Development of new information and communication technologies, based on advanced mathematical methods, with applications in medicine, telecommunications, power systems, protection of national heritage and education

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Development of new information and communication technologies, based on advanced mathematical methods, with applications in medicine, telecommunications, power systems, protection of national heritage and education (en)
Развој нових информационо-комуникационих технологија, коришћењем напредних математичких метода, са применама у медицини, телекомуникацијама, енергетици, заштитити националне баштине и образовању (sr)
Razvoj novih informaciono-komunikacionih tehnologija, korišćenjem naprednih matematičkih metoda, sa primenama u medicini, telekomunikacijama, energetici, zaštititi nacionalne baštine i obrazovanju (sr_RS)
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Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije

Beloica, Jelena R.

(Univerzitet u Beogradu, Šumarski fakultet, 2015)

TY  - THES
AU  - Beloica, Jelena R.
PY  - 2015
UR  - https://nardus.mpn.gov.rs/handle/123456789/5038
UR  - http://eteze.bg.ac.rs/application/showtheses?thesesId=2647
UR  - https://fedorabg.bg.ac.rs/fedora/get/o:10742/bdef:Content/download
UR  - http://vbs.rs/scripts/cobiss?command=DISPLAY&base=70036&RID=513376412
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/24
AB  - Acidifikacija je proces smanjenja pH vrednosti zemljišta i rezultat je brojnih biogeohemijskih procesa. U vlažnim i umerenim klimatskim zonama, acidifikacija je prirodan proces uslovljen hemizmom mineralne faze zemljišta, tipom vegetacije i klimom. U prirodnim uslovima ovaj proces je dugotrajan i deo je procesa razvoja zemljišta, zbog čega se ne može posmatrati kao proces degradacije. Dejstvom antropogenog faktora, prekomernim emisijama sumpora i azota, neadekvatnim sistemima upravljanja, promenom načina korišćenja zemljišta, kao i globalnih klimatskih promena, proces acidifikacije može biti znatno ubrzan i intenziviran. U ovom kontekstu acidifkacija zemljišta predstavlja oblik hemijske degradacije zemljišta. Acidifkacija zemljišta, izazvana depozicijama sumpora i azota, zbog negativnih efekata na vitalnost prirodnih ekosistema i biodiveritet poslednjih 70 godina, je dostigla status ekološkog problema globalnih razmera. Na području istočne Srbije u šumskim i ekosistemima visoko-planinskih pašnjaka, acidifikacija zemljišta dovodi do smanjenja kvaliteta zemljišta kao resursa i prirodnog dobra. Nagle promene hemizma zemljišta izazvane kiselim depozicijama direktno i indirektno utiču na destrukciju prirodnih staništa, što vodi do trajnog gubitka ekoloških i socio-ekonomskih funkcija ekosistema. U okviru ovog rada definisani su trendovi depozicija sumpora i azota kao i njihova veza sa osetljivošću zemljišta na proces acidifikacije i izdvojene su aktuelne i potencijalne zone rizika degradacije zemljišta. Procena stepena osetljivosti zemljišta šumskih i visoko-planinskih pašnjačkih ekosistema prema procesu acidifikacije, izvršena je metodom za proračun kritičnih opterećenja primenom VSD modela. Kritična opterećenja i prekoračenja zagađujućih materija u vazduhu predstavljaju jedan od glavnih indikatora osetljivosti šumskih i drugih terestričnih ekosistema i predstavljaju osnovu za održivo upravljanje ekosistemima kao osnovnih principa međunarodnog ekološkog prava i nacionalne politike...
AB  - Acidification is a process of decreasing soil pH value over time as a result of numerous biogeochemical processes. In humid and temperate climatic zones, acidification is a natural process caused by soil mineral phase, vegetation type and climate. Under natural conditions, this is a long term process of soil development which can not be seen as a process of land degradation.The influence of anthropogenic factors, excessive emissions of sulphur and nitrogen, inadequate ecosystem management, land use changes, as well as global climate change, acidification process can be significantly accelerated and intensified. In this context, soil acidification is a form of soil chemical degradation. Acidification induced by deposition of sulphur and nitrogen, due to the negative effects on natural ecosystems and biodiversity loss in the past 70 years, has become a global environmental problem. In forest and highland grasslands of Eastern Serbia soil acidification leads to a reduction/loss of soil quality, as resource and natural good. Rapid change of soil chemistry caused by acidic deposition directly and indirectly leads to destruction of natural habitats, and disturbance of environmental and socioeconomic functions of ecosystems. In this paper were defined trends of sulphur and nitrogen deposition, their relationship with the soil sensitivity to acidification as well as current and potential soil degradation risk areas. Assessment of soil sensitivity to acidification of forest and high mountain grasslands, were performed by using critical load concept and VSD model. Critical loads and exceedances of air pollutants are one of the main indicators of forest and terrestrial ecosystem sensitivity to acidification. The critical load concept can be considered as a tool for integrated monitoring of air pollution effects on ecosystems and fundamental principle of international environmental law and national clean air policy. Different ecosystem vulnerability zones to air pollutants were performed and based on soil sensitivity and concentrations of sulphur and nitrogen deposition for the period 1980-2009. The interdependence of soil properties and factors with the greatest impact on soil acidification were singled out by applying the method of simple and multiple regression, as well as factor analysis...
