Претрага
670 items
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Overcoming the Low Oral Bioavailability of Deuterated Pyrazoloquinolinone Ligand DK-I-60-3 by Nanonization: A Knowledge-Based Approach
Jelena R. Mitrović , Branka Divović-Matović, Daniel E. Knutson, Jelena B. Ðoković, Aleksandar Kremenović, Vladimir D. Dobričić, Danijela V. Randjelović, Ivana Pantelić, James M. Cook, Miroslav M. Savić, Snežana D. Savić (2021)Poor water solubility of new chemical entities is considered as one of the main obstacles in drug development, as it usually leads to low bioavailability after administration. To overcome these problems, the selection of the appropriate formulation technology needs to be based on the physicochemical properties of the drug and introduced in the early stages of drug research. One example of the new potential drug substance with poor solubility is DK-I-60-3, deuterated pyrazoloquinolinone, designed for the treatment of various neuropsychiatric ...... column tempera- ture was set to 35 ◦C. Detection and quantification of DK-I-60-3 and internal standard were performed in positive HESI mode (m/z = 328.10–282.05 and m/z = 349.00–303.85, respec- tively). 2.2.6. Statistical Analysis All measurements were performed in triplicate, and results were expressed ...
... likelihood of interparticle collisions [8]. Table 3. Particle size (z-ave), polydispersity index (PDI), and zeta potential (ZP) of nanocrystal dispersions after one hour of milling (mean ± SD, n = 3). Formulation Milling Media Volume (%, v/v) z-Ave (nm) PDI ZP (mV) 60 195.8 ± 1.7 0.238 ± 0.029 F1 40 236 ...
... are mandatory for new drug substances [2,9]. Table 4. Particle size (z-ave), polydispersity index (PDI), and zeta potential (ZP) of nanocrystal dispersions after one and three months of storage (mean ± SD, n = 3). Formulation z-Ave (nm) PDI ZP (mV) 1 Month 3 Months 1 Month 3 Months 1 Month 3 Months ...Jelena R. Mitrović , Branka Divović-Matović, Daniel E. Knutson, Jelena B. Ðoković, Aleksandar Kremenović, Vladimir D. Dobričić, Danijela V. Randjelović, Ivana Pantelić, James M. Cook, Miroslav M. Savić, Snežana D. Savić. "Overcoming the Low Oral Bioavailability of Deuterated Pyrazoloquinolinone Ligand DK-I-60-3 by Nanonization: A Knowledge-Based Approach" in Pharmaceutics, MDPI, Basel, Switzerland (2021). https://doi.org/10.3390/pharmaceutics13081188
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Palaeoflora of Kamenica (Pranjani Basin, western Serbia)
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 ...... anali Balkanskoga poluostrva, 80: 1–15. LaZarevIć, Z. 2008. Neogene flore Srbije [Neogene Floras of Serbia – in Serbian, with an english abstract]. un- publ.Phd Thesis, Faculty of Mining and Geology, uni- versity of Belgrade, 147pp. LaZarevIć, Z. & MILIvOjevIć, j. 2010. early Miocene flora of the ...
... intramontane Žagubica Basin (Serbian carpatho- Balkanides). Neues Jahrbruch für Geologie und Paläon- tologie, Abhandlungen, 256: 141–150. LaZarevIć, Z., MILIvOjevIć, j., BOGIćevIć, K. & NeNadIć, d. 2013. early Miocene flora from the valjevo-Mionica Basin (Western Serbia). Neues Jahrbruch für Geologie ...
