Претрага
828 items
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Geology of South-Eastern Europe
Cvetković Vladica, Prelević Dejan, Schmid, S."". "Geology of South-Eastern Europe" in Mineral and thermal waters of South-Eastern Europe, :Springer Verlag (2016)
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Dating intrusion and cooling of Cenozoic granitoids in the Dinarides of Southern Serbia and discussion of the geodynamic setting of Paleocene-Miocene magmatism in the Balkan Peninsula.
Schefer S., Cvetković Vladica, Fügenschuh Bernhard, Kounov A., Ovtcharova M., Schaltegger U., Schmid S. (2010)Schefer S., Cvetković Vladica, Fügenschuh Bernhard, Kounov A., Ovtcharova M., Schaltegger U., Schmid S.. "Dating intrusion and cooling of Cenozoic granitoids in the Dinarides of Southern Serbia and discussion of the geodynamic setting of Paleocene-Miocene magmatism in the Balkan Peninsula." in Geophysical Research Abstracts 12, Vienna, Austria:EGU (2010): 2530-2530
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The Late Cretaceous Klepa basalts in Macedonia (FYROM) - Constraints on the final stage of Tethys closure in the Balkans
Dejan Prelević, S. Wehrheim, M. Reutter, Romer, R.L., Blažo Boev, Milica Božović, P. van den Bogaard, Vladica Cvetković, Stefan M. Schmid (2017)Dejan Prelević, S. Wehrheim, M. Reutter, Romer, R.L., Blažo Boev, Milica Božović, P. van den Bogaard, Vladica Cvetković, Stefan M. Schmid. "The Late Cretaceous Klepa basalts in Macedonia (FYROM) - Constraints on the final stage of Tethys closure in the Balkans" in Émile Argand Conference - 13th Workshop on Alpine Geological Studies - September 7th-18th 2017 in Serbia, Zlatibor Mts., Beograd:University of Belgrade - Faculty of Mining and Geology (2017): 87-87
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Middle Jurassic radiolarian assemblages from the sedimentary cover of the Adriatic margin (Zlatar Mountain, SW Serbia)
Đerić Nevenka, Schmid Stefan, Gerzina Nataša. "Middle Jurassic radiolarian assemblages from the sedimentary cover of the Adriatic margin (Zlatar Mountain, SW Serbia)" in Bulletin de La Societe Geologique de France 4 no. 183, Paris:La Societe Geologique de France (2012): 359-368
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Mesozoic Radiolarians from the Dinarides (Bosnia and Serbia)
Đerić Nevenka, Vishnevskaya Valentina, Schmid Stefan, Gerzina Nataša. "Mesozoic Radiolarians from the Dinarides (Bosnia and Serbia)" in Зборник радова 15. конгреса геолога Србије са међународним учешћем, Београд, [26-29 мај] 2010. = Proceedings of the 15th Congress of Geologists of Serbia with International Participation, Belgrade [26-29 May] 2010, Beograd:Srpsko geološko društvo (2010): 154-154
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Mesozoic Radiolarians from the Dinarides (Serbia and Bosnia)
Đerić Nevenka, Schmid Stefan, Vishnevskaya Valentina, Gerzina Nataša. "Mesozoic Radiolarians from the Dinarides (Serbia and Bosnia)" in Proceedings of the 19th Congress of the Carpathian Balkan Geological Association, Thessaloniki, Greece, 23-26 September 2010, (Abstract Volume), Geologica Balcanica, Sofia:Carpathian-Balkan Geological Association (2010): 95-95
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New radiolarian data from the Jurassic ophiolitic mélange of Avala Mountain (Serbia, Belgrade Region)
Nikita Bragin, Liubov Bragina, Nataša Gerzina Spajić, Nevenka Đerić, Stefan Schmid. "New radiolarian data from the Jurassic ophiolitic mélange of Avala Mountain (Serbia, Belgrade Region)" in Swiss Journal of Geosciences (2019)
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Cenozoic granitoids in the Dinarides of southern Serbia: age of intrusion, isotope geochemistry, exhumation history and significance for the geodynamic evolution of the Balkan Peninsula
Schefer Senecio, Cvetković Vladica, Fugenschuh Bernhard, Kounov Alexandre, Ovtcharova Maria, Schaltegger Urs, Schmid Stefan M. (2011)Schefer Senecio, Cvetković Vladica, Fugenschuh Bernhard, Kounov Alexandre, Ovtcharova Maria, Schaltegger Urs, Schmid Stefan M.. "Cenozoic granitoids in the Dinarides of southern Serbia: age of intrusion, isotope geochemistry, exhumation history and significance for the geodynamic evolution of the Balkan Peninsula" in International Journal Earth Sci (Geol Rundsch) 100 no. 5, Heidelberg, Germany:Springer-Verlag (2011): 1181-1206. https://doi.org/10.1007/s00531-010-0599-x
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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.... c lu s io n o f c a te g o r ie s s u c h a s d e m o n y m s (D E M O ), p ro fe s s io n s a n d t i t le s (R O L E ) , w o rk s o f a r t (W O R K ) in th e ta g s e t , a lo n g s id e m o re c a n o n ic a l c a te g o r ie s , s u c h a s p e r - s o n n a m e s (P E ...
