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Упит dcterms_creator_txt:Dragoslav R Rakić

910 items

  • Agates of the Lece Volcanic Complex (Serbia): Mineralogical and Geochemical Characteristics

    Zoran Miladinović, Vladimir Simić, Nenad Nikolić, Nataša Jović Orsini, Milena Rosić (2024)
    Agate veins and nodules occur in the Lece Volcanic Complex (Oligocene-Miocene) situated in the south of Serbia and occupying an area of 700 km2. This volcanic complex is composed predominantly of andesites, with sporadic occurrences of andesite-basalts, dacites and latites, and features agate formations that have been very little investigated. This study focuses on five selected agate occurrences within the Lece Volcanic Complex, employing optical microscopy, scanning electron microscopy (SEM), X-ray powder diffraction analysis, inductively coupled plasma mass spectrometry ...
    Lecki vulkanski kompleks, andeyit, kalcedon, kvarc, opal-CT, mikrostruktura, organska materija

  • Mikroorganizmi - biohidrogeološki indikatori odabranih pojava mineralnih voda Srbije

    Vladimir Šaraba (2021)
    Sa namerom definisanja hidrogeološke uloge i značaja mikrobiološkog diverziteta odabranih pojava mineralnih voda Srbije, primenom sistema biodetektora, dokazano je prisustvo gvožđevitih, sulfato-redukujućih, sluz-produkujućih, heterotrofnih aerobnih i denitrifikacionih bakterija, na osnovu čega je proračunat rizik od razvoja procesa biokorozije i biohemijske inkrustacije, te zdravstveni rizik. Uz procenu rizika, izvedene su analize skenirajuće elektronske mikroskopije biofilmova i hidrogeohemijsko modeliranje, te makroskopska, otpička i difrakciona ispitivanja naslaga inkrustacije, dok je fizičko-hemijskim analizama utvrđena vrednost ukupne mineralizacije iznad 1 g/L, kao i povišeni ...
    biohidrogeologija, SEM analize, makroskopska i optička ispitivanja, rendgenska difrakcija praha, hidrogeohemijsko modeliranje, BART analize, metabarkoding analize mikrobioma, fizičko-hemijske analize, starenje bunara (biokorozija, biohemijska inkrustacija i biozarastanje), zdravstveni rizik
    ... 000 – list Šabac, (Map). Beograd: Savezni geološki zavod. Rakić, M. O., Hadži-Vuković, M., Kalenić, M., Marković, V., & Milovanović, Lj. (1976). Geološka karta 1:100.000 – list Kruševac, (Map). Beograd: Savezni geološki zavod. Ramalho, R., Cunha, J., Teixeira, P., & Gibbs, P. A. (2001). Improved ...
    ... i.org/10.1007/978-3-642-38922-1_245 Terzin, V., Rakić, M. O., Bodić, D., Vukanović, M., Dimitrijević, M., Dimitrijević, M. N., & Karajičić, Lj. (1977). Geološka karta 1:100.000 – list Vranje, (Map). Beograd: Savezni geološki zavod. Terzin, V., Rakić, M., Hadži-Vuković, M., & Strajin, V. (1994). Geološka ...
    ... of Microbiological Methods, 44 (2), 97-103. R Core Team. (2012). R: A language and environment for statistical computing. R Foundation for Statistical Computing. Vienna, Austria. ISBN: 3-900051-07-0, URL: http://www.R- project.org/ Riding, R. (2000). Microbial carbonates: the geological record ...