... северозападном делу грабена. Има изглед плитког рова ограниченог раседима пружања СЗ–ЈИ и додатно је издељен на мање блокове системом раседа СИ–ЈЗ и И–З. То је депозициони простор слабог интензитета тоњења (MarOvIć et al., 2007). Биљни фосилни остаци су прикупљени са локалитета Каменичке реке у селу ...Zorica Lazarević, Ljubica Milovanović, Jelena Milivojević, Ivana Vasiljević . "Palaeoflora of Kamenica (Pranjani Basin, western Serbia)" in Geološki anali Balkanskog poluostrva, Beograd : Rudarsko-geološki fakultet (2019). https://doi.org/10.2298/GABP1902053L
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A new copper(II) arsenate, Na2Cu3(AsO3OH)4·4H2O containing discrete [Cu3O12]18− units: Synthesis, crystal structure and magnetic properties
Single crystals of the new disodium tricopper(II) tetrakis(hydrogenarsenate(V)) tetrahydrate, Na2Cu3(AsO3OH)4·4H2O were grown under hydrothermal conditions. The compound was characterized by room-temperature single-crystal X-ray diffraction, SEM-EDS analysis, Raman spectroscopy and magnetic susceptibility measurements. Na2Cu3(AsO3OH)4·4H2O represents a new layered structure-type [space group P21/c, a = 8.7089(17), b = 9.7452(19), c = 9.3353(19) Å, β = 92.63(3)°, V = 791.4(3) Å3, Z = 4]. The layers are normal to [100] and are composed of the isolated Cu3O12 units interconnected by AsO3OH coordination ...Na2Cu3(AsO3OH)4•4H2O, хидротермална синтеза, кристална структура, хидрирани хидрокси-арсенати, магнетна својстваTamara Đorđević, Ljiljana Karanović, Zvonko Jagličić. "A new copper(II) arsenate, Na2Cu3(AsO3OH)4·4H2O containing discrete [Cu3O12]18− units: Synthesis, crystal structure and magnetic properties" in Journal of Solid State Chemistry, Elsevier BV (2018). https://doi.org/10.1016/j.jssc.2018.05.024
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Hydrochemical changes and groundwater grouping data by multivariate statistical methods within one karst system: recharge–discharge zone (Eastern Serbia case study)
Ljiljana Vasić, Dragana Živojinović, Vladana Rajaković-Ognjanović. "Hydrochemical changes and groundwater grouping data by multivariate statistical methods within one karst system: recharge–discharge zone (Eastern Serbia case study)" in Carbonates and Evaporites, Springer Science and Business Media LLC (2020). https://doi.org/10.1007/s13146-019-00548-6
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Definition of groundwater genesis and circulation conditions of the complex hydrogeological karst system Mlava–Belosavac–Belosavac-2 (eastern Serbia)
Ljiljana Vasić, Saša Milanović, Zoran Stevanović, Laszlo Palcsu. "Definition of groundwater genesis and circulation conditions of the complex hydrogeological karst system Mlava–Belosavac–Belosavac-2 (eastern Serbia)" in Carbonates and Evaporites, Springer Science and Business Media LLC (2020). https://doi.org/10.1007/s13146-020-00550-3
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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 ...... . Cunrerampe ce no0uja rpeko caenehuax JenHauuHa: Se _ ___4 Se(1) i [1+(%)]Z (4.1.1.1) Se — c1ferabbe TeMeJba JUHMeH3HJa B x B Se(1)— CJterabbe Ipo0OHe nunoue Bi x Bi BeoMa 30HJjeHo 30nHjeHO Nao=30 i-] Z |--- = |2 Š F3 F- 5 [-] Fa = = 5 |El i Hi s Š [ 2 ImHpliHa TeMeJba ...
... MIOIIyHCKO HeTO oOnTepeheme B – nmipunHa ripaBoyraoHor HJIH IpeuHHK Kpy)KHOr TeEMCJba Es Ey — npoceuHut HeJipeHHpaHu MOJILyJ e_tacTHuHOCTH OJL Z=0 no z=4B B' = B/2 – s3a neHrpHuHy TauKy TeEMECJba B' = B – a3a yraoHy Tauky TeMeJba V = Vu= 0.5 – HeJipeHupaHu IIoacoHoB koe()HijeHT Ie— yramajnu ...
