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Упит dcterms_subject_txt:the Velika Morava River

665 items

  • The Importance of Geotechnical Investigations for the Construction of Transfer Station „Prelići“ on Landfill in Cacak – Serbia

    Dragoslav Rakić, Irena Basarić, Jovana Janković, Tina Đurić (2019)
    For the purpose of the facilities construction within the transfer station „Prelici“ in Cacak, specific geotechnical investigations were carried out based on which the technological project with the facilities schedule was developed. Significant deviations in relation to the presented results were determined during earthworks, so the additional geotechnical investigation works were carried out. Since the new investigation works have determined a different cross section of the terrain, it was proposed to move the planned facilities which led to the ...
    landfill, geotechnical investigations, transfer station
    ... become the integral part of the inhabited area. The landfill covers an area of about 13.5 ha, and the estimated volume of disposed waste is about 1800000 m3. The landfill is formed in alluvial plane of the left valley side of the West Morava River, i. e. left valley side of the Atenica River, which ...
    ... eastern border of the landfill and which flows into the West Morava River in the landfill zone. Unfortunately, this is a very common case in many municipalities in Serbia, where city landfills are located next to the rivers or in their vicinity (Rakic, 2013). Until 1994 at the city landfill „Prelici“ ...
    ... waters in the terrain), as well as by the occasional rise in the groundwater level. Figure 3. Characteristic geotechnical cross sections of the terrain at the location of the transfer station In the central part of the landfill itself, which is outside the planned construction zone of the transfer ...

  • Stratigraphic implications of the Mio-Pliocene geodynamics in the area of Mt. Avala: new evidence from Torlak Hill and Beli Potok (Belgrade, Serbia)

    Ljupko Rundić, Meri Ganić, Slobodan Knežević, Dejan Radivojević, Miloš Radonjić (2019)
    Mt. Avala is located on the southern margin of the Pannonian basin (SPB), a border zone between the uplifted morphostructures of the Dinarides and Carpathian-Balkanides. Similar to the Pannonian basin, tectonostratigraphic evolution of the Mt. Avala area during the last 23 Ma has is characterized by syn- and post-rifting processes as well as tectonic inversion. Here, we present the results of field investigations of the Miocene‒Pliocene dynamics that led to different spatial positions of the same stratigraphic units (e.g. ...
    мио-плиоценска геодинамика, јужни Панонски басен, Авалски и Торлак хорст, Белопоточки трог, Србија
    ... to the Sopot and Stojnik in the south (MAROVIĆ & KNEŽEVIĆ, 1985; MAROVIĆ et al., 2007). The Avala horst is oriented almost meridionally, and it is constrained on all sides by extensional faults related to the syn-rift phase of which the most striking are those towards the Velika Morava trough (MAROVIĆ ...
    ... parts of the Velika Morava trough (MAROVIĆ & KNEŽEVIĆ, 1985; DJOKOVIĆ & MAROVIĆ, 1990; MAROVIĆ et al., 2007 – see Fig. 17). Later, during the Pontian, the Beli Potok trough was reduced and directed to the east, towards the Grocka-Sme- derevo area (MAROVIĆ & KNEŽEVIĆ, 1985; see Fig. 17). From a ...
    ... same age were drilled in the Grocka depression (the local peripheral structure of the Velika Morava trough) at depths between 1000 and 1100 m, i.e. between 900 and 1000 m absolute altitude (KNEŽEVIĆ et al., 1994). This means that in the study area the significant vertical movements began in post-Badenian ...