... r iv a te s p a c e o f a b o u rg e o is h o m e , s o m e th in g w h ic h d e m a n d s re s e a rc h e rs to b e a b le to d e te c t in d ic a to r s o f so c ia l s tru c tu re a n d ro le s , su c h a s h o n o r if ic s , n a m e s o f p ro fe s s io n s , e tc . ...
... ita l le t te r s in th e b e g in n in g o f s e n te n c e s , a n d it re c o g n is e s e n ti t ie s c o m p o s e d o f m o re th a n 4 to k e n s , w h ic h a re a c tu a lly ra re . Serbian: S rp N E R is a ru le b a s e d s y s te m a n d th e b e s t N E R to o ...Francesca Frontini, Carmen Brando, Joanna Byszuk, Ioana Galleron, Diana Santos, Ranka Stanković. "Named Entity Recognition for Distant Reading in ELTeC" in CLARIN Annual Conference 2020, Oct 2020, Virtual Event, France, CLARIN (2020)
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Developing Termbases for Expert Terminology under the TBX Standard
... ❢r♦♠ t❡r♠❜❛s❡s ❛s ❝❡♥tr❛❧ r❡s♦✉r❝❡s ✐♥ ❛ ❝✉st♦♠ ✐♥✲❤♦✉s❡ s❝❤❡♠❡ t♦ st❛♥❞❛r❞ ❢♦r♠❛ts s✉❝❤ ❛s ❚❇❳ ❤❛s ❜❡❡♥ ♣r♦✈✐❞❡❞✱ ❜② ❛ ✇✐③❛r❞ ✐♥t❡❣r❛t❡❞ ✐♥ t❤❡ t❡r♠✐♥♦❧♦❣✐❝❛❧ ✐♥❢♦r♠❛t✐♦♥ s②st❡♠ s✉♣♣♦rt✐♥❣ t❤❡ t❡r♠❜❛s❡s✳ ❑❡②✇♦r❞s✿ ❚❡r♠❜❛s❡s✱ ❚❇❳ st❛♥❞❛r❞✱ ▲❛♥❣✉❛❣❡ ❘❡s♦✉r❝❡s✱ ❚❡r♠✐♥♦❧✲ ♦❣② ■♥t❡❣r❛t✐♦♥ ❛♥❞ P♦rt❛❜✐❧✐t② ...
... ❣❡♥❡r❛t❡❞ t♦ s♦❧✈❡ ♣r♦❜❧❡♠s✳ ❚♦ t❤❛t ❡♥❞ t❤❡② ❤❛✈❡ t♦ ❞❡s❝r✐❜❡ r❡❛❧ ❞❛t❛ ❛♥❞ ♠✉st ❜❡ ✐♥t❡r♥❛❧❧② ❝♦♥s✐st❡♥t ❬✷❪✳ ❇❡s✐❞❡s ❜❡✐♥❣ ✉s❡❞ ❢♦r tr❛♥s❧❛t✐♦♥ ♣✉r♣♦s❡s✱ t❡r♠❜❛s❡s ❞❡✈❡❧♦♣❡❞ ❛t ❋▼● ❛r❡ t❤✉s ✉s❡❞ ❢♦r ❝♦♥tr♦❧ ♦❢ ❞♦♠❛✐♥ ✈❛❧✉❡s✱ ❝❧❛ss✐✲ ✜❝❛t✐♦♥ ❛♥❞ s❡❛r❝❤ ✇✐t❤✐♥ ♠✐♥✐♥❣ ❛♥❞ ❣❡♦❧♦❣✐❝❛❧ s♦❢t✇❛r❡ s②st❡♠s✳ ✷✳✶ ...