  • Утицај промене нивоа подземне воде за услове плитког фундирања у крупнозрном тлу

    Милана Мичета (2024)
    Подземне воде представљају изузетно важан природни ресурс, као и важну компоненту система, којим је представљено тло. У складу са тим, приликом пројектовања плитких темеља на крупнозрном тлу, односно приликом анализе граничне носивости и слегања, треба узети у обзир и утицај воде. Верује се да ниво подземне воде значајно смањује носивост тла, док се слегања значајно повећавају. Terzaghi (1943) је први сугерисао да се потапањем масе тла, његова носивост смањује за половину, док се слегање удвостручује. Циљ овог рада је ...
    ниво подземне воде, плитко фундирање, крупнозрно тло, гранична носивост, слегање
    ... AyropcTBo – HekoMepnujaznHo (CC BY-NC) AyTopcTBo – HeKoMepnujajHo — 0e3 r pepana (CC BY-NC-ND) AyTOpcTBO — HeKOMCPIIHJAJIHO — JIeJIHTH IIOJ1 HCTHM yCJIOBHMa (CC BY-NC-SA) Ayropcrsno – 0e3 ıiipepana (CC BY-ND) m r —R O — — AyTOpcTBO — JeJIHTH IOJ HCTHM yCJIOBHMa (CC BY-SA) (3aokpyotcume ...
    ... ĐDAKVJITET z! - nyOHHa yrHiaja IIpoMeHe HanmoHa H - ne0JbuHa coja KOjH Ce CJIOOKC Da – arMocQbepcku rnpHrHcaK , 0.75 Š_ = 144· (BŽ) (4.1.4.5) R R Ako ce pajui o (bHHOM H rIpanmiHacTOM HecKy ca Nao > 15, Neo je norpeoHo nonecHTH KopHirhePeM (bakTopa Kopekrnuje, KoOjH cy HIpeJUIO'KHm Terzaghi ...
    ... 92 kPa + 231.79 kPa + 42.6 kPa Ra ršai 315.31 kPa MuznaHna Muuera, T615/21 R kN kN — = 2.4·kPa·17.05·1·1·1+(19.2—·1.1m+20 A m? —3·0.4}?1)·7.96·1·1 m npuzor 0p. 6 B) Tpehu cnyuaj HIIBs= 3.9 m B-im r EI [? ~ iji _ E P % s ž - Hsa>B Ppr i I f % P | a j\ Pu ha =4 .7 m Ra ...

  • Developing Termbases for Expert Terminology under the TBX Standard

    http://drug.rgf.bg.ac.rs/s/repo/item-set/522 (2014)
    ... ❣❡♦❧♦❣②✮✱ ❛♥❞ r❡❧❛t❡❞ ❝♦♥❝❡♣ts ♣♦❥❛✈❛ ♠✐♥❡r❛❧♥✐❤ s✐r♦✈✐♥❛ ✭♦❝❝✉r❡♥❝❡ ♦❢ ♠✐♥❡r❛❧ r❡s♦✉r❝❡✮✱ r✉❞♥♦ t❡❧♦ ✭♦r❡ ❜♦❞②✮ ✐ r✉❞❛ ✭♦r❡✮✳ ❘❡❧❛t❡❞ ♥❛rr♦✇❡r ❝♦♥✲ ❝❡♣ts ❛r❡ ❛❧s♦ r❡♣r❡s❡♥t❡❞✿ ❧❡➸✐➨t❡ ♠❡t❛❧✐↔♥✐❤ ♠✐♥❡r❛❧♥✐❤ s✐r♦✈✐♥❛✱ ❧❡➸✐➨t❡ ♥❡♠❡✲ t❛❧✐↔♥✐❤ ♠✐♥❡r❛❧♥✐❤ s✐r♦✈✐♥❛✱ ❧❡➸✐➨t❡ ❡♥❡r❣❡ts❦✐❤ ♠✐♥❡r❛❧♥✐❤ s✐r♦✈✐♥❛ ✭❞❡♣♦s✐ts ...
    ... t❤❡ r❡q✉✐r❡❞ t❡r♠✐♥♦❧♦❣② ❛r❡ t②♣✐✲ ❝❛❧❧② ❧❛r❣❡✳ ❚❤❡r❡❢♦r❡✱ ✐♥t❡❣r❛t✐♥❣ r❡❧❛t❡❞ t❡r♠✐♥♦❧♦❣② ✐♥t♦ ❛ tr❛♥s❧❛t✐♦♥ ♣✐♣❡❧✐♥❡ s❤♦✉❧❞ ❜❡ ❡①♣❧♦r❡❞ ❬✶✼❪✳ ❚❤✐s ❛♣♣r♦❛❝❤ r❡q✉✐r❡s ❛ ♣r♦❝❡ss t❤❛t ✐s ❛s ❛✉t♦♠❛t❡❞ ❛s ♣♦ss✐❜❧❡✳ ❲✐t❤ t❡r♠ ❡①tr❛❝t✐♦♥ ❛s ✐ts ❝♦r♥❡rst♦♥❡✱ ✐t r❡q✉✐r❡s ❛ ♣♦st✲♣r♦❝❡ss✐♥❣ str❛t❡❣② t❤❛t r❡♣✉r♣♦s❡s ...
    ... ❉❡✈❡❧♦♣✐♥❣ ❚❡r♠❜❛s❡s ✉♥❞❡r t❤❡ ❚❇❳ ❙t❛♥❞❛r❞ ✶✸ ❛r❡ st✐❧❧ ❜♦✉♥❞ t♦ ♠❛✐♥t❛✐♥ t❤❡✐r ✐♠♣♦rt❛♥❝❡ ✐♥ t❤❡ ❝❛s❡ ♦❢ ❡①♣❡rt t❡r♠✐♥♦❧♦❣② ✐♥ ❞♦♠❛✐♥s ✇❤❡r❡ ❛❧✐❣♥❡❞ ❝♦r♣♦r❛ ❛r❡ s♣❛rs❡ ❬✶✵❪✱ s✉❝❤ ❛s✱ ❢♦r ❡①❛♠♣❧❡ ♠✐♥✐♥❣ ❡♥❣✐♥❡❡r✐♥❣ ♦r ❣❡♦❧♦❣②✳ ■♥ ♦r❞❡r t♦ s❡❝✉r❡ t❡r♠✐♥♦❧♦❣✐❝❛❧ ❝♦♥s✐st❡♥❝② ✐♥ ♦♥❡ ♦r ♠♦r❡ t❡r♠❜❛s❡s✱ ❛♥❞ ...

