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Упит dcterms_subject_txt:the Velika Morava River

661 items

  • Anthropogenic impact on the groundwater regime: Case study of the Velika Morava alluvium

    Jovana Mladenović, Vesna Ristić Vakanjac, Milan Kresojević, Boris Vakanjac, Jugoslav Nikolić, Dušan Polomčić, Dragoljub Bajić (2023)
    The Velika Morava River originates at the junction of the Južna Morava and Zapadna Morava at the town of Stalać in Serbia. It is 185 km long and empties into the Danube. The Velika Morava River Basin occupies a land area of 37 444 km2. The river flows through central Serbia, which features the most fertile land and the highest population density in the country. Public water supply in this region of Serbia relies on groundwater formed in alluvial ...
    hydrology, surface water regime, groundwater regime, the Velika Morava River

  • Проширивање мреже пловних путева Републике Србије у функцији одбране земље

    Милан Кресојевић, Весна Ристић Вакањац, Драган Трифковић (2023)
    Мрежу пловних путева Републике Србије чини мрежа међународних и међудржавних пловних путева. Међународне пловне путеве чине реке Дунав, Сава, Колубара, Дрина, Канал Дунав-Тиса-Дунав (Д-Т-Д) „Нови Сад – Савино село“ и Беочински рукавац – канал, док међудржавни пловни пут на коме важи међународни режим пловидбе чини река Тиса. Поред наведених пловних путева који већим делом обухватају територију Аутономне покрајине Војводине, Република Србија има потенцијал проширења мреже пловних путева и у централном делу Србије пре свега у Поморављу. Проширењем мреже пловних ...
    унутрашњи пловни пут, Велика Морава, одбрана земље, бродови Речне флотиле

  • Impact of river bank filtration on alluvial groundwater quality: A case study of the Velika Morava River in central Serbia

    Branislav Petrović, Vladimir Živanović (2016)
    филтрација кроз обалске и седименте речног корита, алувијални седименти, прихра- њивање подземних вода, квалитет подземних вода, Велика Морава

  • The Effect of Gravel and Sand Mining on Groundwater and Surface Water Regimes — A Case Study of the Velika Morava River, Serbia

    Milan Kresojević, Vesna Ristić Vakanjac, Dragan Trifković, Jugoslav Nikolić, Boris Vakanjac, Dušan Polomčić, Dragoljub Bajić (2023)
    Овај рад описује како неконтролисано и нелегално откопавање песка и шљунка може утицати на режим површинских и подземних вода на местима где постоји активна хидрауличка веза између њих, са студијом случаја реке Велике Мораве у Србији. Такође, промена геометрије попречног профила, као последица антропогених и природних фактора, отежава уливање ове реке за укључивање у водне токове Србије. Плодност Велике Мораве омогућила би развој речног саобраћаја како за трговачке бродове, тако и за пловила Речне флотиле Војске Србије. Корелације између ...
    експлоатација песка и шљунка, режим површинског тока, режим подземних вода

  • Kvantitativni status podzemnih voda aluvijona Velike Morave (potez Bagrdan - ušće)

    Jovana Mladenović, Milan Kresojević, Dušan Polomčić, Dejan Đorđević, Boris Vakanjac, Jugoslav Nikolić, Vesna Ristić Vakanjac (2023)
    Велика Морава настаје спајањем Јужне и Западне Мораве код Сталаћа и њена дужина тока од формирања до ушћа у Дунав износи 185 км. Укупна сливна површина ове реке заједно са њеним саставницама износи од 37.444 км2 што је територијално око 42% Републике Србије чинећи ову реку њеним главним дреном. Протиче централним делом Србије, најплоднијим земљиштем као и најгушће насељеним деловима наше земље. Добра хидрауличка веза вода Велике Мораве и подземних вода утицале су на то да у оквиру алувијона ...
    режим подземних вода, хидрауличка веза површинских и подземних вода, алувијон, Велика Морава

  • Impact of river bank filtration on alluvial groundwater quality – a case study of the Velika Morava River in central Serbia

    Petrović Branislav, Živanović Vladimir (2015)

  • Analiza uslova formiranja oticaja reke Resave (istočna Srbija)

    Vesna Ristić Vakanjac, Marina Mitrašinović, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Branislav Petrović, Petar Vojnović (2023)
    Reka Resava zbog veličine sliva i količine vode koju daje Velikoj Moravi predstavlja jednu od najznačajnijih njenih desnih pritoka. U okviru njenog sliva jasno se izdvajaju gornji, geomorfološki raznolik deo sliva, koji je uglavnom izgrađen od karbonatnih sedimenata, i donji deo koji pripada Velikomoravskom basenu. Proticaj reke Resave se beleži u profilima Manastir Manasija koji kontroliše gornji deo sliva u iznosu od 358 km2 i Svilajnac, koji se nalazi na oko 3.5 km pre njenog ušća i koji kontroliše ...

