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649 items
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Low-temperature phase transition and magnetic properties of K3YbSi2O7
Predrag Dabić, Volker Kahlenberg, Biljana Krüger, Marko Rodić, Sabina Kovač, Jovan Blanuša, Zvonko Jagličić, Ljiljana Karanović, Václav Petříček, Aleksandar Kremenović (2021)alkalni silikati elemenata retkih zemalja, fazni prelazi, magnetne karakteristike, razdvajanje kristalnog polja, silikati lantanica... observed reflections 2409, 208, 187 [I > 2�(I)] 2644, 922, 840 [I > 2�(I)] Rint 0.040 0.045 (sin �/�)max (Å �1) 0.649 0.704 Refinement R[F 2 > 2�(F 2)], wR(F 2), S 0.013, 0.035, 1.17 0.027, 0.064, 1.14 No. of reflections 208 922 No. of parameters 20 26 � max, � min (e Å�3) 1.02, �0.44 1.40, �0.77 ...
... observed reflections 2409, 208, 187 [I > 2o(J)] 2644, 922, 840 [J > 2o(J)] Rint . 0.040 0.045 (sin 6/A) max (A7') 0.649 0.704 Refinement R[F? > 20(F’)], wR(F°), S 0.013, 0.035, 1.17 0.027, 0.064, 1.14 No. of reflections 208 922 No. of parameters 20 26 APimax» APmin (¢ AW) 1.02, —0.44 1.40, —0.77 ...
... a low-temperature polymorph (f’- K3YbSi,O7). The crystal structures of both modifications were determined. The magnetic properties of K;YbSi,O7 are interpreted based on the features of its crystal structures. Using group theory, the structural phase transition between f- and £’-K3YbSi,O, was analyzed ...Predrag Dabić, Volker Kahlenberg, Biljana Krüger, Marko Rodić, Sabina Kovač, Jovan Blanuša, Zvonko Jagličić, Ljiljana Karanović, Václav Petříček, Aleksandar Kremenović. "Low-temperature phase transition and magnetic properties of K3YbSi2O7" in Acta Crystallographica Section B Structural Science, Crystal Engineering and Materials, International Union of Crystallography (IUCr) (2021). https://doi.org/10.1107/S2052520621006077
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Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate
Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević (2021)Supported by evidence of deep crustal sources for the observed magnetic anomalies in Central Italy and by outcropping gabbros in the Croatian archipelago, we model the observed gravity and magnetic anomalies in the Central Adriatic Sea and surroundings. We suggest that the major magnetic anomalies in the area are related to a wide underplating and propose that this volume represents the first stage of the back-arc Adria continental breakup in Early Permian times. During the Palaeotethys-Adria collision, underplating has ...Paolo Mancinelli, Vittorio Scisciani, Cristina Pauselli, Gérard M. Stampfli, Fabio Speranza, Ivana Vasiljević. "Back-arc underplating provided crustal accretion affecting topography and sedimentation in the Adria microplate" in Marine and Petroleum Geology, Elsevier Ltd. (2021). https://doi.org/10.1016/j.marpetgeo.2021.105470
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Hidrogeohemijska valorizacija esencijalnih mikroelemenata mineralnih voda Srbije
Jana S. Stojković (2013-09-25)Mineralne vode još od davnina privlače pažnju ljudi i to kako u pogledu istraživanja iproučavanja, tako i u pogledu njihovog iskorišćavanja. Naročito je važno poznavanjesadržaja mikroelemenata u njima, jer su to komponente njihovog hemijskog sastavakoje ih odvajaju od tzv. „običnih“ malomineralizovanih voda.U ovom radu proučavani su odabrani esencijalni mikroelementi (fluor, bor, litijum,kalijum, stroncijum i silicijum), u mineralnim vodama Srbije, pri čemu je analiziranopreko 130 uzoraka mineralnih voda iz različitih geoloških sredina, to jest hidrogeološkihrejona. Cilj ovog istraživanja bio je ...esencijalni mikroelementi, faktori migracije, zakonomernosti rasprostranjenja, hidrogeohemijski procesi, multivarijantna statistička analiza, mineralne vode Srbije... kompleksa, pri čemu se u rastvoru, koji sadrži fluor i aluminijum, može obrazovati sledeća ravnoteža: Al3+ + F‒ ↔ AlF2+ + F‒ ↔ AlF2 + + F‒ ↔ AlF3 +F‒ ↔ AlF4 ‒ + F‒ ↔ AlF5 2‒ + F‒ ↔ AlF6 3‒ Pri uvećanju koncentracija fluora, ravnoteža se sve više pomera u desnu stranu, ka krajnjem članu ...