  • Pleistocene rhinoceros from Bogovina Cave: the first report of Stephanorhinus hundsheimensis Toula, 1902 (Mammalia, Rhinocerotidae) from Serbia

    Predrag Radović, Miloš Radonjić, Emmanuel Billia (2020)
    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 ...
    rhinoceros, Stephanorhinus hundsheimensis, Serbia
    ... República y El Molinar en Alcoy, España. Recerques del Museu d’Alcoi, 16:7-18. Veselinović, M., Antonijević, I., Krstić, B., Mićić, I., Milošaković, R., Rakić, B., and Banković, V., 1964. Osnovna geološka karta SFRJ 1:100000 - list Boljevac. Savezni geološki zavod, Beograd. (In Serbian) Vislobokova, I ...
    ... istensen, R.R., Mackie, M., Ginolhac, A., Ferring, R., Tappen, M., Palkopoulou, E., Dickinson, M.R., Stafford Jr, T.W., Chan, Y.L., Götherström, A., Nathan, S.K.S.S., Heintzman, P.D., Kapp, J.D., Kirillova, I., Moodley, Y., Agusti, J., Kahlke, R.-D., Kiladze, G., Martínez-Navarro, B., Liu, S., Velasco ...
    ... iz Trlice kod Pljevlja (Crna Gora). Annales Géologiques de la Péninsule Balkanique, 61(2):161-175. (In Serbian with English translation) Cvetičanin, R. and Novković, M. 1975. The Bogovina Basin, p. 80-85. In Aksin, V. and Maksimović, B. (eds.), Geologija Srbije, Fosilna goriva, VII, Beograd. (In Serbian) ...