... b= |j 4. 7m js - - hi - Ra/A' = C'Nebcicse + q'Nabaiqsa + 0.5y B'NybyLySy Ra Z= 24kPa'17.05:1-1-1 kN kN kN + (19.2—3·0.4m+9.2—3,·0.7m+ 10—3·0.491)·7.96·1·1 m m m kNxN '1+0-5'10—Z'1M'5-68'1'1'1 m Ra _= 40.92 kPa + 144.24 kPa + 28.4 kPa % = 213.56 kPa MuznaHna Muuera, ...Милана Мичета. Утицај промене нивоа подземне воде за услове плитког фундирања у крупнозрном тлу, 2024
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A new polymorph of Ba(AsO3OH): Synthesis, crystal structure and vibrational spectra
Tamara Đorđević, Ljiljana Karanović (2010)A new monoclinic polymorph of Ba(AsO3OH) was synthesized under hydrothermal conditions. It represents a previously unknown structure type. Its crystal structure was determined from a racemic twin using single-crystal X-ray diffraction data collected at 120 and 293 K [space group P21, a=7.2149(14)/7.2370(2), b=7.7028(15)/7.7133(2), c=21.7385(43)/21.8079(5) Å, β=95.95(3)/96.073(1)1, V=1201.6(4)/1210.51(5) Å3, Z=12]. The crystal structure of P21-Ba(AsO3OH) has a layered character and is built up of four types of regularly alternating layers parallel to (0 0 1). Every AsO3OH tetrahedron is chelating to two Ba atoms and ...Ba(AsO3OH), хидротермална синтеза, структурна анализа монокристала, Раманска спектроскопија, инфрацрвена спектроскопија, водоничне везе, хидрогенарсенати земноалкалних металаTamara Đorđević, Ljiljana Karanović. "A new polymorph of Ba(AsO3OH): Synthesis, crystal structure and vibrational spectra" in Journal of Solid State Chemistry, Elsevier BV (2010). https://doi.org/10.1016/j.jssc.2010.09.027
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Razvoj ARCGIS geobaze površinskog kopa korišćenjem UML CASE alata
... position in this diagram is taken by the class Busotine, defined geometrically as a point (EsriGeometryPoint). It has the following attributes: X, Y, Z coordinates, borehole depth and year of drilling. Each of the attributes is defined, according to the data that are to be entered, as numerical, with ...
... esriFieldTypeInteger -Oznaka : esriFieldTypeString -Opis : esriFieldTypeString ProstorneKlase -X : esriFieldTypeDouble -Y : esriFieldTypeDouble -Z : esriFieldTypeDouble -Dubina : esriFieldTypeDouble -GodBusenja : esriFieldTypeInteger Busotina {GeometryType = EsriGeometryPoint, HasM = False,HasZ ...
... that are going to follow, these classes will be used for geostatistical modeling of deposits. -X : esriFieldTypeDouble -Y : esriFieldTypeDouble -Z : esriFieldTypeDouble -Dubina : esriFieldTypeDouble -GodBusenja : esriFieldTypeInteger Busotina -DTE : esriFieldTypeDouble -Vlaga : esriFieldTypeDouble ...Aleksandra Tomašević, Ljiljana Kolonja, Ivan Obradović, Ranka Stanković, Olivera Kitanović. "Razvoj ARCGIS geobaze površinskog kopa korišćenjem UML CASE alata" in Podzemni radovi, Beograd : Univerzitet u Beogradu - Rudarsko-geološki fakultet (2012)
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Proračun recirkulacionih pumpi u postrojenju za odsumporavanje dimnih gasova ,,TENT B"
Tomislav Trpković (2024)Predmet ovog rada baziraće se na proračunu i usvajanju mašinskih instalacija potrebnih za nesmetano funkcionisanje sistema dve međusobno povezane celine Absorber - Pumpna stanica, preko FRP ( Fiberglass Reinforced Plastic) cevovoda kojim se odvija transport suspenzije krečnjaka neophodnog u samom procesu odsumporavanja dimnih gasova. Pored tehničkog opisa same tehnologije koja uključuje tri objekta: Absorber, Pumpna Stanica i cevovod, glavni deo rada odnosiće se na proračun i usvajanje mašinskih instalacija koji uključuju recirkulacione radijalne centrifugalne pumpe i cevovode kojima ...postrojenje za odsumporavanje dimnih gasova, termoelektrana, pumpna stanica, FRP cevovod, Absorber, transport suspenzije gipsa, prirubnica, ventil, potisni cevovod, usisni cevovod... prečnika DN1400. Usisni cevovodi su u grafičkoj dokumentacijioznačeni: L stepen:2 TF 13/14 ZO010 IL stepen:2 TF 23/24 Z 010 II stepen:2 TF 33/34 Z 010 IV. stepen: 2 TF 43/44 Z 010zavisno od pumpe na koju su spojeni: L _ stepen:2 TF 11/I2 DOIO IL · stepen:2 TF 21/22 D 010 II stepen:2 TF ...