  • Fault type assessment based on vertical gravity gradient anomalies – advantages and limitations

    Ivana Vasiljević, Snežana Ignjatović, Branislav Sretković (2024)
    The type of dip-slip faults can be assessed based on the analysis of vertical gravity gradients. Theoretically, just a simple comparation of the gradient extreme values can give us an answer whether the fault is normal or reverse (thrust). Practical application of this method is far more complicated and the results depend on a number of parameters, such as a complexity of geological setting, the quality of gravity data, dip angle and displacement of the fault, density contrast, etc. ...
    dip-slip faults, vertical gravity gradients, field data analysis
    ... [] ? 4 6 8 10 12 14 South Morava x [km] Fla FIb F2a F2b River F3 F4 i i vi < VOA - K i (b) s VOA V X V a \ c u Figure 3. Field example from South Morava trench: (a) vertical gravity gradient (Uzz) curves A, B and C and (b) disposition of the faults obtained from geological data (red dashed ...
    ... application of the method can be much more challenging. FIELD EXAMPLE A profile across the South Morava trench, near Brestovac in eastern Serbia, was chosen as a field example (Fig. 3). First, the gravity anomalies werc calculated for the wider area around the profile and then residual anomalies ...
    ... JIEJIHMITIA: HCTHMBAĐA – AKVMMJIALIHJA KAJIMHMAHILIIH Hukoana /luvos6 u 4nekcaHdap Kapajo8aHOcKU a 197 GEOLOGICAL-ENGINEERING ASPECTS OF THE VJOSA RIVER DELTAIC PLAIN Majlinda Mecaj O aaiaaaaaaananaanoı 211 FEOTEXHMHUKH HCTPA)KHMH PABOTH HA VCEK II(xM 11+240-11+460) HA TIIPYFA KVMAHOBO-BEJbAKOBIIE ...

  • Režim pogranične reke Jerme

    Vesna Ristić Vakanjac, Marina Čokorilo Ilić, Dušan Polomčić, Dragoljub Bajić, Boris Vakanjac, Peđa Kostić (2019)
    Reka Jerma izvire na Vlasinskoj visoravni u zoni Vlasinskog jezera, teče prema severozapadu padinama planine Gramade kroz selo Klisuru. Kod sela Strazimirovci prelazi u susednu državu Bugarsku, prolazi kroz Trnovsko ždrelo i zatim se ponovo vraća u Srbiju nedaleko od sela Petačinci. Uliva se kod sela Gradište u Nišavu. Ukupna dužina ove reke je 72.1 km od toga je 45.1 km formirala na teritoriji Srbije a preostali deo pripada Bugarskoj. Posmatrajući površine sliva nešto manje od 50 % pripada ...
    klimatske promene, režim reke, monitoring, međugranična saradnja, Jerma

  • Idejno rešenje zaštite površinskog kopa Zapadni Kostolac od površinskih i podzemnih voda

    Željko Savić (2024)
    Svaki veći površinski kop ima dobro razvijene etaže, pa samim tim i veće površine na koje dospe površinska voda, koju je potrebno prikupiti i dirigovano provesti do odgovarajućih recipijenata, kako ne bi ugrozila eksploataciju otkrivke i uglja.
    odvodnjavanje, kanali, vosabirnici, bunari, ekrani
    ... vodosnabdevanja domaćinstava u seoskim naseljima i privrednih subjekata. Velika Morava i Dunav su hidraulički povezani sa ovom izdani. Generalni pravac strujanja podzemnih voda je jug-sever, odnosno paralelno sa tokom Velike Morave, s obzirom da, na severu, Dunavac, sa kotom 67 mnm, predstavlja erozioni ...
    ... Meminac i Ključ grada Požarevca. Jelika Morava i Dunav Za analizu nivoa reke Velike Morave na istražnom prostoru, od ušća u Dunav do okvirno km 26, korišćeni su podaci za period od 1952 do 2015.god. Generalno se može konstatovati da je nivo vode u Velikoj Moravi (posmatrano na profilu h.s Ljubičevski ...
    ... filtracije većim od ovog, odvodnjavanje je ili nemoguće ili nije ecekonomski opravdano i da pliokvartarne peskove, s obzirom na filtracione karakteristike, možemo odvodnjavati sistemima bunara. Imajući u vidu gore navedence kriterijume i blizinu graničnih uslova (reka Velika Morava, Dunav, Dunavac ...