  • Named Entity Recognition for Distant Reading in ELTeC

    Francesca Frontini, Carmen Brando, Joanna Byszuk, Ioana Galleron, Diana Santos, Ranka Stanković (2020)
    Akcija COST „Udaljeno čitanje za evropsku književnu istoriju“, koja je počela 2017. godine, ima među svojim glavnim ciljevima stvaranje višejezične zbirke evropskih književnih tekstova (ELTeC) otvorenog koda. U ovom radu predstavljamo rad koji je obavljen na ručnom označavanju selekcije ELTeC kolekcije za imenovane entitete, kao i na proceni postojećih alata za prepoznavanje imenovanih entiteta u pogledu njihove sposobnosti da automatski urade takve anotacije. U poslednjem paragrafu se razmatraju zajedničke tačke između ove inicijative i CLARIN-a.
    ... te g o r ie s a n d ru le s fo r c r e a t in g a n n o ta te d c o rp o ra , so th a t a u to m a tic a lg o r i th m s c a n t ry to r e p l ic a te su c h a n n o ta tio n . H o w e v e r , N E R is a p r e l im in a ry m o d u le fo r o th e r ta s k s , s u c h a s in ...
    ... u p . F o r e a c h c o lle c tio n , w e te s te d tw o to o ls : o n e c o m m o n fo r a ll ( s p a C y 9), a n d a n o th e r o n e la n g u a g e sp e c if ic (S ta n fo rd -N E R fo r E n g l is h 10, S E M fo r F re n c h 11, P A L A V R A S -N E R fo r P o r tu g u e s ...
    ... e rn P o r tu g u e s e w o u ld p e r fo rm s ig n if ic a n tly w o rs e in th e por2 c o lle c tio n . T h is w a s c o n f irm e d fo r P A L A V R A S -N E R , w h ic h s h o w e d lo w e r p e r fo rm a n c e fo r por2, b u t n o t fo r sp aC y . T h is N E R s y s te m ...

  • Parameter determination of soil oscillation law using quotient of the relative growth increments of oscillation velocity and reduced distances at “Nepričava“ open pit mine

    Suzana Lutovac, Sanja Bajić, Marina Ravilić, Radmila Gaćina (2015)
    ... in our case n > 0. For R = R1, i = 2, 3, ..., N, from the equation (9), we can take that: 1 1 2,3,..., n i i R v v i N R         from where the relation is obtained: 1 1 2 1 1 2 ... ... n N N N N R v v v v R R R             (10) From the ...
    ... of relation (10) we obtain: 1 21 1 2 1 ... log log ... N N N N v v vR n R R R v                where we find: 1 2 1 1 1 2 ... log log ... N N N N v v v v n R R R R                (11) By the replacement of the ...
    ... that: v v n R R     (2) Thereby it can be considered that: 0 lim R v v n R R       which means that is: 12 Lutovac S.; Bajić S.; Gaćina R.; Ravilić M. ...

  • Models of Determining the Parameters of Rock Mass Oscillation Equation with Experimental and Mass Blastings

    Suzana Lutovac, Branko Gluščević, Rade Tokalić, Jelena Majstorović, Čedomir Beljić (2018)
    ... distance R from any level is increased (decreased) by 1%, the oscillation velocity of the soil v will decrease (increase) by approximately n% [8]. Indeed, for h = ± R 100 = ±1%R, from (12) we obtain: v ( R ± R 100 ) ≈ v(R)∓ n· R 100 · v(R) R , v ( R ± R 100 ) ≈ v(R)∓ n· v(R) 100 , v(R ± 1%R) ≈ v(R)∓ ...
    ... function v(R) from (7), in the final growth increment, we obtain: v(R + h) ≈ v(R) + h·v′(R + θ·h), 0 < θ < 1. (11) For small absolute values h, from (11), we obtain the relation: v(R + h) ≈ v(R) + h·v′(R). (12) Having (10) in mind, relation (12) becomes: v(R + h) ≈ v(R)− n·h·v(R) R . (13) A s ...
    ... the form: v(R) = K-R™. (7) Then from the Equation (7) for the derivation v’(R), we obtain: o'(R) = —n-K-R-"1, (8) Minerals 2018, 8, 70 5 of 18 which may be written in the form: v′(R) = − n R ·K·R−n. (9) Having in mind Equation (7), from the Equation (9), we obtain: v′(R) = −n·v(R) R . (10) If ...