... jednačinom: Ksp,fluorit = [Ca2+] [F‒]2 = 10-10,57 na 25 °C Ako aktivnosti jona izrazimo preko koeficijenta aktivnosti, gornja jednačina dobija sledeći oblik: γ Ca 2+ · m Ca 2+ · γ F- 2 · m F- 2 = Ksp,fluorit m Ca 2+ · m F- 2 = 1 γ Ca2+ · γ F- 2 · Ksp,fluorit Konačno ...
... Ycq2t = 0,66 Isti postupak ponavljamo i za F: 16 Jana S. Stojković Doktorska disertacija 17 log γ F- = ‒ 0,5085 · (‒1)2 0,01 1+ 0,01 ‒ 0,3 · 0,01 = ‒ 0,0447 γ F- = 0,90 Važno je uočiti da je koeficijent aktivnosti jednovalentnog jona (F‒) znatno veći od koeficijenta aktivnosti ...Jana S. Stojković. "Hidrogeohemijska valorizacija esencijalnih mikroelemenata mineralnih voda Srbije" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2013-09-25)
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Understanding the effect of synthesis and sintering temperature on the functional properties of barium titanate/cobalt ferrite composites
Marija Šuljagić, Aleksandar Kremenović, Ivan Petronijević, Adis Džunuzović, Miljana Mirković, Vladimir Pavlović, Ljubica Anđelković (2023)To investigate the effect of synthesis procedure and sintering temperature on the functional properties of perovskite/spinel ceramics, BaTiO3/CoFe2O4 composites were prepared by thermal decomposition, coprecipitation, and microemulsion method, and sintered at 1150°C and 1300°C. The phase composition and morphology of as-prepared powders as well as sintered ceramics were thoroughly examined by X-ray powder diffraction (XRPD) and scanning electron microscopy (SEM) coupled with electron dispersive spectroscopy (EDS). The dielectric and ferroelectric measurements were performed in detail. Generally, the ...Marija Šuljagić, Aleksandar Kremenović, Ivan Petronijević, Adis Džunuzović, Miljana Mirković, Vladimir Pavlović, Ljubica Anđelković. "Understanding the effect of synthesis and sintering temperature on the functional properties of barium titanate/cobalt ferrite composites" in Science of Sintering (2023). https://doi.org/10.2298/SOS220512013S
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Mechanosynthesis and structural characterization of nanocrystalline Ce1–Y O2– (x=0.1–0.35) solid solutions
Martin Fabián, Bratislav Antić, Vladimír Girman, Milica Vučinić-Vasić, Aleksandar Kremenović, Shigeru Suzuki, Horst Hahn, Vladimír Šepelák (2015)A series of nanostructuredfluorite-type Ce1–xYxO2–δ (0rxr0.35) solid solutions, prepared via highenergy milling of the CeO2/Y2O3mixtures, are investigated by XRD, HR-TEM, EDS and Raman spectroscopy. For thefirst time, complementary information on both the long-range and short-range structural features of mechanosynthesized Ce1–xYxO2–δ, obtained by Rietveld analysis of XRD data and Raman spectroscopy, is provided. The lattice parameters of the as-prepared solid solutions decrease with increasing yttrium content. Rietveld refinements of the XRD data reveal increase in microstrains in the host ceria ...Martin Fabián, Bratislav Antić, Vladimír Girman, Milica Vučinić-Vasić, Aleksandar Kremenović, Shigeru Suzuki, Horst Hahn, Vladimír Šepelák. "Mechanosynthesis and structural characterization of nanocrystalline Ce1–Y O2– (x=0.1–0.35) solid solutions" in Journal of Solid State Chemistry, Elsevier BV (2015). https://doi.org/10.1016/j.jssc.2015.06.027
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Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia
Finds of Pleistocene rhinoceros are rare in Serbia, and only one species (the woolly rhinoceros Coelodonta antiquitatis Blumenbach, 1799) has been reported so far. The current paper presents the dental material of an extinct so-called Hundsheim rhinoceros, Stephanorhinus hundsheimensis Toula, 1902 from Bogovina Cave (East ern Serbia). Both the morphological and metric characteristics of the teeth are consis tent with the attribution to S. hundsheimensis. Unfortunately, the rhinoceros material originated from an uncertain geological context, so there is no ...... Society of Vertebrate Paleontology, Paris Las Vegas, Nevada, November 2-5, 2011:159- 160. Monesi, E., Muttoni, G., Scardia, G., Felletti, F., Bona, F., Sala, B., Tremolada, F., Francou, C., and Raineri, G. 2016. Insights on the opening of the Galerian mammal migration pathway from magnetostratigraphy of ...