... FRP PNG |12906 | 2,33 b 70 093 12. |2 TE 34 Z.020 Š·@ DN1300 | · SEP FRP PNG |12906 | 2,0 b 70 093 13. |2 TE43 Z010 ŠI';ŽŽ DN1400 | · SEP FRP PNG |12906 | 2,33 b 70 093 14. |2 TE 43 Z.020 Š·@ DN1300 | · SEP FRP PNG |12906 | 2,0 b 70 093 15. |2 TEF44 Z 010 ŠI';ŽŽ DN1400 | · SEP FRP PNG |12906 | 2 ...
... |DN750 2TF24 Z 020 N-2.3 (d) N-2.2(d) | |N-2.1(d) - |N-2(d) | || ı | JEL.+20500 · |EL.+20500 ·|EL.+20500 ~ |EL.+20500 . DN750. |DN600 DN600. |DN600r 2TF33Z020 |G N-2.1(e) N-2.2 (e) |N-2.3 (e) EL.+22000 |EL.+22000 |EL.+22000 |EL.+22000 / | / | ~ |DN600 |DN600 |DN600 |DN750 2 TF 34 Z 020 N-2.3(f) ...Tomislav Trpković. Proračun recirkulacionih pumpi u postrojenju za odsumporavanje dimnih gasova ,,TENT B", 2024
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Збирка задатака из Механике 1 и Отпорности материјала
Aна Петровић, Инес Гроздановић (2023)... 4.1 3a narTy rpemy Ha CnvuvM 4.1 HaupTaTMW cTaTMuke mvjarpave (mnvjarpaM TpaHcBep3amHMX cMHMma M muMjarpaM MOMeHaTa caBujaM»a). Haro je na je q = Z% Ma=1m. M=2q·a"=4kNm Cnuka 4.1 Tlocmaeka 3a0amka, ape0a ormepeheHa Ha cagdujakbe Tpena Ha cnwuM onTepeheHa je KOHLHeHTpMCaHMM MOMeHTOM M = 2qa ...
... moMepaMbe, OBaKO HaupTaH ocnoHau je 96 CaBujaHbbe XOpM3OHTaiHO HoOkpeTaH, a WMMa peakuMjy y BepTMKaNHHOM IipaBUNy }g (Cnuka 4.3). < _ ___ b&z i Cnuka 4.3 XopuaoHmanuo nokpemHu ocnoHau B Jou! jemHOM, Ha cnMuM Cce youdaBajy omTepeheM=a: kOHUHeHTpMCaHM MOMeHT (cnper) M = 2qa? = 4kNm, KoHueHTpMcaHa ...