  • Stanje i perspektivnost vodosnabdevanja Obrenovca i naselja opštine posle poplava, 2014. godine

    Bojan Hajdin, Dušan Polomčić, Dragoljub Bajić (2017)
    Obrenovac i okolna naselja su tokom 2014. godine zbog poplava u Srbiji pretpeli veliku materijalnu štetu, a pored brojnih privrednih preduzeća ozbiljno je bio ugrožen i sistem vodosnabdevanja. Izvorište „Vić bare“ za vodosnabdevanje grada u selu Zabrežje, na Savi, u potpunosti je potopljeno, a vodovodna mreža, u pojedinim delovima već veoma stara, dodatno je oštećena. Poslednjih nekoliko decenija kao glavni razlozi za probleme u vodosnabdevanju Obrenovca isticane su nedovoljne rezerve podzemnih voda na izvorištu. Novijim istraživanjima utvrđene su rezerve ...
    ... PROSPECTS AFTER THE 2014. FLOOD In 2014, major floods in Serbia caused enormous damage in Obrenovac Municipality. Apart from nu- merous businesses, the flood affected the water supply system. The water source “Vić Bare” in the village of Zabrežje on the Sava river was inundated and the water distribution ...
    ... water use and water losses in the distribution network. Given that the said water source relies on bank filtration, the flood was extremely important from a hydrogeological perspective. The paper assesses the data collected during the course of extremely high river stages and water tables and examines ...
    ... Hajdin K. State of art of Vić Bare Source for Obrenovac Water Supply. Regional IWA Conference on groundwater management in the Danube river basin and other large river basins, Beograd pp. 217-225, 2007. [6] Hajdin B, Polomčić D, Stevanović Z, Bajić D, Hajdin K. Ocena perspektivnosti izvorišta ...

  • Hidrodinamički proračun zaštite površinskog kopa Drmno od podzemnih voda u periodu 2018-2022. godina

    Dušan Polomčić, Tomislav Šubaranović, Zoran Stojićević (2019)
    Površinski kop lignita Drmno nalazi se u blizini velikih reka (Dunav i Mlava), zbog čega eksploatacija otkrivke i lignita u velikoj meri zavisi od sistema zaštite od podzemnih voda. Ukoliko je sistem zaštite od podzemnih voda dobro isplaniran, a njegov kapacitet dobro proračunat, onda će se eksploatacija obavljati u suvoj sredini, što podrazumeva sigurnu proizvodnju otkrivke i lignita. U današnje vreme uz primenu adekvatnih softvera olakšano je kvalitetno planiranje i proračunavanje sistema za zaštitu površinskih kopova od podzemnih voda. ...
    odvodnjavanje, podzemne vode, površinski kop, lignit, Drmno

  • Старење бунара у алувијалним срединама различитог степена оксичности

    Brankica Majkić (2013-09-27)
    Старење бунара настаје као последица процеса корозије и колмирања. Процесекорозије могуће је спречити уградњом филтерских конструкција од материјалаотпорних на корозију. Колмирање може да настане без обзира на врсту материјалаод кога се праве бунарске конструкције, а процесом може бити захваћенаприфилтарска зона па и зона саме водоносне средине. Из тог разлога тезa јеусмеренa на процесе који доводе до колмирања бунара и последицe опадањaкапацитета водозахватних објеката. Полазна хипотеза је да бунари стареразличитом брзином у срединама различитог степена оксичности. Хидрохемијскеи микробиолошке карактеристике подземних ...
    старење бунара, алувијалне издани, степен оксичности средине,колмирање, бунарски талог, локални хидраулички губитак, дозвољене улазнебрзине
    ... (2007): State and problems of using alluvial water in Great Morava valley, Proceedings Regional IWA conference on Groundwater management in the Danube river basin and other large river basins, 7-9 June 2007, „Jaroslav Černi“ Institutefor the development of water resources, Belgrade, p. 201-208 19 ...
    ... мрежу чине река Велика Морава и њене притоке. Велика Морава настаје спајањем Јужне и Западне Мораве. Њено укупно сливно подручје износи скоро 38.000 km 2 , што представља близу 40% површине Републике Србије. Сама Велика Морава има сливно подручје површине око 6.800 km 2 . Велика Морава по својим ...
    ... results. The drainage wells of the Kovin-Dubovac system collect anoxic groundwater featuring elevated iron concentrations and low sulfate levels. The aquifer is under the direct influence of the surface water regime of the Danube River, whose stages govern the discharge rates of the drainage ...