... HMP-139b in (F) occlusal, (G) lingual, and (H) distal views. PALAEO-ELECTRONICA.ORG 5 FIGURE 4. Upper molars of Stephanorhinus hundsheimensis from Bogovina Cave: right M1/M2 HMP-131 in (A) occlu- sal, (B) vestibular, (C) lingual, (D) mesial and (E) distal views; right M1/M2 HMP-X in (F) occlusal, ...
... 1016/j.crpv.2015.05.004 Lacombat, F. 2005. Les Rhinocéros fossiles des sites préhistoriques de l’Europe méditerranéenne et du Massif Central, Paléontologie et implications biochronologiques. British Archaeological Research International Series, 1419:1-175. Lacombat, F. 2006a. Morphological and biometrical ...Predrag Radović, Miloš Radonjić, Emmanuel Billia. "Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia" in Palaeontologia Electronica, Coquina Press (2020). https://doi.org/10.26879/985
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Preliminary regional landslide susceptibility assessment using limited data
Igor Peshevski, Milorad Jovanovski, Biljana Abolmasov, Jovan Papic, Uroš Đurić, Miloš Marjanović, Ubydul Haque, Natasha Nedelkovska (2019)In this paper a heuristic approach for preliminary regional landslide susceptibility assessment using limited amount of data is presented. It is called arbitrary polynomial method and takes into account 5 landslide conditioning parameters: lithology, slope inclination, average annual rainfall, land use and maximum expected seismic intensity. According to the method, in the first stage, a gradation is performed for each of the carefully selected conditioning parameters by assigning so called rating points to the grid cells on which the ...... EECKHAUT, M.V.D., HER- VÁS, J., DASHWOOD, C. & GUZZETTI, F. (2013b): Tier-based approaches for landslide susceptibility assessment in Europe.– Landslides, 10/5, 529–546. doi: 10.1007/s10346-012-0349-1 GUZZETTI, F., REICHENBACH, P., ARDIZZONE, F., CARDINALI, M. & GAL- LI, M. (2006): Estimating the quality ...
... and likelihood ratio methods: a case study at İzmir, Turkey.– Landslides, 9/1, 93–106. doi: 10.1007/s10346-011-0283-7 ARDIZZONE, F., CARDINALI, M., CARRARA, A., GUZZETTI, F. & REICHEN- BACH, P. (2002): Impact of mapping errors on the reliability of landslide hazard maps.– Nat. Hazards Earth Syst. Sci ...