... orTepeheMe. VMlapauyHaBajy ce peakuuvje ocnoHaLa: ŽXFO XA=0 _+ M,=0=M- R ·2a+Ya·3a—F-4a = 2qa? – (2qa) · 2a + Yp · 3a — (qa):4a 1 YB=šqa(—Z+4+4)=an=4kN ŽYŽ:O: VA R +y -F =Vı - 2qa +2qa – qa Ya=qa=2kN Kana cy uapauyHaTe peakubuje ocioHua, 43pauyHaBa ce TpaHcBep3a;Ha cMna M MOMeOHT HO ...Aна Петровић, Инес Гроздановић. Збирка задатака из Механике 1 и Отпорности материјала, Београд : Универзитет у Београду, Рударско-геолошки факултет, 2023
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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 ...... aKaJIČMCKHM C!y/(MjaMa HOJI HaCJTOBOM: Q@W mfauofč;a CRĆA M e VAACTbe. JJG Tu MeA cfac{aiie _ Me{/O4G Koju je ypabjeH noj];, MeHTOpCTBOM ApM %l} E%Z“Q 7720 Z (ue, npe3uMe u 36atbe) 3a JlariTanHi penosnTopHjyM 3aBpmrHMx pajtona PI O-a. IIoTBp/la ce M3jaje 3a noTpeGe OJejbemwba 3a CTyJICHTCKa H HacTaBHa ...
... 10255 0.102549 0.010516 Ispunjen uslov 27 0.445229 -0.1233 0.123303 0.015204 Ispunjen uslov 28 0.487733 -0.16581 0.165807 0.027492 Ispunjen uslov z suma 9.013913 0.175477 23 3.2.2 Određivanje kohezije za visokoplastičnu glinu U tabeli broj 4 prikazani su osnovni deskriptivni parametri kohezije ...
... vrednost koeficijenta varijacije predstavljeni su na slici 11. X.w=26,14 [1 — 1,645 + (,4 * / 1+ i]=8,64k—1! 28 m' Xc„mean=26,l4[1 — 1,645 * 0,4 * \/z]=22,89k—1\2] 28 m' X.w=26,14 [1 + 1,645 + (,4 * / 1+ i]=43,65k—1! 28 m' Xc,mm=26,14[1 +1,645*0,4* F]=29,39k—“2' 28 m 24 C (kPa) - V je poznat ...Božidar Rudnjanin. Određivanje parametara smičuće čvrstoće tla primenom statističke metode, 2024
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Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)
In the late Neogene, the Pannonian Basin in Central Europe was filled with sediments when rivers from the Alps and Carpathians shed their sediment load into Lake Pannon. The most powerful source-to-sink system was that of the paleo-Danube, transporting sediments from the NW as far as the southeastern part of the lake. In the southeastern margin of the basin, however, local sedimentary systems worked in the opposite direction, against the “tide” of the prevailing N to S sediment transport. ...Dejan Radivojević, Miloš Radonjić, Lajos Tamás Katona, Imre Magyar. "Against the tide: southeast to northwest shelf-edge progradation in the southeastern margin of Lake Pannon, Banat (Serbia and Romania)" in International Journal of Earth Sciences, Springer Science and Business Media LLC (2022). https://doi.org/10.1007/s00531-022-02188-z
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Determination of Mechanical Properties of Altered Dacite by Laboratory Methods
This paper presents a methodology for determining the uniaxial and triaxial compressive strength of heterogeneous material composed of dacite (D) and altered dacite (AD). A zone of gradual transition from altered dacite to dacite was observed in the rock mass. The mechanical properties of the rock material in that zone were determined by laboratory tests of composite samples that consisted of rock material discs. However, the functional dependence on the strength parameter alteration of the rock material (UCS, intact ...... is constant up to 100% of the weaker rock material, while in Z. Mohamed et al. [4] study, the σci UCS/σci hard UCS ratio decreases linearly. In the present study, the strength decrease is significantly lesser than the one determined by Z. Mohamed et al. [4], concluding the σci UCS/σci hard UCS ratio ...
... consist of at least two lithological members and have different geomechanical properties are, in fact, the complex geotechnical problem. On the other hand, Z. Mohamed et al. [4] were the first ones who recently investigated UCS on composite samples. This study includes composites of sandstone and shale aimed ...
