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Упит dcterms_creator_txt:Kristina R. Gopcević

739 items

  • The influence of Al<sup>3+</sup>ion on porcine pepsin activity<i>in vitro</i>

    Vesna M. Pavelkić, Kristina R. Gopcević, Danijela Z. Krstić, Marija A. Ilić (2008)
    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 ...
    Пепсин, алуминијум, кинетика, активација, електрофоретска мобилност
    ... vitro Vesna M. Pavelkić, Kristina R. Gopcević, Danijela Z. Krstić, Marija A. Ilić Дигитални репозиторијум Рударско-геолошког факултета Универзитета у Београду [ДР РГФ] The influence of Al3+ion on porcine pepsin activityin vitro | Vesna M. Pavelkić, Kristina R. Gopcević, Danijela Z. Krstić, Marija ...
    ... 2008; 23(6): 1002—-1010 informa healthcare • 3+ • • • •. B •. The influence of A' ion on porcine pepsin activity 2? TfO VESNA M. PAVELKIC!, KRISTINA R. GOPCEVIC?, DANIJELA Z. KRSTIC?, & MARIJA A. ILIC? lDepartmem of Physical Chemistry, Vinca-pInstitute of Nuclear Science, POB 522, 11001 Belgrade ...
    ... of AP? ion, the electrophoretic mobility of pepsin under the physio- logical conditions the obtained R. value for pepsin is 0.47 while in the presence of 1, 5 and IOmM Al ions the obtained R. values were 0.46, 0.44 and 0.42, respectively. It is obviously that the highest concen- tration of ...

  • Cognate clinopyroxene from Paleogene mantle xenolith-bearing basanite lavas (East Serbia, SE Europe): the role of dissolution of mantle orthopyroxene

    Cvetković Vladica, Erić Suzana, Radivojević Maša, Šarić Kristina (2012)

  • Геологија планине Козаре

    Грубић Александар, Цвијић Ранко, Цветковић Владица, Шарић Кристина, Милошевић Алексеј"" (2018)

  • Геологија планине Козаре

    Грубић Александар, Цвијић Ранко, Цветковић Владица, Шарић Кристина, Милошевић Алексеј"" (2018)

  • Геологија планине Козаре

    Грубић Александар, Цвијић Ранко, Цветковић Владица, Шарић Кристина, Милошевић Алексеј (2018)

  • Геологија планине Козаре

    Грубић Александар, Цвијић Ранко, Цветковић Владица, Шарић Кристина, Милошевић Алексеј (2018)

  • Antioxidant and antimicrobial activity of some tetradentate Schiff bases and their Cu (II) complexes

    Aleksandar Mijatović, Milan Nikolić, Snežana Spasić, Aleksandra N. Žerađanin, Kristina Joksimović, Aleksandar Lolić, Rada Baošić (2020)
    Šifove baze i njihovi Cu(II) kompleksi su poznati po svojoj biološkoj aktivnosti. U ovom radu proučavana je antibakterijska aktivnost protiv gram-negativnih sojeva Escherichia coli, Pseudomonas aeruginosa i Staphilococcus piogenes, kao i Gram-pozitivnih Staphilococcus piogenes i Pseudomonas aeruginosa, zajedno sa antifungalnim dejstvom protiv Musperg strainilusa, A. Takođe, tehnički jednostavni i brzi testovi kao što su ABTS, HORAC i ORAC korišćeni su za ispitivanje antioksidativne aktivnosti kako bi se uporedili dobijeni rezultati sa različitim tipovima testova. Uprkos tome što je princip ...

  • Products of oxidative dissolution on waste rock dumps at the Pb-Zn mine Rudnik in Serbia and their possible effects on the environment

    Alena Zdravković, Vladica Cvetković, Aleksandar Pačevski, Aleksandra Rosić, Kristina Šarić, Vesna Matović, Suzana Erić (2017)

  • Products of oxidative dissolution on waste rock dumps at the Pb-Zn mine Rudnik in Serbia and their possible effects on the environment

    Alena Zdravković, Vladica Cvetković, Aleksandar Pačevski, Aleksandra Rosić, Kristina Šarić, Vesna Matović, Suzana Erić (2017)

  • Geochemical characterization of sediments from the archaeological site Vinča – Belo Brdo, Serbia

    Gorica Veselinović, Dragana Životić, Kristina Penezić, Milica Kašanin-Grubin, Nevenka Mijatović, Jovana Malbašić, Aleksandra Šajnović (2020)
    Earth-Surface Processes

  • Developing Termbases for Expert Terminology under the TBX Standard

    http://dr.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✱ ❛♥❞ ...

  • 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 ...

  • 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% ...

  • Petrologija magmatskih i metamorfnih stena - praktikum

    Kristina Šarić (2014)
    petrologija, magmatske stene, metamorfne stene

  • Petrologija magmatskih stena dijabazarožnjačke formacije kod Ždraljice(Kragujevac)

    Kristina Resimić (2000)
    Petrologija, magmatske stene, dijabazarožnjačka formacija, Ždraljica