  • Karst aquifer impact on the formation of surface runoff: case study of the Resava River catchment, Serbia

    Marina Mitrašinović, Vesna Ristić Vakanjac, Veljko Marinović, Saša Milanović, Ljiljana Vasić, Dušan Polomčić (2022)
    The paper compares the flow regimes of the Resava River at the gauging stations of the Manasija Monastery (upper course) and the town of Svilajnac (lower course). The hydrological analysis encompasses a multiyear period of monitoring (1982–2020). The water budget and baseflow index are assessed for the catchment areas monitored by the Svilajnac station (683 km2) and the Manasija Monastery station (358k m2), considering the overall monitoring period and characteristic years. The results indicate that the specific runoff in ...
    hydrogeological characteristics, water regime, water balance, karst aquifer, Resava catchment area
    ... Resava catchment area. Introduction The Resava catchment is in the northern part of East- ern Serbia, between the Velika Morava River and the slopes of the Kučaj-Beljanica Mountains. The Resava River originates at the junction of the Zlots- ka River and the Karapandžin Creek at an altıtude of ...
    ... is 93 m. The upper catchment of the Resava is a composite valley comprised of gorg- es, ravines, and canyons (mostly karst), which cn- ters the Velika Morava River Basin near the town of Despotovac (Paunković, 1953). The upper Resava runs from the village of Strmosten in the west and ('C BbjirapcKo ...
    ... tributary ofthe Velika Morava (Dukić, Gavrilović, 2014). The total length ofthe Resava is 65.5 km and its catchment area (ac- cording to the National Hydrometeorological Scr- vice) is 681 km?. It generally flows in the SE-NW direction, all the way to its mouth near Svilajnac, where the clevation is ...

  • Prilog poznavanju režima i bilansa voda reke Resave

    Marina Mitrašinović, Vesna Ristić Vakanjac, Saša Milanović, Ljiljana Vasić, Dušan Polomčić (2022)
    Sliv Resave zauzima područje između reke Velike Morave i obronaka Kučajsko-beljaničkih planina. Sliv i režim ove reke kontroliše se dvema hidrološkim stanicama: Manastir Manasija (slivno područje u iznosu od 388 km2) i Svilajnac (681 km2). Za potrebe analize režima voda reke Resave i uticaja padavina na formiranje oticaja sa njenog sliva preuzeti su podaci o padavinama sa meteorološke stanice Crni Vrh (1037 m nm) koji odslikava režim gornjeg dela sliva ove reke, i meteorološke stanice Smederevska ...
    Hidrogeološke karakteristike, hidrološke karakteristike, režim voda bilans voda, rijeka Resava

  • Seasonal Variations of the Zapadna Morava River Water Quality

    Nebojša Đ. Pantelić, Jana S. Štrbački, Goran Marković, Jelena B. Popović-Đorđević (2021)
    The water samples collected from four localities of the middle course of the Zapadna Morava River during 2020 were analyzed via the selected physicochemical parameters with the aim to estimate the quality of surface water. According to the results of selected physico-chemical parameters (pH, conductivity, dissolved oxygen, chemical oxygen demand, biochemical oxygen demand), analyzed surface water show a good chemical status, while the values of nutrient content (nitrate, nitrite, ammonium ion, total phosphorus) indicated the poor chemical status especially ...
    water quality, dissolved oxygen, ammonium ion, total phosphorus

  • Kvantitativna ocena režima i bilansa podzemnih voda u aluvijonu Velike Morave od Bagrdana do ušća u Dunavu

    Aleksandar Balubdžić (2024)
    Aluvijalni sedimenti velikih reka raspolažu značajnim količinama podzemnih voda, što je zajedno sa površinskim vodama dozvolilo razvoj naselja i ljudskih aktivnosti. Ovaj razvoj uslovljava veće potrebe za vodnim resursima i njihovim kvalitetom. Sa povećanjem eksploatacije podzemnih voda, uticaj iste je značajniji i može da dovede do opadanja nivoa podzemnih voda i pogoršanja kvaliteta. Aluvijon Velike Morave ima značajno rasprostranjenje, usled čega predstavlja važno ležište izdanskih voda sa velikim eksploatacionim mogućnostima. Izradom hidrodinamičkog modela aluvijona Velike Morave od Bagrdana do ...
    režim podzemnih voda, bilans podzemnih voda, intergranularna izdan, hidrodinamički model
    ... Polomčić, D., Čokorilo Ilić, M., Bajić, D., Kresojević, M. (2019). Surface water flows as impacted by sand and gravel minig: Case study of the Velika Morava river, Serbia. In: 7 International Symposium "Mining and Environmental Protection (str. 203-210). Beograd: Rudarsko-geološki fakultet, Univerzitet ...
    ... području aluvijona Velike Morave od Bagrdana do ušća u Dunavu, najvažniju ulogu imaju površisnki tokovi, pre svega Velika Morava koja se proteže dužinom celog modela, kao i Dunav na severnom delu područja. Njihov uticaj na modelu je simuliran graničnim uslovom reka (eng. „river“). Smer kretanja vode ...
    ... hidrološke karakteristike istražnog područja Velika Morava nastaje spajanjem Zapadne i Južne Morave kod Stalaća ı predstavlja najveću reku koja pripada Srbiji. Istočno od Smedereva uliva se u Dunav. Dužina Velike Morave je 245 km, dok dužina dela Velike Morave koji obuhvata istražno područje iznosi ...