... doi: 10.1007/s12665-010-0724-y COROMINAS, J., VAN WESTEN, C., FRATTINI, P., CASCINI, L., MALET, J-P., FOTOPOULOU, S., CATANI, F., VAN DEN EECKHAUT, M., MAVROULI, O., AGLIARDI, F., PITILAKIS, K., WINTER, M.G., PASTOR, M., FERLISI, S., TOFANI, V., HERVAS, J. & SMITH, J. T. (2014): Recommendations for the ...Igor Peshevski, Milorad Jovanovski, Biljana Abolmasov, Jovan Papic, Uroš Đurić, Miloš Marjanović, Ubydul Haque, Natasha Nedelkovska. "Preliminary regional landslide susceptibility assessment using limited data" in Geologica Croatica , Croatian Geological Society (2019). https://doi.org/10.4154/gc.2019.03
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Merenje pritiska u bušotinskom cevovodu
Ratko Matija (2024)Merenje pritiska ima veliki značaj u naftovodima i gasovodima. U ovom završnom radu analizirane su različite metode merenja pritiska , kao što su merenje pritiska manometrima sa tečnostima, kapacitivnim manometrima, električnim manometrima nekim drugim. Objašnjena je kalibracija senzora pritiska koja u velikoj meri utiče na tačnost merenja. Navedeni su i objašnjeni elementi cevovoda i u vezi s tim pad pritiska, čije je merenje tema ovog završnog rada.... efekat uzrokovati dejstvo sile. Pritisak je u fizici matematički definisan kao intenzitet sile F, koja deluje na površinu S: P=F/S. Očigledno je da će za male vrednosti površine S, a pri delovanju iste sile F, vrednost pritiska biti veća nego što bi bila da se dejstvo sile raspodelilo na veću površinu ...
... podlozi. Vaga se dovodi u ravnotežno stanje kada je pritisak u zvonu jednak atmosferskom. Pri promeni pritiska, na dno cilindra deluje sila F = SAp. Sila F, odnosno promena pritiska meri se dodavanjem tegova kojima se vaga dovodi u ravnotežno stanje. Merni princip Je dakle isti kao i kod klipnog: ...
... pritisak p ili razliku pritisaka Zp u silu F usled koje dolazi do deformacije- pomaka /. Sila ili pomak pretvaraju se u narednom element u clektrični signal. Uređaj za normalizaciju električnog izlaznog signala daje standardni naponski ili izlazni signal. pili Ap F ili Ax Uili l STANDARDNI SIGNAL ...Ratko Matija. Merenje pritiska u bušotinskom cevovodu, 2024
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The subthermal potential of karstic groundwater of Kučaj–Beljanica region in Serbia estimated by the multivariate analysis
Earth-Surface Processes, Geology, Pollution, Soil Science, Water Science and Technology, Environmental Chemistry, Global and Planetary ChangeLjiljana Vasić, Dragana Ž. Živojinovic, Vladana Rajaković-Ognjanović, Huang Fen, Cao Jianhua. "The subthermal potential of karstic groundwater of Kučaj–Beljanica region in Serbia estimated by the multivariate analysis" in Environmental Earth Sciences, Springer Science and Business Media LLC (2021). https://doi.org/10.1007/s12665-021-09392-1
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Hypogene speleogenesis related to porphyry magmatic intrusions and its influence on subsequent karst evolution in the Peruvian high Andes
Alexander Klimchouk, David Evans, Sasa Milanovic, Cristian Bittencourt, Mauro Sanchez, F. Carlos Aguirre (2022)Alexander Klimchouk, David Evans, Sasa Milanovic, Cristian Bittencourt, Mauro Sanchez, F. Carlos Aguirre. "Hypogene speleogenesis related to porphyry magmatic intrusions and its influence on subsequent karst evolution in the Peruvian high Andes" in Geomorphology, Elsevier BV (2022). https://doi.org/10.1016/j.geomorph.2022.108488
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Određivanje parametara smičuće čvrstoće tla primenom statističke metode
Božidar Rudnjanin (2024)Određivanje parametara smičuće čvrstoće tla je od ključne važnosti u geotehničkom inženjerstvu jer utiče na stabilnost i nosivost raznih građevinskih konstrukcija. Ovaj master rad obrađuje temu primene deskriptivne statistike za analizu parametara smičuće čvrstoće tla,čime se obezbeđuje osnov za donošenje odluka o planiranju i izvođenju građevinskih projekata.U prvom delu rada, prikupljaju se relevantni podaci o smičućoj čvrstoći tla iz prethodnih laboratorijskih ispitivanja za trasu buduće brze saobraćajnice Novi Sad - Ruma.Ti podaci uključuju vrednosti smičuće čvrstoće i različite faktore ...... s ž i Granulometrijski saslav Zapreminska masa a j3 Slanje konsistencije Proktor CBR ';'Š;';::" F Koeficijent filtracije L g š Šš|S|4a N š|š3 | š |a * | Š | š žš s| 5 F-i š s| — [ I Š|sS}|Š I''T ~. F. iii thJ r — š| š r s |ž HBIET E slz sl |B|B|s _ 3|% |B g Š š| š Š 3 ||E s|E|ž|E|žš|š #rDJIB | ...