... ✈❡rs✐♦♥ ✇❛s ✉s❡❞✱ r❛t❤❡r t❤❛♥ ❚❇❳ ❇❛s✐❝✱ ❛s ✐t ✐s ♠♦r❡ s✉✐t❛❜❧❡ ❢♦r ❝♦♠♣♦✉♥❞s✱ ✇✐t❤ ✐♥✢❡❝t✐♦♥❛❧ ❝❤❛r❛❝t❡r✐st✐❝s ♠♦r❡ ❝♦♠♣❧❡① t❤❛♥ t❤♦s❡ ♦❢ s✐♥❣❧❡ ✇♦r❞s✳ ◆❛♠❡❧②✱ ❚❇❳ ❇❛s✐❝ ❛❧❧♦✇s ❛ ❧✐♠✐t❡❞ s❡t ♦❢ ❞❛t❛ ❝❛t❡❣♦r✐❡s ❛♥❞ ❝❛♥♥♦t ❛❝❝❡♣t ♠♦r♣❤♦❧♦❣✐❝❛❧ ❛♥❞ s♦♠❡ ♦t❤❡r ✐♠♣♦rt❛♥t ✐♥❢♦r♠❛t✐♦♥✳ ❆❧❧ ❧❛♥❣✉❛❣❡s ✉s❡❞ ✐♥ ❛ ...Ranka Stanković, Ivan Obradović, and Miloš Utvić. "Developing Termbases for Expert Terminology under the TBX Standard" in Natural Language Processing for Serbian - Resources and Applications, Belgrade : University of Belgrade, Faculty of Mathematics (2014)
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Оптимизација управљања процесима рекултивације површинских копова угља
Bojan S. Dimitrijević (2014-05-30)Ширење површинске експлоатације минералних сировина а нарочито енергетских ресурсафосилних горива, чине површинске копове угља просторно доминантним објектима великих рударскихбасена како у нас тако и у свету. Експлоатациона активност, прати негативне еколошке утицаје наживотну средину шире околине, што нас обавезује на интегрално планирање, ревитализацију,рекултивацију и уређење нарушеног простора за његово поновно хумано коришћење упостексплоатационом периоду. Постексплоатационо санирање и уређење предела површинских коповаи одлагалишта односно нарушеног простора изазваног рударским радовима и пратећих објеката,представља синтетички мултидисциплинарно-интердисциплинаран веома комплексан вишефазниинжењерски пројектни задатак.У уводном ...рекултивација, постексплоатациони предео, површински коп угља,вишеатрибутна анализа, одлучивање, процеси, рекултивационо решење... as) s = 2 x = 7 - 4 = 3 1 s = 3 x = 7 - 5 = 2 1 s = 4 x = 7 - 4 = 3 1 s = 5 x = 7 - 7 = 0 0 s = 6 x = 7 - 7 = 0 0 s = 7 x = 7 - 4 = 3 1 s = 8 x = 7 - 4 = 3 1 s = 9 x = 7 - 4 = 3 1 s = 10 x = 7 - 1.5 = 5.5 1 a2, as x = k2(a2) - k2(as) P2(a2, as) s = 1 x = 4 - 7 = -3 0 s = 3 x = ...
... -1 0 s = 4 x = 4 - 4 = 0 0 s = 5 x = 4 - 7 = -3 0 s = 6 x = 4 - 7 = -3 0 s = 7 x = 4 - 4 = 0 0 s = 8 x = 4 - 4 = 0 0 s = 9 x = 4 - 4 = 0 0 s = 10 x = 4 - 1.5 = 2.5 1 a3, as x = k2(a3) - k2(as) P2(a3, as) s = 1 x = 5 - 7 = -2 0 s = 2 x = 5 - 4 = 1 1 s = 4 x = 5 - 4 = 1 1 s = 5 x ...
... 189 s = 2 x = 4 - 4 = 0 0 s = 3 x = 4 - 5 = -1 0 s = 5 x = 4 - 7 = -3 0 s = 6 x = 4 - 7 = -3 0 s = 7 x = 4 - 4 = 0 0 s = 8 x = 4 - 4 = 0 0 s = 9 x = 4 - 4 = 0 0 s = 10 x = 4 - 1.5 = 2.5 1 a5, as x = k2(a5) - k2(as) P2(a5, as) s = 1 x = 7 - 7 = 0 0 s = 2 x = 7 - 4 = 3 1 s = 3 x ...Bojan S. Dimitrijević. "Оптимизација управљања процесима рекултивације површинских копова угља" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2014-05-30)
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A Knowledge-Based Approach to Mine Ventilation Planning in Yugoslav Mining Practice
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 ...... 4 m 3 /s 2 7 ,7 m 3 /s 5,7 m 3 /s 1 1 ,7 m 3 /s 1 6 ,1 m 3 /s 1 6 ,1 m 3 /s 1 1 ,6 m 3 /s 3 3 ,4 m 3 /s 9,0m 3 /s 42,4 m3 /s 33,4 m 3 /s 3 4 5 6 7 8 1 0 4 ,4 m 3 /s 8 ,9 m 3 /s 6 ,8 m 3 /s 4 ,4 m 3 /s 2 ,8 m 3 /s 2 7 ,7 m 3 /s 1 6 ,1 m 3 /s - ...