  • Some models for determination of parameters of the soil oscillation law during blasting operations

    Suzana Lutovac, Dragan Medenica, Branko Gluščević, Rade Tokalić, Čedomir Beljić (2018)
    ... Equation (3), we obtain: v “ Kv ¨ ˝ 3 b 3¨Q 4¨π r ˛ ‚ n “ Kv ¨ ˜ 3 c 3 4 ¨ π ¸n ¨ ˆ 3 ? Q r ˙n “ Kv ¨ K1 ¨ ˆ r 3 ? Q ˙´n “ K ¨ ˆ r 3 ? Q ˙´n “ K ¨ R´n (5) where as: ˜ 3 c 3 4 ¨ π ¸n “ K1; Kv “ K K1 ; r 3 ? Q “ R (6) where: R—reduced distance is the distance from blasting ...
    ... marked ´n, meaning that: ∆v v ∆R R « ´n (7) Thereby it can be considered that: lim∆RÑ0 ∆v v ∆R R “ ´n, which means: dv v dR R “ ´n (8) Equation (8) can be written in the form: dv v “ ´n ¨ dR R , where by integration is obtained: ż dv v “ ´n ¨ ż dR R , namely: logv “ logR´n ` logC (9) ...
    ... Sm—surfaces of some trapezoids. R Rk Rk R RR RR £R R Figure 2. Graphic view of the polygonal line, N-1 of the trapezoid and curve v = K- R™". If: Ry —R Rigi -Ri =h= a (19) then, for S7, the following value is obtained: h Srp = = [01 +2(v2 +03 +...+U0N-1) + UN] (20) 2 If points R; are not equally spaced, ...

  • Soil oscillation law parameter determination with the application of Lagrange’s theorem at “Kovilovača“ open pit

    Suzana Lutovac, Nebojša Vidanović, Čedomir Beljić, Zoran Gligorić (2015)
    ... v RK Q r K Q r KK r Q K r Q Kv 331 3 3 3 4 34 3 Whereas: 1 3 4 3 K n ; KKKv 1 ; R Q r 3 whereby: R - reduced distance is the distance from blasting point to observation point re- duced to a quantity of explosive and given in the following form 0r r R No ...
    ... theo- rem is valid for it: ),( R- )v(R-)( 1 1 c s s Rv R Rv R1 < Rc < Rs. (8) Bearing in mind the formulas (4) and (5), formula (8) is reduced to: 1-n- c 1 -n 1 -n s Rn-k R- Rk-R sR k , (9) namely to: 1-n- c 1 -n 1 -n s R-n R- R-R sR , R1 < Rc < Rs. (10) No ...
    ... za nju važi Lagranžova teorema: ),( R- )v(R-)( 1 1 c s s Rv R Rv R1 < Rc < Rs. (8) Imajući u vidu formule (4) i (5), for- mula (8) se svodi na: 1-n- c 1 -n 1 -n s Rn-k R- Rk-R sR k , (9) tj. na: 1-n- c 1 -n 1 -n s R-n R- R-R sR , R1 < Rc < Rs. (10) Broj 3, 2015 ...

  • Determining the Groundwater Balance and Radius of Influence Using Hydrodynamic Modeling: the Case Study of the Groundwater Source “Šumice” (Kikinda, Serbia)

    Dušan Polomčić, Dragoljub Bajić, Jelena Zarić (2015)
    A groundwater flow model was developed to simulate groundwater extraction from the public water supply source of the City of Kikinda. The hydrodynamic model includes the municipal groundwater source of Kikinda (Šumice and the Jezero Well), but also an extended area where there are groundwater sources that provide water supply to three factories: (MSK, TM and LŽT - Kikinda). Hydrodynamic modeling, based on the numerical method of finite differences will show the groundwater balance of the sources in the ...
    Water supply, Aquifer, Flow, Groundwater regime, Numerical modeling, Particle tracking
    ... Kikinda Territory, Faculty of Mining and Geology, Belgrade, 2007. 19. Rakić, D., Study on the Groundwater Reserves at the Groundwater Source of “MSK” Factory in Kikinda, Hidrozavod DTD, Novi Sad, 2006. 20. Harbaugh, A. W., Banta, E. R., Hill, M. C. and McDonald, M. G., MODFLOW-2000: The U.S. Geological ...
    ... O. & Rumbaugh, D. B., Guide to using Groundwater Vistas: version 5. New York: Environmental Simulations, 2007. 22. Akindunni, F. F. and Gillham, R. W., Unsaturated and Saturated Flow in response to pumping of an Unconfined Aquifer: Numerical investigation of Delayed Drainage, http://dx.doi.org/10 ...