  • Hidrološki i hidraulički mehanizam isticanja vrela Rijeka Crnojevića

    Golub Ćulafić, Veljko Marinović, Branislav Petrović, Jelena Krstajić (2022)
    Rijeka Crnojevića predstavlja karstno (kraško) vrelo, koje u teritоrijalnom pogledu pripada Opštini Cetinje, u gеоlоškо-tеktоnskоm pоglеdu pripаdа zоni Visоkоg kršа (оblаst stаrе Crnе Gоrе), dоk prema hidrogeološkoj rejonizaciji spаdа u prоstоr Spoljašnjih Dinarida. Izvire iz Obodske (ili Crnojevića) pećine u selu Obod (81 m.n.m.). Voda koja ističe iz Obodske pećine vodi porijeklo od atmosferskih voda, koje se formiraju na prostoru Cetinjskog polja i Dobrskog sela. Vоdе nа оbоdu pоljа pоniru i kreću se uglаvnоm podzemnim kаvеrnаmа i kаnаlimа, nаstаlim ...
    Riјеkа Crnoјеvićа, karstnо vrelo, mehanizmi isticanja

  • Flood protection and water utilization of karst poljes: example of Gatačko Polje, Eastern Herzegovina

    Tina Dašić, Ljiljana Vasić (2020)
    Earth-Surface Processes,Geology, Pollution, Soil Science, Water Science and Technology, Environmental Chemistry,Global and Planetary Change

  • Ocena kvaliteta i mogućnost korišćenja podzemnih voda za piće i navodnjavanje u slivu reke Ralje

    Sunčica Ninković, Nebojša Atanacković, Sava Magazinović, Jakov Andrijašević, Mihailo Šević (2016)
    Analiza mogućnosti korišćenja podzemnih voda za potrebe vodosnabdevanje stanovništva kao i za navodnjavanje vršena je na prostoru sliva reke Ralje. Istražni prostor veličine oko 280 km2 je obuhvatio veći deo sliva reke Ralje koji se administrativno nalaze na području grada Beograda. Podzemne vode su glavni izvor za vodosnabdevanje i navodnjavanje u ovom području. Seoska naselja nemaju urađenu komunalnu infrastrukturu pa predstavljaju značajan faktor za degradaciju kvaliteta podzemnih voda na ovom području. U periodu 2012-2014 godine prikupljeno je 100 uzorka ...
    kvalitet voda, hidrohemijski parametri, navodnjavanje, zagađenje, reka Ralja

  • Хидрогеохемијске карактеристике и квалитет вода слива Требишњице, Република Српска, Босна и Херцеговина

    Dragoslav R. Banjak (2016-08-25)
    Упркос неповољном временском и просторном распореду, воде су најзначајнијиприродни ресурс Источне Херцеговине. Ова чињеница довела је до реализацијепројекта „Вишенамјенског хидросистема Требишњица“, којим је, премаМилановићу (2006), до сада обухваћено: седам хидроелектрана, шестакумулација, шест брана, шест тунела укупне дужине 59,7 km, неколикоприступних тунела, 62,5 km бетонског канала кроз Попово поље, канал крозДабарско (6750 m) и Фатничко поље (2770 m) и систем тунел-канал или цјевоводпрема Дубравама.У почетку са доминантним енергетским предзнаком, концепција јетрансформисана у интегрално рјешење вишенамјенског коришћења и заштитевода и животне ...
    хидрогеохемијски процеси, мултиваријантна статистичкаанализа, инверзно геохемијско моделовање, квалитет воде, употребиљивост водеза наводњавање, слив Требишњице
    ... between swallow holes the Trebišnjica river and the spring Omble, between swallow holes the Mušnica and the spring of the Trebišnjica river and in accumulation Gorica which is a place of mixing water from water accumulation Bileća, the river Sušica and the spring in Lastva. The results of modelling ...
    ... down the wastewater treatment plant and in the lower flow of the Mušnica river. The irrigation suitability of water in the river Trebišnjica catchment referring to the chemical composition is not balanced. To Allison's et al. classification (Allison et al, 1954) which is based on the value of ...
    ... modelling based on the example the Trebišnjica-Ombla showed that the mineral dissolution is the dominant hydrogeochemical process between the initial and final water and that's why open system is convenient to CO2. The spring of the Trebišnjica river shows modifying impact of Bileća accumulation on ...