... Granulometrijski sastav Zapreminska masa }i Stanje konsistencije Proktor CBR r Koeicijent fihracije s|ls|e čvrstoće ii : s š|r|3 F| i & b| Hi ~ F š#|5 | 3 |i HIFSEE i <| ' | F -- t Š #* | & s |s ljE -l i Š E E s| š |1 || 5 \ s\ . š |ž ii š IBI FRIK:BoOFIEHIFa P E :||č|š|s|S |sihsši}ss} } |-.,|Š|2|, ...
... 12. X.w=21,30 [1 — 1,7 * 0,525 * /1 + i]: 2,30 El 28 m Xc„mea„=21,30[1 — 1,7 * 0,525 * F]: 21,73 k—Az, 28 m Xoow=21,30 [1 + 1,7 * 0,525 * /1 + i]: 49,89 FN 28 m 25 Xc„m„„=21,30[1 + 1,7 * 0,525 * F]: 30,55 ' 28 m C (kPa) - V je nepoznat 3.5 |i r3] E 3 •• H a D 2.5 Š e Vredno ...Božidar Rudnjanin. Određivanje parametara smičuće čvrstoće tla primenom statističke metode, 2024
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Optimizacija parametara reza rotornog bagera pri otkopavanju materijala sa povećanom čvrstoćom
Saša D. Bošković (2016-09-09)Otkopavanje materijala rotornim bagerom je veoma sloţen fiziĉko-mehaniĉki proces. Pokazatelji efektivnosti tog procesa zavise od velikog broja raznovrsnih ĉinilaca od kojih se posebno mogu istaći: fiziĉko-mehaniĉke karakteristike materijala koji se otkopava, reţim rada bagera i izbor tehnoloških parametara bloka, odreska i reza, geometrije vedrica i zuba itd. Poseban problem se javlja kod otkopavanja materijala povećane ĉvrstoće, što je ĉest sluĉaj na našim površinskim kopovima. Dimenzionisanje specifiĉne sile kopanja bagera prema manjim masama izuzetno ĉvrstog materijala je neracionalno i rešenje ...rotorni bager, parametri reza, otpor na kopanje, dinamika bagera, kapacitet, optimizacija, specifična potrošnja energije... kopanje razlaţe na tri komponente (Slika 3.24.): tangentnu (Pt), boĉnu (Pb) i normalnu (Pn). 4 3 2 1 F F m in F m F m in F m a x F m F m in F m a x F m F m in F m a x S f fn fs fs fn 73 Slika 3.24. Sile koje deluju na vedricu pri otkopavanju materijala (P – rezultanta ...
... . 1,2,3ji, , M M F F, w , 3x3 reda je k , F F F kkk kkk kkk , 1,2,3ji, , F F F, v u , 2x2 reda je k , F F F kkk kkk kkk yi xi zi i yi xi i i sij e3 2 1 e3 2 1 s es33s32s31 ...