  • A Knowledge-Based Approach to Mine Ventilation Planning in Yugoslav Mining Practice

    Nikola Lilić, Ivan Obradović, Ranka Stanković (2002)
    Ventilation system analysis is a complex process based on the calculation and analysis of numerous parameters. These problems can be successfully solved by the SimVent numerical package, but a full understanding and use of the obtained results require the involvement of an experienced specialist in the ventilation field. The solution was found in the creation of a hybrid system INVENTS, whose knowledge base represents a formalization of the expert knowledge in the mine ventilation field. In this paper, we ...
    ... M in . R es . E n g . 2 0 0 2 .1 1 :3 6 1 -3 8 2 . D o w n lo ad ed f ro m w w w .w o rl d sc ie n ti fi c. co m b y U N IV E R S IT Y O F A L B E R T A o n 0 4 /2 6 /1 5 . F o r p er so n al u se o n ly . 362 N. Lilić, I. Obradović & R. Stanković ...
    ... M in . R es . E n g . 2 0 0 2 .1 1 :3 6 1 -3 8 2 . D o w n lo ad ed f ro m w w w .w o rl d sc ie n ti fi c. co m b y U N IV E R S IT Y O F A L B E R T A o n 0 4 /2 6 /1 5 . F o r p er so n al u se o n ly . 364 N. Lilić, I. Obradović & R. Stanković ...
    ... M in . R es . E n g . 2 0 0 2 .1 1 :3 6 1 -3 8 2 . D o w n lo ad ed f ro m w w w .w o rl d sc ie n ti fi c. co m b y U N IV E R S IT Y O F A L B E R T A o n 0 4 /2 6 /1 5 . F o r p er so n al u se o n ly . 366 N. Lilić, I. Obradović & R. Stanković ...

  • Analysis of a simplified model for determining rock mass oscillation velocity at the Kovilovača open pit

    Suzana Lutovac, Miloš Gligorić, Jelena Majstorović, Luka Crnogorac (2023)
    ... ~_n: Ap 5 (4) R Thereby, it can be considered that: Av Av lim „ _, Š =-n _ Which means that is: & =-n 6) R R . . Av AR . NEAR . Equation (5) can be written in the form: — %* — · R whereby integration, it is obtained: v Av AR — ~-n·| —,,respectively: logv=logR" +logC; j v j R p y: 108 ii Š ...
    ... equation where oscillation velocity V is given in the form of: v=K-R"; (D where R is reduced distance, that represents distance from the blasting site to monitoring site r , reduced to the total quantity of the explosive Q i.e., R =%č. Parameters K and m are conditioned by } v characteristics ...
    ... [m], Q - total amount of explosive [kg] . r [] v R - the reduced distance, given in the form R = | A significant property of the equation of rock mass oscillation velocity depending on the reduced distance is as follows: if the reduced distance R from any level is increased (decreased) by 1% ...

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    ... *e-mail: ppapic@rgf.bg.ac.rs A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • (10 μg/L). About 500 ...
    ... location of the test area. A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • Experimental Procedures ...
    ... Tap Water of Serbia’s... 1785 A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • A u th o r C o p y • some cases. Below this ...