  • Tectonic evolution of the Vršac Mts. (NE Serbia): Inferences from field kinematic and microstructural investigations

    Uroš Stojadinović, Nemanja Krstekanić, Bojan Kostić, Marija Ružić, Aleksa Luković (2021)
    The Vršac Mts. in NE Serbia represent the key area to investigate structural relations between the Northern Serbo-Macedonian Subunit and Supragetic Unit of the Dacia Mega-Unit. The geodynamic events during the Variscan orogeny in the Late Paleozoic colligated the two units and led to their metamorphic differentiation. The Late Cretaceous extension exhumed the medium-grade Serbo-Macedonian metamorphic rocks and structurally juxtaposed them against the low-grade metamorphosed basement of the Supragetic Unit along an E-dipping shear zone, which outcrops in the ...
    severna srpsko-makedonska subjedinica, supragetikum, kinematska analiza, multifazna ekstenzionalna deformacija
    ... northernmost outcrops in the Pannonian Basin (i.e., the Vršac Mts.) to the southern termination of the Morava Valley Corridor (Fig. 1b). The Central Serbo- Macedonian Subunit outcrops south of the Morava Valley Corridor, in south-eastern Serbia, Bulgaria and North Macedonia, while the Southern Serbo-Macedonian ...
    ... between the Vršac Mts. and the Jastrebac Mts., are still buried beneath the Neogene sediments along the Morava Valley Corridor (Fig. 1b). The final tectonic uplift of the Vršac Mts. occurred in middle to late Miocene times along the SW- dipping normal faults that control deposition in the Zagajica ...
    ... South of the Vršac Mts., in the Morava Valley Corridor (Fig. 1b) such exhumation was hampered by the presence of the rigid Moesian Platform indenter (see Krstekanić et al. 2020). In this southern prolongation of the Pannonian Basin, the E–W oriented extension was governed by the retreat of the Dinaridic ...

  • Pokazatelji recentne tektonske aktivnosti u speleološkim objektima Dževrinske grede (istočna Srbija)

    Ana Mladenović, Jelena Ćalić (2022)
    Sistem Timočkog raseda predstavljen je sistemom desnih transkurentnih raseda generalnog pružanja sever – jug, koji su bili aktivni u periodu oligocena i miocena u okviru Karpato-balkanskog orogena. Početak njihove aktivnosti vezuje se za rotaciju tektonskih jedinica Karpato-balkanida (Dacia Mega Unit) oko rigidne Mezijske jedinice. Aktivnost ovih transkurentnih raseda je akomodirala ovu rotaciju, pa se smatra da je kumulativno kretanje duž Timočkog raseda tokom perioda njegove aktivnosti bilo do 100 km. Usled kompleksnih tektonskih rotacija, rasedi ovog sistema doveli su ...
    Тимочки расед, Џеврински расед, Балта расед, спелеолошки објекат

  • Exhumation history of the Juhor Mts. in central Serbia, the Northern Serbo–Macedonian Subunit

    Uros Stojadinovic, Hannah Pomella, Nemanja Krstekanić, Bojan Kostić, Maja Maleš, Nikola Randjelovic, Miloš Radonjić (2024)
    Northern Serbo–Macedonian Subunit, low-t thermochronology, kinematic analyses, extensional deformations