  • Hydrographic and hydrological characterization of the Vodenička and Rosomačka rivers

    Vesna Ristić Vakanjac, Marina Čokorilo Ilić, Dušan Polomčić, Dragoljub Bajić, Jelena Ratković (2017)
    The Visočica River rises in Bulgaria, on the Berovo Mountain. Its course in Bulgaria is 16.7 km long. It enters Serbia near the village of Donji Krivodol. Up to the village of Pakleštica, or the beginning of Lake Zavoj, its right-bank tributaries are the Krivodolštica, the Vodenička, the Rosomačka and the Dojkinačka. There are no left-bank tributaries. Among the tributaries, water levels and discharges are gauged only on the Dojkinačka River. The Vodenička had also been gauged but only ...
    hydrographic characteristics, river discharge, the Vodenička River, the Kamenička River
    ... 138‰; - The Caričin Creek: 168 ‰; - The Rosomačka, from the source of the Zanoška to the mouth (junction with the Visočica): 47‰. The Vodenička River rises at an elevation of 1384 m.a.s.l., at the union of the Jelov Dol and the Studena Bara. It empties into the Visočica between the villages of ...
    ... and the catchment is between the watersheds of the Jelovica River, which is the main right-bank tributary of the Dojkinačka (west) and the Vodenička (east). They are separated from the Dojkinačka and the immediate catchment of the Visočica by a water divide which runs, from the south to the east ...
    ... Пиротски зборник 42 (2017) 1-24 7 - The Vodenička River, from mouth to origin (union of the Jelov Dol and the Studena Bara): 33‰, - The Jelov Dol: 83‰, - The Studena Bara: 79‰, - The Vodenička River, from the source of the Jelov Dol to the confluence with the Visočica: 42‰. 600 700 800 900 ...

  • Seizmo-tektonske karkteristike terena između Velike Morave i Drine : I tekstualni deo

    Milorad Vukašinović (1970)
    Seizmo-tektonika,Velika morava, Drina

  • Hidrogeološke karakteristike aluvijalnih naslaga i oboda Velike Morave sa aspekta mogućnosti iskorišćenja izdanskih voda

    Dušan Stojadinović (1992)
    Hidrgeologija, aluvijalne naslage, izdanske vode, Velika Morava

  • Hidrogeologija tercijarnih basena u slivu Velike Morave sa osvrtom na mogućnosti vodosnabdevanja

    Petar Dokmanović (1992)
    Hidrogeologija, vodosnabdevanje, tercijar, Morava

  • Heavy metals in lignite and soil of Kostolac-Kovin coal basin, eastern Serbia - comparative analysis with selected cities in Serbia, region, Europe and world

    Bogoljub Vučković, Bojan Dimitrijević (2023)
    The Kostolac-Kovin coal basin with an area of 320 km2, with 5 separate layers of coal and with a total of about 5.7 Bt of geological resources and reserves represents an exceptional potential for coal production in Serbia. The coal resources listed in this way are not fully exploitable, but they represent potential for consideration. In this paper, we deal with the geochemical characteristics of coal seams and perform a comparative analysis of coal affectation on the environment. With ...
    lignite, heavy metals, concentrations
    ... compare with the concentrations in our lignite. In the following chapters we will deal with this issue. Key Words: lignite, heavy metals, concentrations 1. GENERAL INFORMATIONS The coal basin is located in castern Serbia, between the Velika Morava and Mlava rivers, which flow into the Danube in ...
    ... Figure 2. General overview of exploration wells (black dots) for the period 1941-2022. years in the Kostolac-Kovin coal-bearing basin, blue thick line — river Danube, blue thin line left – river Pelika Morava, blue thin line center — river Mlava, gray circle - uhderwater mining of Kovin lignite 178 ...
    ... 7. Presentation of the content of Zn, Pb and Cu in the urban, recreational and industrial top soil in the cities of the region; yellow – I, II and II Kostolac coal, black - the most polluted soil Figure 7 shows that the contents of Zn, Pb, Cu in the top soil in the cities of the region behave almost ...