... ec t cb cb a ec ec t cb cb a kkkk LEIeLEId LEILEI LEIeLEId LEILEI LGIt (5.2) Opterećenje elementa grede glasi: F F F F M M M F F F M M M e x y z x y z x y z x y z T 1 1 1 1 1 1 2 2 2 2 2 2 . (5.3) Matrica masa bez momenata inercije ...Saša D. Bošković. "Optimizacija parametara reza rotornog bagera pri otkopavanju materijala sa povećanom čvrstoćom" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2016-09-09)
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Adaptive neuro-fuzzy prediction of operation of the bucket wheel drive based on wear of cutting elements
The capacity of the rotor excavator depends largely on the operation of the subsystem for digging. There is a great contribution to the correct and sharp teeth when the capacity is the highest. In the function of time, the teeth become clogged due to abrasive wear, or changes in their geometric shape. To analyze the bucket wheel drive in depend on wear of the cutting elements in this study adaptive neuro fuzzy inference system (ANFIS) approach was implemented. ANFIS ...Filip Miletić, Predrag D. Jovančić, Milos Milovančević, Dragan Ignjatović. "Adaptive neuro-fuzzy prediction of operation of the bucket wheel drive based on wear of cutting elements" in Advances in Engineering Software, Elsevier BV (2020). https://doi.org/10.1016/j.advengsoft.2020.102824
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Multihazard Exposure Assessment on the Valjevo City Road Network
Miloš Marjanović, Biljana Abolmasov, Svetozar Milenković, Uroš Đurić, Jelka Krušić, Mileva Samardžić Petrović (2019)Miloš Marjanović, Biljana Abolmasov, Svetozar Milenković, Uroš Đurić, Jelka Krušić, Mileva Samardžić Petrović. "Multihazard Exposure Assessment on the Valjevo City Road Network" in Spatial Modeling in GIS and R for Earth and Environmental Sciences, Elsevier Inc (2019). https://doi.org/10.1016/B978-0-12-815226-3.00031-4.
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Threshold-induced correlations in the Random Field Ising Model
... as duration T, and the area between the imposed threshold and the portion of the signal above it as the size of subavalanche, § = f 7 dt[V(t, + t) — Vj} see Fig. 1a, where f is the time measured from the start t, of the subavalanche. ° Once a threshold is applied, a portion of the signal will remain below ...
... avalanche type ˆ iSb is ′ ≡ ′ˆf t b f bt( ) ( ), (2)i x iSb where x is an exponent speci�ed by the type of the involved system5. For this family of transformations one can prove that = = − ˆ ˆT T b S b S/ , , (3)i i i x iS S 1 b b where Ti is duration, and ∫≡ ′ ′S f t dt( )i T i0 i is the size ...
... random media: from superconductors to earthquakes. Phys. Rep. 301, 113–150 (1998). 17. Omori, F. On the a�ershocks of earthquakes. J. Coll. Sci. Imp. Univ. Tokyo 7, 111–200 (1894). 18. Jagla, E. A., Landes, F. P. & Rosso, A. Viscoelastic E�ects in Avalanche Dynamics: A Key to Earthquake Statistics. Phys ...Sanja Janićević, Dragutin Jovković, Lasse Laurson, Đorđe Spasojević. "Threshold-induced correlations in the Random Field Ising Model" in Scientific Reports, Springer Science and Business Media LLC (2018). https://doi.org/10.1038/s41598-018-20759-6
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The influence of Al<sup>3+</sup>ion on porcine pepsin activity<i>in vitro</i>
The in vitro effect of Al3þ ions in the concentration range 1.7·1026M–8.7·1023M on pepsin activity at pH 2, via kinetic parameters and its electrophoretic mobility was evaluated. Kinetic study demonstrated the existence of an activation effect of Al3þ at pH 2 on pepsin molecule. Kinetic analysis with respect to concentrations of haemoglobin showed that Al3þ ions increase the maximal velocity (Vmax) and kcat values rather than apparent affinity for substrate (KS) implying the non-competitive nature of activation which indicated ...... RIGHTSLIMKMK&~Ž --| zj g s = 6 = || Fa Š F1 || -| |-s} e --| = > 5 E 8 o 9 H i 5 | 9 -i : i:| |-i | P 3 ' o F| FI o [= i F Š |} i Jo ur al of En zy me In hi l Fo r pe rs on al us e on ly . 1004 I7 M. Pavelhic et al. water. The concentration ...
... RIGHTSLIMKMK&~Ž --| zj g s P o 5 | Š o S - s = 5 j| E > F3 E o 9 Š Đ 8 8 -| = P F-| |- o al Ch em is tr y Do wn lo ad ed fr om -| -} P |l = & Š |-5} |j 6 | || F| 5 -i Fo r pe rs on al us e on ly . in dose-dependent manner and linear curve (the ...