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    Изингов модел, хексагонална решетка

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    Физика кондензоване материје

  • Sorpcija herbicida na neorganski i organski modifikovanom prirodnom montmorionitu iz Bogovine

    Lazar M. Kaluđerović (2018-01-17)
    fikasnost prilikom sorpcije S-metolahlora i klomazona od strane neorganskih iorganski modifikovanih montmorionita sa lokaliteta Bogovina odreĎena je metodombach adsorpcije. Uzorci montmorionita su tretirani prvo rastvorom NaCl a zatim irazličitim koncentracijama organskih kompleksa. Adsorpcione izoterme su dobijenetretiranjem uzoraka različitim koncentracijama herbicida. Detaljna mineraloškakarakterizacija uzoraka uraĎena je metodom rendgenske difrakcije. Rezultati interakcijemontmorionita sa organskim kompleksima i herbicidima dobijeni su primenomrendgenskih, optičkih, termičkih i spektroskopskih metoda.Na osnovu rezultata rendgenskih ispitivanja uzoraka, utvrĎeno je prisustvoorganskih kompleksa i herbicida u meĎuslojnom prostoru montmorionita.Montmorioniti modifikovani ...
    adsorpcija, montmorionit, heksadeciltrimetilamonijum bromid,feniltrimetilamonijum hlorid, S-metolahlor, klomazon
    ... Veselinović M., Antonijević I., Krstić B., Mićić I., Milošaković R., Rakić B., Banković V. 1970. Osnovna geološka karta SFRJ 1:100000, list Boljevac, K34-8. Savezni geološki zavod, Beograd. Westra E., Shaner D., Barbarick K., Khosla R. 2015. Evaluation of sorption coefficients for pyroxasulfone ...
    ... ugljovodoničnom R grupom (dvanaesti ili više ugljenikovih atoma u lancu) kao što je dodeciltrimetilamonijum bromid (DDTMABr- C15H34BrN) sa R grupom C12H25, heksadeciltrimetilamonijum bromid (HDTMABr-C19H42BrN) sa R grupom C16H33, oktadeciltrimetilamonijum bromid (ODTMABr-C21H46BrN) sa R grupom C18H37 ...
    ... Monitoring ground water or pesticides. In: Garnar, R. C., Honeycure, R. C., Higg, H. N., (Eds.), Evaluation of Pesticides in Ground Water. ACS Symposium Series 315, American Chemical Society, Washington, DC, 170–196. Cruz-Guzman M., Celis R., Hermosin C., Koskinen C. W., Cornejo J. 2005. Adsorption ...

  • Investigation of Co0.9Ho0.1MoO4 Nanopowders Obtained by Glycine Nitrate Procedure

    Milena Rosić, Maja Milošević, Maria Čebela, Vladimir Dodevski, Vesna Lojpur, Radomir Ljupković, Aleksandra Zarubica (2023)
    ... University in Skopje, R. N. Macedonia Members: Assoc. Prof. Dr. Vojo Jovanov, Faculty of Technology and Metallurgy, Ss. Cyril and Methodius University in Skopje, R. N. Macedonia Iva Dimitrievska, MSc, Faculty of Technology and Metallurgy, Ss. Cyril and Methodius University in Skopje, R. N. Macedonia ...
    ... and Metallurgy, Ss. Cyril and Methodius University in Skopje, R. N. Macedonia Members: Prof. Dr. Trajče Stafilov, Institute of Chemistry, Faculty of Natural Sciences and Mathematics, Ss. Cyril and Methodius University in Skopje, R. N. Macedonia Prof. Dr. Viktor Stefov, Institute of Chemistry ...
    ... Faculty of Natural Sciences and Mathematics, Ss. Cyril and Methodius University in Skopje, R. N. Macedonia Prof. Dr. Blazo Boev, Faculty of Natural and Technical Sciences, Goce Delčev University, Štip, R. N. Macedonia Prof. Dr. Panče Naumov, Division of Science and Mathematics, New York University ...

  • Hydrogeothermal potentials of Rogozna mountain and possibility of their valorization

    D. R. Ivanović, Dj. A Valjarević, R. D. Srećković-Batoćanin, N. M. Martić-Bursać, D. Ž. Vukoičić, R. M. Ivanović (2020)
    Geotermalna energija, hidrogeotermalni potencijal, stepen iskorišćenja, banja, Rogozna, Srbija

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    Изингов модел, критично понашање, танки системи