... gradient to about 38% of weaker rock material, leading the values to be approximately equal to intact UCS of weaker rock material. On the other hand, in Z. Mohamed et al. [4] study, the ratio was σci hard UCS/σci weak UCS = 4.4 and strength decrease has a steeper gradient to about 10% of weaker rock material ...Veljko Rupar, Vladimir Čebašek, Vladimir Milisavljević, Dejan Stevanović, Nikola Živanović. "Determination of Mechanical Properties of Altered Dacite by Laboratory Methods" in Minerals, MDPI AG (2021). https://doi.org/10.3390/min11080813
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Stanje i perspektivnost vodosnabdevanja Obrenovca i naselja opštine posle poplava, 2014. godine
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 ...... podze- mnih voda, Beograd, 1997. [3] Stevanović Z, Hajdin B. Elaborat o rezervama podzemnih voda izvorišta „Vić bare“ u Zabrežju za vodosnabdevanje Obrenovca. Fond RGF, Departman za hidrogeologiju, Beograd, 2008. [4] Polomčić D, Hajdin B, Stevanović Z, Bajić D, Hajdin K. Groundwater management by ...
... Dokmanović P, Stevanović Z, 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 ...Bojan Hajdin, Dušan Polomčić, Dragoljub Bajić. "Stanje i perspektivnost vodosnabdevanja Obrenovca i naselja opštine posle poplava, 2014. godine" in Tehnika, Beograd : Savez inženjera i tehničara Srbije (2017). https://doi.org/10.5937/tehnika1705675H
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FTIR spectroscopic study оf S-мetolachlor сorption оn inorganic and organically modified montmorillonite from Bogovina
... conjugation mode due to the distribution of double bonds and lone electron pairs (Liu et al., 2002). š š š F| ž Ž\ š L š a% 3 NaM-SM E |Eg \' 'KN z a N2 _ :1 k a ____NM /V \gp / a MNL J INRA ŠR 10'00 4000 3000 2000 Wavenumber (cm ) Ab so rb an ce Ab so rb an ce T T u 4000 3500 3000 ...
... bentonita. Hem. Ind., 62(3), 131—137. DOI: 10.2298/HEMIND0803131J 336 SERBIAN SOCIETY OF SOIL SCIENCE Soils for Furure under Global Challenges Li, Z., Jiang, Hong, H., 2008. An FIIR investigation · of hexadecyltrlmethylammomum intercalation into rectorite. Spectrochim. Acta, Part A, 71, 1525—1534 ...
... Clay Miner., 57, 392-403. DOI: 10.1346/CCMN.2009.0570311 Majdan, M., Bujacka, M., Sabah, E., Gladysz-Plaska, A., Pikus, S., Stemik, D., Komosa, Z., Padewski, A., 2009. Unexpected Difference in Phenol Sorption on PTMA - and BTIMA- «· Bentonite. J. Environ. Manage., 91, 195-205. DOI: 10.1016/J ...Lazar Kaluđerović, Zorica Tomić, Jelena Bogosavljević, Ljubomir Životić, Maja Milošević. "FTIR spectroscopic study оf S-мetolachlor сorption оn inorganic and organically modified montmorillonite from Bogovina" in Book of Proceedings / 3rd International and 15th National Congress Soils for Future Under Global Challenges, 21-24 September 2021 Sokobanja, Serbia , Belgrade : Serbian Society of Soil Science (2021)
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Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia
This paper presents LA-ICP-MS data for garnets from the Rudnik skarn deposit (Serbia), which range from Grs45–58Adr40–52Alm2–3 in the core and Adr70–97Grs2–29Sps1 in the rim displaying anisotropy and zoning. In spite of wide compositional variations the garnets near the end-member of andradite (Adr > 90) are generally isotropic. Fe-rich rims exhibit LREE depletion and flat HREE pattern with weak negative Eu anomaly, including higher As and W contents. On the other side, the Fe-poorer core shows flat REE pattern ...... Yugoslavia 1:100,000. Federal Geological Institute, Belgrade, 1–82 (in Serbian with English and Russian summaries). Brković T., Radovanović Z., Pavlović Z. & Dimitrijević M. 1980: Geological Map of Yugoslavia 1:100,000, Sheet Kragujevac. Federal Geological Institute, Belgrade. Ciobanu L.C. & Cook ...