... RIGHTSLIMKMK&~Ž --| zj g s P o 5 | Š o S - s = 5 j| E > F3 E o 9 Š Đ 8 8 -| = P F-| |- o al Ch em is tr y Do wn lo ad ed fr om -| -} P |l = & Š |-5} |j 6 | || F| 5 -i Fo r pe rs on al us e on ly . 1006 I7 M. Pavelhic et al. Table I. Influence of ...Vesna M. Pavelkić, Kristina R. Gopcević, Danijela Z. Krstić, Marija A. Ilić. "The influence of Al3+ion on porcine pepsin activityin vitro" in Journal of Enzyme Inhibition and Medicinal Chemistry, Informa UK Limited (2008). https://doi.org/10.1080/14756360701841095
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Развој модела употребног квалитета помоћне механизације на површинским коповима лигнита
Драгица Јагодић Крунић (2021)Тренутно стање помоћне механизације на површинским коповима лигнита је незадовољавајуће узроковано пре свега старошћу и неблаговременом заменом машима услед чега је расположивост недовољна а трошкови експлоатације и одржавања високи. Тренутно стање и захтеви који се постављају пред ове машине указују на неопходност оптимизације процеса управљања помоћном механизацијом. Одређивање оптималног времена замене и преосталих могућности је најодговорнији управљачки задатак који треба да буде заснован на свеобухватном сагледавању економских, техничких и других узрочно последичних веза. Са економског аспекта гледано треба одржавати ...помоћна механизација, употребни квалитет, ефективност, расположивост, сигурност функционисања, ризик, трошкови животног циклуса, фази логика, Монте Карло метода... процена показатеља F за остале машине. У табели 8.1.2.4.5. дате су процене показатеља F за све посматране машине. V F НИЗАК НИВО IV F ПРИХВАТЉИВ НИВО III F ПРОСЕЧАН НИВО II F ВИСОК НИВО I F ВЕОМА ВИСОК НИВО 0,63 0,60 0.00 0.25 0.50 0.75 1.00 1 2 3 4 5 μ (F) j 70 0 27 ...
... скуповима показатеља F: μ (FПРИХ. НИВО) = 0,55 ; μ (FПРОС. НИВО) = 0,70. Очитане вредности се скалирају како би њихов збир био 1: FПРИХ. НИВО + FПРОС. НИВО = 1 ΔQmax ΔQsr ΔQmin 00.1 1 2 3 4 5 V F НИЗАК НИВО IV F ПРИХВАТЉИ В… III F ПРОСЕЧА Н … II F ВИСО К НИВО I F ВЕОМА ВИСОК НИВО ...
... вредности f (xi , а, b, c, …..) минимална [119]: 𝐹 = ∑ 𝐹𝑖 =𝑛 𝑖=1 ∑[𝑦𝑖 − 𝑓(𝑥𝑖 , 𝑎, 𝑏, 𝑐, … . . )]2𝑛 𝑖=1 → 𝑚𝑖𝑛 (7.28) Функција F се назива функцијом циља. Ако је F функција непознатих параметара функције f, онда тражимо минимум (глобални) функције облика F (а, b ...Драгица Јагодић Крунић. Развој модела употребног квалитета помоћне механизације на површинским коповима лигнита, Београд : [Д. Јагодић Крунић], 2021
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Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians
Nemanja Krstekanić, Liviu Matenco, Marinko Toljić, Oleg Mandić, Uroš Stojadinović, Ernst Willingshofer (2020)... Jolivet, L., Rossetti, F., 2004. Lateral slab deformation and the origin of the western Mediterranean arcs. Tectonics 23, TC1012. https://doi.org/10.1029/2002TC001488. Faccenna, C., Becker, T.W., Auer, L., Billi, A., Boschi, L., Brun, J.P., Capitanio, F.A., Funiciello, F., Horvàth, F., Jolivet, L., Piromallo ...