... / s 3 2 .1 0 m / s 3 9 .3 9 2 2 N s /m 2 8 0 .0 0 0 1 N s /m 2 8 0 .0 7 5 6 N s /m 2 8 1 3 .3 0 m / s 3 2 .8 0 m / s 3 8 .2 1 0 4 N s /m 2 8 5 .7 0 m / s 3 6 .0 5 2 3 N s /m 2 8 0 .0 0 9 3 N s /m 2 82 7 .7 0 m / s 3 0 .0 6 9 3 N s /m ...
... .4 1 0 6 N s /m 2 8 3 4 .4 0 m / s 3 1 8 .2 2 m / s 3 0 .0 3 4 7 N s /m 2 80 .8 6 4 5 N s /m 2 8 2 .8 7 9 1 N s /m 2 8 1 0 .6 4 m / s 3 8 .1 m / s 3 0 .1 4 m / s 3 9 .0 3 3 9 N s /m 2 8 0 .0 0 0 1 N s /m 2 8 0 .0 7 5 6 N s /m 2 8 1 6 ...Nikola Lilić, Ivan Obradović, Ranka Stanković. "A Knowledge-Based Approach to Mine Ventilation Planning in Yugoslav Mining Practice" in Mineral Resources Engineering 11 no. 4, Imperial College Press (2002): 361-382. https://doi.org/10.1142/S0950609802001014
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A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia
Radosavljević Slobodan, Stojanović Jovica, Pačevski Aleksandar, Radosavljević-Mihajlović Ana, Kašić Vladan (2016)Radosavljević Slobodan, Stojanović Jovica, Pačevski Aleksandar, Radosavljević-Mihajlović Ana, Kašić Vladan. "A review of Pb-Sb(As)-S, Cu(Ag)-Fe(Zn)-Sb(As)-S, Ag(Pb)-Bi(Sb)-S and Pb-Bi-S(Te) sulfosalt systems from the Boranja orefield, West Serbia" in Geološki anali Balkanskoga poluostrva 77, Beograd :Rudarsko-geološki fakultet (2016): 1-12. https://doi.org/10.2298/GABP1677001R
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Multivarijabilni modeli upravljanja u rudarstvu
Marjan M. Hudej (2014-02-03)osetljivost i rizik. Više pobuda generiše ovakvu atribuciju. Prva je, multivarijabilnostambijentalnih uslova i funkcionalna i strukturna složenost rudarskih sistema (čovek -priroda (radna sredina) - mašina – okruženje); Druga se odnosi na ne postojanje opštenaučne saglasnosti oko ocene pogodnosti modela za podršku odlučivanju i upravljanje.Treća, ako bi saglasnost i postojala, nije sigurno da bi raspoloživi modeli, metode i taktike,dale ekvivalentne rezultate za iste rudničke uslove. Četvrta, sistemske nauke još uveknemaju opšte prihvaćen i u praksi primenljiv algoritam izbora najboljeg rešenja ...... as) s = 2 x = 8 - 10 = -2 1 s = 2 x = 8 - 8 = 0 0 s = 3 x = 8 - 12 = -4 1 s = 3 x = 8 - 5 = 3 1 s = 4 x = 8 - 12 = -4 1 s = 4 x = 8 - 4 = 4 1 a2, as x = k3(a2) - k3(as) P3(a2, as) a2, as x = k4(a2) - k4(as) P4(a2, as) s = 1 x = 10 - 8 = 2 0 s = 1 x = 8 - 8 = 0 0 s = 3 x ...
