifer and retention basin characteristics. This paper deals with the possibility of analysis and simulation of baseflow, and the determination of the pattern of its changes based on the total registered streamflow hydrograph at the catchment outlet. The basis for modeling the base flow changes in the time were base flow values obtained from the streamflow hydrograph by application of the graphical local minimum method. Applying the simulation model developed in this study, simulations of base flow hydrographs were performed for three characteristic years (1970, 1985, and 1990). It was shown that discrepancies between values of the base flows obtained through application of the local minimum method and the model are within the limits of tolerance.",
publisher = "Univerzitet u Nišu, Niš",
journal = "Facta universitatis - series: Architecture and Civil Engineering",
title = "Analiza režima podzemnih voda na osnovu hidrograma oticaja, Analysis of groundwater regime on the basis of stream flow hydrograph",
pages = "314-301",
number = "3",
volume = "10",
doi = "10.2298/FUACE1203301D",
url = "conv_586"
}

Đukić, V.,& Mihailović, V.. (2012). Analiza režima podzemnih voda na osnovu hidrograma oticaja. in Facta universitatis - series: Architecture and Civil Engineering
Univerzitet u Nišu, Niš., 10(3), 301-314.
https://doi.org/10.2298/FUACE1203301D
conv_586

Đukić V, Mihailović V. Analiza režima podzemnih voda na osnovu hidrograma oticaja. in Facta universitatis - series: Architecture and Civil Engineering. 2012;10(3):301-314.
doi:10.2298/FUACE1203301D
conv_586 .

Đukić, Vesna, Mihailović, Vladislava, "Analiza režima podzemnih voda na osnovu hidrograma oticaja" in Facta universitatis - series: Architecture and Civil Engineering, 10, no. 3 (2012):301-314,
https://doi.org/10.2298/FUACE1203301D .,
conv_586 .