... zavod, Belgrade. Bada, G., Horváth, F., Dövényi, P., Szafián, P., Windhoffer, G., Cloetingh, S., 2007. Present-day stress field and tectonic inversion in the Pannonian basin. Glob. Planet. Chang. 58, 165–180. Balázs, A., Matenco, L., Magyar, I., Horváth, F., Cloetingh, S., 2016. The link between ...
... Bojar, A.-V., Neubauer, F., Fritz, H., 1998. Cretaceous to Cenozoic thermal evolution of the southwestern South Carpathians: evidence from fission-track thermochronology. Tectonophysics 297, 229–249. Calignano, E., Sokoutis, D., Willingshofer, E., Brun, J.-P., Gueydan, F., Cloething, S., 2017. Oblique ...Nemanja Krstekanić, Liviu Matenco, Marinko Toljić, Oleg Mandić, Uroš Stojadinović, Ernst Willingshofer. "Understanding partitioning of deformation in highly arcuate orogenic systems: Inferences from the evolution of the Serbian Carpathians" in Global and Planetary Change, Elsevier BV (2020). https://doi.org/10.1016/j.gloplacha.2020.103361
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Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone
The Vardar Zone is a product of the Triassic-Jurassic opening of the Neotethys, Jurassic obduction, Late Cretaceous/Paleogene consumption of the oceanic crust and continental collision. During the last process, the Eastern Vardar Zone was thrust over the Central and eventually both onto the Western Vardar Zone. The present paleomagnetic and structural study provided new results from the first two zones in the Belgrade area. The younger set of data, together with published ones from the third zone, provide firm ...Emő Márton, Marinko Toljić, Vesna Cvetkov. "Late and post-collisional tectonic evolution of the Adria-Europe suture in the Vardar Zone" in Journal of Geodynamics, Elsevier BV (2022). https://doi.org/10.1016/j.jog.2021.101880
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Petrološke karakteristike dunavskog šljunka (Beograd – Zemun)
Miloš Mihajlović (2024)Dunavski šljunak u okolini Zemuna karakterističan je za obalne rečne naslage formirane dugotrajnim procesima erozije i transporta materijala koje reka Dunav nosi sa različitih područja uzvodno. Ispitivanja šljunka sa lokacije „Gemax” su pokazala je šljunak uglavnom zaobljen, najčešće u rasponu od nekoliko milimetara do nekoliko centimetara u prečniku. Kako Dunav nosi materijal sa velikog sliva, ovaj šljunak sadrži raznovrsne sastojke sa dominacijom kvarca i odlomaka stena visokosilicijskog sastava. Mineraloško-petrografska ispitivanja pokazala su prisustvo klasta različitog sastava, čime je potvrđena ...... ostala na situ 0,063 mm posle pranja Sadržaj finih čestica f(%) f= 100 - (M2(100+W)/MI1) ako je f < 10%, onda je MT = 120*(100+w)/100 ako je f> 10%, onda je MT = M3 + M4 M3 = 1200/f *(1+ (w/100)) - Uzorak 0/2 mm M4 = 120 - (1200/ f) - Uzorak 0,003/2 mm Masa test uzorka - Mt (g) hl-Visina ...
... ·m„·„„...··,„..„„„.„„„ F F " 4 {aranii tts -..a_..–.·.·„„„.m i » 1y RRRAAAAA -,...„„ · e |psteiideskbipekmi |s |s p ec:een ı F1 Pz= P |= | |_ ms ps b \gea bsa0 |_ OOO 9 |sweche uhs ispekni — Ls · albari | alkarenii Baskovili irežnjaci (urganiki slojevi)– f yeščari \ ginai liaci ...
... PRIMARNA OZNAKA OPISNA OZNAKA Krupnozrna tla sa preko — G (šljunak) w dobra 50% zrna većih od U jednolična graduiranost 0.075mm S (pesak) P slaba F prašine . . primese c gline Sitnozrna tla sa preko M (prašina) L niska 50% zrna manjih od C (glina) (I) (srednja) | plastičnost 0.075mm O (organsko ...Miloš Mihajlović. Petrološke karakteristike dunavskog šljunka (Beograd – Zemun), 2024