... -2 1 s = 3 x = 8 - 5 = 3 1 s = 4 x = 10 - 12 = -2 1 s = 4 x = 8 - 4 = 4 1 a3, as x = k3(a3) - k3(as) P3(a3, as) a3, as x = k4(a3) - k4(as) P4(a3, as) s = 1 x = 12 - 8 = 4 0 s = 1 x = 5 - 8 = -3 0 s = 2 x = 12 - 10 = 2 0 s = 2 x = 5 - 8 = -3 0 s = 4 x = 12 - 12 = 0 0 s = 4 x ...
... as) s = 2 x = 7 - 8 = -1 0 s = 3 x = 7 - 6 = 1 1 s = 4 x = 7 - 6 = 1 1 a2, as x = k5(a2) - k5(as) P5(a2, as) s = 1 x = 8 - 7 = 1 1 s = 3 x = 8 - 6 = 2 1 s = 4 x = 8 - 6 = 2 1 a3, as x = k5(a3) - k5(as) P5(a3, as) s = 1 x = 6 - 7 = -1 0 s = 2 x = 6 - 8 = -2 0 s = 4 ...Marjan M. Hudej. "Multivarijabilni modeli upravljanja u rudarstvu" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2014-02-03)
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Multivarijabilni modeli upravljanja u rudarstvu
Marjan M. Hudej (2014-02-03)osetljivost i rizik. Više pobuda generiše ovakvu atribuciju. Prva je, multivarijabilnostambijentalnih uslova i funkcionalna i strukturna složenost rudarskih sistema (čovek -priroda (radna sredina) - mašina – okruženje); Druga se odnosi na ne postojanje opštenaučne saglasnosti oko ocene pogodnosti modela za podršku odlučivanju i upravljanje.Treća, ako bi saglasnost i postojala, nije sigurno da bi raspoloživi modeli, metode i taktike,dale ekvivalentne rezultate za iste rudničke uslove. Četvrta, sistemske nauke još uveknemaju opšte prihvaćen i u praksi primenljiv algoritam izbora najboljeg rešenja ...... as) s = 2 x = 8 - 10 = -2 1 s = 2 x = 8 - 8 = 0 0 s = 3 x = 8 - 12 = -4 1 s = 3 x = 8 - 5 = 3 1 s = 4 x = 8 - 12 = -4 1 s = 4 x = 8 - 4 = 4 1 a2, as x = k3(a2) - k3(as) P3(a2, as) a2, as x = k4(a2) - k4(as) P4(a2, as) s = 1 x = 10 - 8 = 2 0 s = 1 x = 8 - 8 = 0 0 s = 3 x ...
... -2 1 s = 3 x = 8 - 5 = 3 1 s = 4 x = 10 - 12 = -2 1 s = 4 x = 8 - 4 = 4 1 a3, as x = k3(a3) - k3(as) P3(a3, as) a3, as x = k4(a3) - k4(as) P4(a3, as) s = 1 x = 12 - 8 = 4 0 s = 1 x = 5 - 8 = -3 0 s = 2 x = 12 - 10 = 2 0 s = 2 x = 5 - 8 = -3 0 s = 4 x = 12 - 12 = 0 0 s = 4 x ...
... as) s = 2 x = 7 - 8 = -1 0 s = 3 x = 7 - 6 = 1 1 s = 4 x = 7 - 6 = 1 1 a2, as x = k5(a2) - k5(as) P5(a2, as) s = 1 x = 8 - 7 = 1 1 s = 3 x = 8 - 6 = 2 1 s = 4 x = 8 - 6 = 2 1 a3, as x = k5(a3) - k5(as) P5(a3, as) s = 1 x = 6 - 7 = -1 0 s = 2 x = 6 - 8 = -2 0 s = 4 ...Marjan M. Hudej. "Multivarijabilni modeli upravljanja u rudarstvu" in Универзитет у Београду, Универзитет у Београду, Рударско-геолошки факултет (2014-02-03)
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Polyhedral characteristics of the cosalite-type crystal structures
Sabina Kovač, Predrag Dabić, Aleksandar Kremenović, Aleksandar Pačevski, Ljiljana Karanović, Marko V. Rodić, Martina Tribus (2019)Sabina Kovač, Predrag Dabić, Aleksandar Kremenović, Aleksandar Pačevski, Ljiljana Karanović, Marko V. Rodić, Martina Tribus. "Polyhedral characteristics of the cosalite-type crystal structures" in The Canadian Mineralogist, Mineralogical Association of Canada (2019). https://doi.org/10.3749/canmin.1900017
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Threshold-induced correlations in the Random Field Ising Model
... obtained using − ∝ − σg T T T T( / ) exp[ ( / ) ] T 0 0 T , and − ∝ − σg S S S S( / ) exp[ ( / ) ] S 0 0 S , where σT and σS are the cuto� exponents whose values are close to 1 for all the distributions being analysed. �e average size 〈S〉T of subavalanches with duration T is shown against T in the main panel ...