... Geology Reviews 24, 315–370. https://doi.org/10.1016/j. oregeorev.2003.04.002 Cvetković V., Prelević D., Downes H., Jovanović M., Vaselli O. & Péskay Z. 2004: Origin and geodynamic significance of Tertiary postcollisional basaltic magmatism in Serbia (central Balkan Peninsula). Lithos 73, 161–186. ...
... mid-ocean ridge segment of the Neotethys? Geologica Carpathica 65, 117–130. https://doi.org/10.2478/ geoca-2014-0008 Cvetković V., Šarić K., Pecskay Z. & Gerdes A. 2016: The Rudnik Mts. Volcano-intrusive complex (central Serbia): An example of how magmatism controls metallogeny. Geologia Croatica 69 ...Bojan Kostić, Danica Srećković-Batoćanin, Petyo Filipov, Pavle Tančić, Kristijan Sokol. "Anisotropic grossular–andradite garnets: Evidence of two stage skarn evolution from Rudnik, Central Serbia" in Geologica Carpathica, Central Library of the Slovak Academy of Sciences (2021). https://doi.org/10.31577/GeolCarp.72.1.2
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Prostorni položaj ofiolita istočne Vardarske zone: geofizičko-geološki model i njegove geodinamičke implikacije
Dragana D. Petrović (2015-12-29)Centralni deo Balkanskog poluostrva je geotektonski veoma složen. Tetis je zatvorentokom gornjeg mezozoika, a ofioliti na zapadu i ofioliti Vardarske zone predstavljajuostatke nekadašnjih okeanskih prostora. Najistočniji deo Vardarske zone razlikuje se odsvih ostalih ofiolita na Balkanskom poluostrvu i karakteriše se najizraženijim suprasubdukcijskimafinitetom. Istočna vardarska zona locirana je u centralom delu Srbije.Na severu se prostire do Apusena u Rumuniji, a na jugu obuhvata cetralni deoMakedonije i Peonias zonu u severnoj Grčkoj. Istočna vardarska zona se nalazi istočnood geotektonske jedinice Kopaonik ...... kojoj se vrši računanje normalizovane standardne devijacije je: NSTD= [σ (∂f/∂z) ] / [σ (∂f/∂x) + σ (∂f/∂y) + σ (∂f/∂z) ] 45 gde je f intenzitet polja (magnetnog ili gravitacionog), ∂f/∂z, ∂f/∂x, ∂f/∂y, ∂f/∂z su izvodi duž pravaca, a σ je standardna devijacija. 3. 2. 1. 6. Redukcija na ...
... prevesti je u horizontalnu ravan. Produženje polja naviše je definisano formulom (Dean, 1958; Gubbins et al., 2007): F=e -│k│z gde je │k│ = 2πλ talasni broj, λ talasna dužina, z nivo produženja. U horizontalnoj ravni, gde je visina 0, stvara se novo polje gde se površinska raspodela uzima u vidu ...
... 62 Slika 23. Karta Z komponente za područje Makedonije, (crne linije ukazuju na položaj profila na području Demir Kapije, poligonom je naznačeno uže područje istraživanja), položaj prikazan na Slici 20 63 Slika 24. Geomagnetska karta Z komponente užeg područja na prostoru ...Dragana D. Petrović. "Prostorni položaj ofiolita istočne Vardarske zone: geofizičko-geološki model i njegove geodinamičke implikacije" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2015-12-29)
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Review: Methodological approaches and research techniques for addressing construction and remediation problems in karst reservoirs
Saša Milanović, Ljiljana Vasić (2021)Saša Milanović, Ljiljana Vasić. "Review: Methodological approaches and research techniques for addressing construction and remediation problems in karst reservoirs" in Hydrogeology Journal, Springer Science and Business Media LLC (2021). https://doi.org/10.1007/s10040-020-02280-1
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Aлтерације перидотита контролисане карактером флуида на примеру харцбургита Рудника - Серпентинизација или талкизација?