PB  - Univerzitet u Beogradu, Šumarski fakultet
T1  - Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije
T1  - Acidification process as a factor of soil degradation in eastern Serbia.
UR  - https://hdl.handle.net/21.15107/rcub_nardus_5038
UR  - t-5034
ER  - 
@phdthesis{
author = "Beloica, Jelena R.",
year = "2015",
abstract = "Acidifikacija je proces smanjenja pH vrednosti zemljišta i rezultat je brojnih biogeohemijskih procesa. U vlažnim i umerenim klimatskim zonama, acidifikacija je prirodan proces uslovljen hemizmom mineralne faze zemljišta, tipom vegetacije i klimom. U prirodnim uslovima ovaj proces je dugotrajan i deo je procesa razvoja zemljišta, zbog čega se ne može posmatrati kao proces degradacije. Dejstvom antropogenog faktora, prekomernim emisijama sumpora i azota, neadekvatnim sistemima upravljanja, promenom načina korišćenja zemljišta, kao i globalnih klimatskih promena, proces acidifikacije može biti znatno ubrzan i intenziviran. U ovom kontekstu acidifkacija zemljišta predstavlja oblik hemijske degradacije zemljišta. Acidifkacija zemljišta, izazvana depozicijama sumpora i azota, zbog negativnih efekata na vitalnost prirodnih ekosistema i biodiveritet poslednjih 70 godina, je dostigla status ekološkog problema globalnih razmera. Na području istočne Srbije u šumskim i ekosistemima visoko-planinskih pašnjaka, acidifikacija zemljišta dovodi do smanjenja kvaliteta zemljišta kao resursa i prirodnog dobra. Nagle promene hemizma zemljišta izazvane kiselim depozicijama direktno i indirektno utiču na destrukciju prirodnih staništa, što vodi do trajnog gubitka ekoloških i socio-ekonomskih funkcija ekosistema. U okviru ovog rada definisani su trendovi depozicija sumpora i azota kao i njihova veza sa osetljivošću zemljišta na proces acidifikacije i izdvojene su aktuelne i potencijalne zone rizika degradacije zemljišta. Procena stepena osetljivosti zemljišta šumskih i visoko-planinskih pašnjačkih ekosistema prema procesu acidifikacije, izvršena je metodom za proračun kritičnih opterećenja primenom VSD modela. Kritična opterećenja i prekoračenja zagađujućih materija u vazduhu predstavljaju jedan od glavnih indikatora osetljivosti šumskih i drugih terestričnih ekosistema i predstavljaju osnovu za održivo upravljanje ekosistemima kao osnovnih principa međunarodnog ekološkog prava i nacionalne politike..., Acidification is a process of decreasing soil pH value over time as a result of numerous biogeochemical processes. In humid and temperate climatic zones, acidification is a natural process caused by soil mineral phase, vegetation type and climate. Under natural conditions, this is a long term process of soil development which can not be seen as a process of land degradation.The influence of anthropogenic factors, excessive emissions of sulphur and nitrogen, inadequate ecosystem management, land use changes, as well as global climate change, acidification process can be significantly accelerated and intensified. In this context, soil acidification is a form of soil chemical degradation. Acidification induced by deposition of sulphur and nitrogen, due to the negative effects on natural ecosystems and biodiversity loss in the past 70 years, has become a global environmental problem. In forest and highland grasslands of Eastern Serbia soil acidification leads to a reduction/loss of soil quality, as resource and natural good. Rapid change of soil chemistry caused by acidic deposition directly and indirectly leads to destruction of natural habitats, and disturbance of environmental and socioeconomic functions of ecosystems. In this paper were defined trends of sulphur and nitrogen deposition, their relationship with the soil sensitivity to acidification as well as current and potential soil degradation risk areas. Assessment of soil sensitivity to acidification of forest and high mountain grasslands, were performed by using critical load concept and VSD model. Critical loads and exceedances of air pollutants are one of the main indicators of forest and terrestrial ecosystem sensitivity to acidification. The critical load concept can be considered as a tool for integrated monitoring of air pollution effects on ecosystems and fundamental principle of international environmental law and national clean air policy. Different ecosystem vulnerability zones to air pollutants were performed and based on soil sensitivity and concentrations of sulphur and nitrogen deposition for the period 1980-2009. The interdependence of soil properties and factors with the greatest impact on soil acidification were singled out by applying the method of simple and multiple regression, as well as factor analysis...",
publisher = "Univerzitet u Beogradu, Šumarski fakultet",
title = "Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije, Acidification process as a factor of soil degradation in eastern Serbia.",
url = "https://hdl.handle.net/21.15107/rcub_nardus_5038, t-5034"
}
Beloica, J. R.. (2015). Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije. 
Univerzitet u Beogradu, Šumarski fakultet..
https://hdl.handle.net/21.15107/rcub_nardus_5038
Beloica JR. Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije. 2015;.
https://hdl.handle.net/21.15107/rcub_nardus_5038 .
Beloica, Jelena R., "Proces acidifikacije kao faktor degradacije zemljišta na području istočne Srbije" (2015),
https://hdl.handle.net/21.15107/rcub_nardus_5038 .

Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste

Đukanović, Gordana; Obradović, Marija

(Univerzitet u Nišu, Niš, 2012)

TY  - JOUR
AU  - Đukanović, Gordana
AU  - Obradović, Marija
PY  - 2012
UR  - https://omorika.sfb.bg.ac.rs/handle/123456789/414
AB  - U radu je inverzijom preslikana prostorna kriva 4. reda prve vrste sa samopresečnom tačkom (sa dve ravni simetrije) i određen je njen harmonijski ekvivalent. Prikazani su harmonijski ekvivalenti za pet grupa površi koje su dobijene kroz prostornu krivu 4 reda 1 vrste. Preslikavanje je rađeno preko sistema kružnih preseka. Dato je klasično i tumačenje u relativističkooj geometriji. Takođe su urađeni i prostorni modeli - prostorni model pramena kvadrika i pramena ekvivalentnih kvadrika. Kroz ovaj pramen površi 4. reda, osim graničnih površi, prolazi i jedna površ 3. reda koja je ekvivalent troosnom elipsoidu. Centar inverzije nalazi se na konturi elipsoida. Parabolički cilindar se preslikava u svoj ekvivalent, tako što se konturna parabola cilindra, za drugu projekciju, preslika u odnosu na centar i sferu inverzije u konturnu krivu površi 4. reda. Izvodnice paraboličkog cilindra, koje su u projicirajućem položaju i prolaze kroz antipod, preslikavaju se u krugove (takođe u projicirajućem položaju) čiji su prečnici od centra inverzije do konturne linije. Prikazana je i primena površi 4. reda u arhitektonskoj praksi.
AB  - This paper shows the process of inverting the 4th ordered space curve of the first category with a self-intersecting point (with two planes of symmetry) and determining its harmonic equivalent. There are harmonic equivalents for five groups of surfaces obtained through the 4th order space curve of the 1st category. Mapping was done through a system of circular cross-sections. Both classical and relativistic geometry interpretations are presented. We also designed spatial models - a spatial model of the pencil of quadrics and a spatial model of the pencil of equivalent quadrics. Besides the boundary surfaces, one surface of the 3rd order, which is an equivalent to a triaxial ellipsoid, passes through this pencil of surface of the 4th order. The center of inversion is located on the contour of the ellipsoid. The parabolic cylinder is mapped into its equivalent, by mapping the contour parabola of the cylinder, in the frontal projection, in relation to the center and the sphere of inversion into a contour curve of the 4th order surface. The generating lines of the parabolic cylinder, which are in a projecting position and pass through the antipode, are mapped into circles (also in a projecting position) whose diameters are from the center of inversion to the contour line. The application of the 4th order surfaces in architectural practice is also presented.
PB  - Univerzitet u Nišu, Niš
T2  - Facta universitatis - series: Architecture and Civil Engineering
T1  - Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste
T1  - The pencil of the 4th and 3rd order surfaces obtained as a harmonic equivalent of the pencil of quadrics through a 4th order space curve of the 1st category
EP  - 207
IS  - 2
SP  - 193
VL  - 10
DO  - 10.2298/FUACE1202193D
UR  - conv_585
ER  - 
@article{
author = "Đukanović, Gordana and Obradović, Marija",
year = "2012",