... time, respectively. �ese numbers obey: = =− ˆ ˆn T b b V n T V n b S b V n S V( / ; ) ( ; ), ( ; ) ( ; ), (8)i T x i T i S x x i S S ( ) th ( ) th S ( ) 1 th ( ) th b b =ˆn T b b V n T V( / ; ) ( ; ), (9)i T x i T S ( ) int th ( ) int th b int int = = .ˆ ˆn T b b V n T V n T b b ...
... We found that in a wide range of thresholds, both types of distribution follow power-laws = −τ−D T T g T T( ) ( / ) T 0 T and = −τ−D S S g S S( ) ( / ) S 0 S , terminated by the cuto� scaling functions gT(x) and gS(x) for duration and size, respectively. �e cuto� time T0, and the cuto� size S0 ...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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FTIR spectroscopic study оf S-мetolachlor сorption оn inorganic and organically modified montmorillonite from Bogovina
... š š |} š ii s e š H || i š } ž Š | e š - H H 1 a Fi i i NMA 41 “0 — s%0 ~ 300 ~ 3%0 __3MO _1%O0 _ 4M00 00 400 30 3000 3800 2000 Wavenumber (cm') Wavenumber (cm') šžg C), &h ı NA d) . HDTMA š A OE ii |} “ LIJPI | Mig ~FML_R “ š |- L šš s i s BOA A H || s|--38 8 P A g s - | „ihi š š ...
... 1000 500 Wavenumber (cm ) Figure 2. FTIR spectra of: a) S-metolachlor, Na -montmorillonite and Na -montmorillonite with adsorbed S-metolachlor; b) HDTMA-montmorillonite with adsorbed S-metolachlor; c) PTMA- montmorillonite with adsorbed S-metolachlor 334 SERBIAN SOCIETY OF SOIL SCIENCE |___H ...
... Sorption of S-metolachlor molecules on PTMA-montmorillonite takes place through the interaction between the aromatic benzene ring of S-metolachlor and the aromatic benzene ring of the organic complex (nm-n bonds). Also, the formation of a hydrogen bond occurs between the molecules of S-metolachlor ...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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Optimisation of underground mine decline development system using genetic algorithm
... , , , , , , , ,s s s s s s s s sf x y z x y z f x y z f x y z x y z f x y z (2) where 2 2 2 1 1 , , n i i i i i i i f x y z c R x x y y z z (3) 2 2 2 2 1 , , , , , n s s s d i s s s i f x y z x y ...
... 2 2 2 3 1 , , n s s s s i m s m s m s i f x y z s c R x x y y z z (5) has to be minimized, subject to max 2 2 i i i z z r x x y y (6) max 2 2 s s s z z r x x y y ...
... (7) max 2 2 m s m s m s z z x x y y (8) min max s s sx x x (9) min max s s sy y y (10) min max s s sz z z (11) where x, y, z - location (coordinates) of the ...Zoran Gligorić, Aleksandar Ganić, Rade Tokalić, Aleksandar Milutinović. "Optimisation of underground mine decline development system using genetic algorithm" in Underground mining engineering, Beograd : Univerzitet u Beogradu – Rudarsko–geološki fakultet (2014)
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Smanjenje sleganja plitkih temelja primenom mikrošipova
Slobodan Ćorić, Dragoslav Rakić (2021)Mikrošipovi su šipovi malog prečnika koji se grade tako što se u tlu specijalni postupkom formira bušotina koja se zatim armira i injektira. Njihov prečnik je najčešće 150 – 300 mm, a dužina može da bude i više desetina metara. Mikrošipovi mogu da se grade u svim vrstama tla i mogu da budu vertikalni i kosi. Oni se, stoga, koriste kao zamena za konvencionalne šipove i ankere. Primena mikrošipova u fundiranju predstavlja jedan savremeni način izgradnje i sanacije temelja/objekata. ...Slobodan Ćorić, Dragoslav Rakić. "Smanjenje sleganja plitkih temelja primenom mikrošipova" in Zbornik radova međunarodno naučno-stručnog savetovanja Zemljotresno inženjerstvo i geotehnički aspekti građevinarstva, Vrnjačka banja, 3-5. novembar 2021., Beograd : Savez građevinskih inženjera Srbije (2021)