  • Palaeoflora of Kamenica (Pranjani Basin, western Serbia)

    Zorica Lazarević, Ljubica Milovanović, Jelena Milivojević, Ivana Vasiljević (2019)
    Palaeofloras of the Paleogene in Serbia are relatively rare, especially in comparison with floras from Neogene sediments. Most Paleogene phytoas sociations from the territory of Serbia existed in a dry and warm climate. The youngest Paleogene phytoassociation originates from the Pranjani Basin (Western Serbia), locality Kamenica. The age of this palaeoflora is determined as Late Oligocene. This fossil plant assemblage is different from other Paleo gene phytoassociations.The palaeoflora from Kamenica is characterized with leaf imprints larger than in other ...
    макрофлора, млађи олигоцен, Прањански басен, Каменица
    ... from the same sediments. Based on fossil fish finding and comparison with other similar early Miocene floras, the deposits of the first horizon probably correspond to the upper parts of the Late Oligocene-early Miocene. The Zapadna Morava Gra ben, also known as the Čačak-Kraljevo Basin, is the largest ...
    ... some of Ne–SW trends, controlled the formation of the Graben and its geometry. a characteristic of the Zapadna Morava Graben is the large subsidence of the Ottnangian-Karpatian, probably superposed upon similar movements of the Oligocene-Miocene. The central Graben sank the most, over a relatively wide area ...
    ... geological setting The Pranjani Basin is part of the West Morava Graben (also known as the Čačak-Kraljevo Basin). Located on the northwestern border of the Ča čak- Kraljevo Basin, the Pranjani Basin covers an area of 45 km2 and is elongated in an east-west direction (Fig. 1). On the southeast it is limited ...

  • Tectonothermal evolution of an asymmetric extensional system: the Juhor Mts in Central Serbia (Northern Serbomacedonian massif)

    Miloš Radonjić, Uroš Stojadinović, Elco Luijendijk, Dejan Radivojević, Željko Golubović, Nikola Vuković (2018)
    асиметрична екстензија, панонски басен, српско‐македонски масив, термохронологија
    ...  Quaternary  sediments  of  the  southernmost  Pannonian  Basin.  The  Juhor Mts,  together with  other  uplifted  areas  along  the Morava  river  corridor,  such  as  Crni  Vrh, Mojsinjske Mts,  Poslonske Mts,  comprise  part  of  northern  Serbomacedonian  Massif.  The  Serbomacedonian  Massif  is  ...
    ...  Miocene deposition of the Morava depression  (the Morava detachment,  see Sant et al., 2016). Subsequent Pliocene  to Quaternary  inversion of  the  Pannonian Basin resulted in further differentiation between uplifted and subsided tectonic blocks along  southern margin of the basin.  253  ЛИТЕР ...
    ... etachments at the contact between the Carpathians and Dinarides—the  Jastrebac Mountains of Central Serbia. Tectonophysics 710–711, 162–183.  Matenco, L., Radivojević, D., 2012. On  the  formation and evolution of  the Pannonian Basin: Constraints derived  from  the  structure of  the  junction are ...

  • Ecological status of the Lim river alluvium in Serbia

    Amel Kurbegović, Boris Vakanjac, Vesna Ristić Vakanjac, Mirjana Bartula, Zorana Naunović, Nikola Milovanović, Jovan Kovačević (2022)
    Three countries share the catchment of the Lim River and they have been engaged in an eco-logical struggle for years, to conserve the river, its tributaries, and biodiversity. Honoring international conventions and declarations, along with active involvement of the civil society and support of Eu-ropean Union agencies, major efforts are being made to draw attention to the degradation of nature, especially water, which is essential for life on the planet Earth. Considering that natural resources are limited and that ...
    aluvijum, zagađenje vode, ekološki status, reka Lim

  • Age And Mode of the Middle Miocene Marine Flooding of the Pannonian Basin—Constraints from Central Serbia

    Oleg Mandic, Ljupko Rundić, Stjepan Ćorić, Ðurðica Pezelj, Dörte Theobalt, Karin Sant, Wout Krijgsman (2019)
    The timing and mode of the marine flooding of the southern margin of the Pannonian basin in SE Europe is still a matter of debate. In central Serbia, integrated bio-magnetostratigraphic data and quantified high-resolution records are completely missing. Here, we provide paleoenvironmental and paleoecological constraints from the Slanci section located near Belgrade that has an excellent preservation of micro-fauna and flora, i.e., planktonic and benthic foraminifera and calcareous nannoplankton. We integrate their quantified records with sedimentological, natural gamma radioactivity ...
    Srednji miocen, morska transgresija, Panonski basen, područje Beograda