abstract = "U radu je inverzijom preslikana prostorna kriva 4. reda prve vrste sa samopresečnom tačkom (sa dve ravni simetrije) i određen je njen harmonijski ekvivalent. Prikazani su harmonijski ekvivalenti za pet grupa površi koje su dobijene kroz prostornu krivu 4 reda 1 vrste. Preslikavanje je rađeno preko sistema kružnih preseka. Dato je klasično i tumačenje u relativističkooj geometriji. Takođe su urađeni i prostorni modeli - prostorni model pramena kvadrika i pramena ekvivalentnih kvadrika. Kroz ovaj pramen površi 4. reda, osim graničnih površi, prolazi i jedna površ 3. reda koja je ekvivalent troosnom elipsoidu. Centar inverzije nalazi se na konturi elipsoida. Parabolički cilindar se preslikava u svoj ekvivalent, tako što se konturna parabola cilindra, za drugu projekciju, preslika u odnosu na centar i sferu inverzije u konturnu krivu površi 4. reda. Izvodnice paraboličkog cilindra, koje su u projicirajućem položaju i prolaze kroz antipod, preslikavaju se u krugove (takođe u projicirajućem položaju) čiji su prečnici od centra inverzije do konturne linije. Prikazana je i primena površi 4. reda u arhitektonskoj praksi., This paper shows the process of inverting the 4th ordered space curve of the first category with a self-intersecting point (with two planes of symmetry) and determining its harmonic equivalent. There are harmonic equivalents for five groups of surfaces obtained through the 4th order space curve of the 1st category. Mapping was done through a system of circular cross-sections. Both classical and relativistic geometry interpretations are presented. We also designed spatial models - a spatial model of the pencil of quadrics and a spatial model of the pencil of equivalent quadrics. Besides the boundary surfaces, one surface of the 3rd order, which is an equivalent to a triaxial ellipsoid, passes through this pencil of surface of the 4th order. The center of inversion is located on the contour of the ellipsoid. The parabolic cylinder is mapped into its equivalent, by mapping the contour parabola of the cylinder, in the frontal projection, in relation to the center and the sphere of inversion into a contour curve of the 4th order surface. The generating lines of the parabolic cylinder, which are in a projecting position and pass through the antipode, are mapped into circles (also in a projecting position) whose diameters are from the center of inversion to the contour line. The application of the 4th order surfaces in architectural practice is also presented.",
publisher = "Univerzitet u Nišu, Niš",
journal = "Facta universitatis - series: Architecture and Civil Engineering",
title = "Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste, The pencil of the 4th and 3rd order surfaces obtained as a harmonic equivalent of the pencil of quadrics through a 4th order space curve of the 1st category",
pages = "207-193",
number = "2",
volume = "10",
doi = "10.2298/FUACE1202193D",
url = "conv_585"
}
Đukanović, G.,& Obradović, M.. (2012). Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste. in Facta universitatis - series: Architecture and Civil Engineering
Univerzitet u Nišu, Niš., 10(2), 193-207.
https://doi.org/10.2298/FUACE1202193D
conv_585
Đukanović G, Obradović M. Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste. in Facta universitatis - series: Architecture and Civil Engineering. 2012;10(2):193-207.
doi:10.2298/FUACE1202193D
conv_585 .
Đukanović, Gordana, Obradović, Marija, "Pramen površi 4. i 3. reda dobijen kao harmonijski ekvivalent pramena kvadrika kroz prostornu krivu 4. reda 1. vrste" in Facta universitatis - series: Architecture and Civil Engineering, 10, no. 2 (2012):193-207,
https://doi.org/10.2298/FUACE1202193D .,
conv_585 .
1