Стефан Петровић, Наталија Батоћанин (2020)У раду су приказани резултати испитивања серпентинисаних харцбургита Брђана (43°58'45.1" СГШ, 20°25'12.6" ИГД) и талкизираних харцбургита откривених у интервалу 429-559.8 m у истражној бушотини 330А/18 (44°07'33.2" СГШ, 20°30'28.5" ИГД) на Руднику. Узорци оба локалитета показују карактеристике резидуалних харцбургита из омотача, односно тектонита; лепидобластичне, бластозрнасте, или порфирокластичне структуре и масивне текстуре. Серпентинисани харцбургити и серпентинити Брђана су изграђени од серпентина, ретких реликата оливина и ортопироксена, акцесорног спинела, и веома ретког секундарног магнезита и магнетита. Најдоминантнији састојак (местимично гради и преко ...... UROŠEVIĆ, M., TRIFUNOVIĆ, S., RADOVANOVIĆ, Z., BOŽANIĆ, M. (1970): Osnovna geološka karta 1:100.000, list Čačak K 34-5. Zavod za geološka i geofizička ispitivanja, Beograd BRKOVIĆ, T., MALEŠEVIĆ, M., UROŠEVIĆ, M., TRIFUNOVIĆ, S., RADOVANOVIĆ, Z., PAVLOVIĆ, Z., RAKIĆ, M. (1978): Tumač za list Čačak ...
... faculty publications available in open access, as well as the employees' publications. - The Repository is available at: www.dr.rgf.bg.ac.rs 15 Z A P I S N I C I S R P S K O G G E O L O [ K O G D R U [ T V A za 2019. godinu COMPTES RENDUS DES SÉANCES DE LA SOCIÉTÉ SERBE DE GÉOLOGIE pour ...
... Geological Survey professional paper, 384-A, pp. 99. United States Government Printing office, Washington. FILIPOVIć, I., MARKOVIĆ, B., PAVLOVIĆ, Z., RODIN, V., MARKOVIĆ, O. (1978): Osnovna geološka karta SFRJ 1:100000. Tumač za list Gornji Milanovac L34-137. Savezni geološki zavod, Beograd. ...Стефан Петровић, Наталија Батоћанин. "Aлтерације перидотита контролисане карактером флуида на примеру харцбургита Рудника - Серпентинизација или талкизација?" in Записници српског геолошког друштва, Српско геолошко друштво, Београд (2020)
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Determining the Groundwater Balance and Radius of Influence Using Hydrodynamic Modeling: the Case Study of the Groundwater Source “Šumice” (Kikinda, Serbia)
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 ...... , Stevanović, Z., Bajić, D., Hajdin, K, Groundwater Management by Riverbank Filtration and an Infiltration Channel: The Case of Obrenovac, Serbia, Hydrogeology Journal, Vol. 21, No. 7, pp1519-1530, 2013, http://dx.doi.org/10.1007/s10040-013-1025-9 5. Stauder, S., Stevanović, Z., Richter, C. et ...
... Development of the Republic of Serbia for financing projects OI-176022, TR-33039 and III-43004. REFERENCES 1. Hajdin, B., Polomčić, D., Stevanović, Z., Bajić, D. and Hajdin, K., Asseings Prospect of Groundwater Source „Vić Bare“ for Obrenovac’s Water Supply, Proceedings of the XIV Serbian Symposium ...
... Management, Vol. 26, No. 2, pp 581-594, 2012, http://dx.doi.org/10.1007/s11269-011-9932-9 6. Polomčić, D., Đekić, M., Milosavljević, S., Popović, Z., Milaković, M., Ristić Vakanjac, V., Krunić, O., Sustainable use of Groundwater Resources in Terms of increasing the Capacity of Two Interconnected ...Dušan Polomčić, Dragoljub Bajić, Jelena Zarić. "Determining the Groundwater Balance and Radius of Influence Using Hydrodynamic Modeling: the Case Study of the Groundwater Source “Šumice” (Kikinda, Serbia)" in Journal of Sustainable Development of Energy, Water and Environment Systems (2015). https://doi.org/10.13044/j.sdewes.2015.03.0017