  • Оцена перспективности изворишта "Вић баре" за водоснабдевање Обреновца

    Бојан Хајдин, Душан Поломчић, Зоран Стевановић, Драгољуб Бајић, Катарина Хајдин (2012)
    ... Urban development of the Obrenovac city (30 km west from Belgrade) and plan to connect smaller settlements to the main waterworks system have initiated hydrogeological research and creation of hydrodynamical model of the exisiting source ,,Vié bare“ located in Sava River alluvium. The source consists of ...
    ... izvoristu u periodu jul, 2007-jul, 2008 Figure 4. Comparative diagram of fluctuations of groundwater levels, Sava river water levels and the exploited amount of water at the groundwater source during the period July 2007-July 2008 109 ...
    ... (sept-dec.) u periodu 2001-2011. godine Figure 2. Comparative diagram of mean values of groundwater extraction and Sava river water levels during the autumn months (Sept.-Dec.) in the period 2001-2011 starenja bunara usled procesa kolmatacije koji su intenzivirani poviSenim koncentracijama gvozda (i preko ...

  • Model određivanja evapotranspiracije u heterogenim geološkim uslovima na primeru gornjeg sliva Zapadne Morave

    Jugoslav Nikolić (2004)
    Evapotranspiracija, geološki uslovi, Zapadna Morava

  • Geneza i stratigrafija kvrtarnih sedimenat u slivu Južne i Zapadne Morave (sa kraćim osvrtom na prilike u Dakijskom i Panonskom basenu)

    M.O. Rakić (1976)
    Geneza , stratigrafija, sedimenti, Morava

  • A hydrogeological model of the open-cast mine Tamnava - West Field (Kolubara Coal Basin, Serbia)

    Jelena Ratković, Dušan Polomčić, Dragoljub Bajić, Bojan Hajdin (2016)
    ... model of the open-cast mine… 45 2. STUDY AREA KBC occupies a land area of about 600 km2. It is located some 50 km southwest of the capital Belgrade (Fig. 1) and encompasses the area around the middle and lower courses of the Kolubara River and its tributaries: the Tamnava (left) and the Peštan ...
    ... alluvial and terrace riverine-lacustrine sediments made up of medium- grain gravels and sandy gravels (river terraces and alluvial plains - riverbed sediments of the Kolubara, the Kladnica, the Turija and the Peštan). There are also other deposits, such as diluvial/proluvial and oxbow sediments - silty clays ...
    ... lower river terrace; Q, Pl - riverine-lacustrine terrace; Pl1 - sand and clay (marly and coaly) There is a triple aquifer system in the extended zone of the study area: upper, intermediate and lower. The three aquifers are all confined and feature a subartesian groundwater level. The upper ...

  • Centar za hidrogeologiju karsta - 15 godina nauke i struke

    urednici Saša Milanović, Ljiljana Vasić, Zoran Stevanović, Branislav Petrović (2023)
    Centar za hidrogeologiju karsta
    ... do 11. juna 2013. godine. vs 3 MEP.L5W{,(y\ , s. _BMYO N pp P O Učesnici ekskurzije ispred Velike prerasti na reci Vratna Participants in front of the Big natural stone bridge at the Vratna River Međunarodna konferencija „Karst bez granica” Međunarodna konferencija i terenski seminar „Karst ...
    ... Krupaja Spring, Veliko Vrelo Spring), as well as one of the arranged caves in this part of Serbia – the Resava Cave. The demonstration and installation of carbonate tablets has been performed in the heart of the Beljanica Mountain at the location of the Busovata Ravine. During the same year, members ...
    ... in the eastern part of the Carpathian orogenic belt A field trip to eastern Serbia was organized by members of the Karst Commission of the Serbian Geological Society (KC SGS) and CKH on June 10 and 11, 2013. Učesnici ekskurzije iznad klisure reke Zamna Participants above the Zamna River gorge ...