Životić, Dragana

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orcid::0000-0001-6218-7091
  • Životić, Dragana (8)
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Author's Bibliography

Forecast resources of zeolithic tuffs of Serbia

Kašić, Vladan; Životić, Dragana; Simić, Vladimir; Radosavljević-Mihajlović, Ana; Stojanović, Jovica; Mihajlović, Slavica; Vukadinović, Melina

(Bor : University of Belgrade, Technical Faculty in Bor, 2021)

TY  - JOUR
AU  - Kašić, Vladan
AU  - Životić, Dragana
AU  - Simić, Vladimir
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
AU  - Mihajlović, Slavica
AU  - Vukadinović, Melina
PY  - 2021
UR  - https://ritnms.itnms.ac.rs/handle/123456789/686
AB  - Our zeolite tuff deposits (Zlatokop, Igroš, Jablanica 1, Beočin, Toponica and Slanci), which were the subject of detailed research, spatially and genetically are connected to volcanic volcaniclastic rocks of marine environment of Senonian and Neogene age, as well as lake sediments of Neogene age. Zeolitic tuff deposits were formed as a product of devitrification of volcanic glass. More will be said here about the prognostic resources of our zeolite tuffs, both in relation to the registered phenomena so far, and to possible areas in terms of finding new quantities of this economically very interesting mineral raw material.
PB  - Bor : University of Belgrade, Technical Faculty in Bor
T2  - 52nd International October Conference on Mining and Metallurgy IOC 2021
T1  - Forecast resources of zeolithic tuffs of Serbia
EP  - 180
SP  - 177
ER  - 
@article{
author = "Kašić, Vladan and Životić, Dragana and Simić, Vladimir and Radosavljević-Mihajlović, Ana and Stojanović, Jovica and Mihajlović, Slavica and Vukadinović, Melina",
year = "2021",
abstract = "Our zeolite tuff deposits (Zlatokop, Igroš, Jablanica 1, Beočin, Toponica and Slanci), which were the subject of detailed research, spatially and genetically are connected to volcanic volcaniclastic rocks of marine environment of Senonian and Neogene age, as well as lake sediments of Neogene age. Zeolitic tuff deposits were formed as a product of devitrification of volcanic glass. More will be said here about the prognostic resources of our zeolite tuffs, both in relation to the registered phenomena so far, and to possible areas in terms of finding new quantities of this economically very interesting mineral raw material.",
publisher = "Bor : University of Belgrade, Technical Faculty in Bor",
journal = "52nd International October Conference on Mining and Metallurgy IOC 2021",
title = "Forecast resources of zeolithic tuffs of Serbia",
pages = "180-177"
}
Kašić, V., Životić, D., Simić, V., Radosavljević-Mihajlović, A., Stojanović, J., Mihajlović, S.,& Vukadinović, M.. (2021). Forecast resources of zeolithic tuffs of Serbia. in 52nd International October Conference on Mining and Metallurgy IOC 2021
Bor : University of Belgrade, Technical Faculty in Bor., 177-180.
Kašić V, Životić D, Simić V, Radosavljević-Mihajlović A, Stojanović J, Mihajlović S, Vukadinović M. Forecast resources of zeolithic tuffs of Serbia. in 52nd International October Conference on Mining and Metallurgy IOC 2021. 2021;:177-180..
Kašić, Vladan, Životić, Dragana, Simić, Vladimir, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, Mihajlović, Slavica, Vukadinović, Melina, "Forecast resources of zeolithic tuffs of Serbia" in 52nd International October Conference on Mining and Metallurgy IOC 2021 (2021):177-180.

Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects

Kašić, Vladan; Mihajlović, Slavica; Životić, Dragana; Simić, Vladimir; Stojanović, Jovica; Sekulić, Živko; Kragović, Milan

(Savez hemijskih inženjera, Beograd, 2018)

TY  - JOUR
AU  - Kašić, Vladan
AU  - Mihajlović, Slavica
AU  - Životić, Dragana
AU  - Simić, Vladimir
AU  - Stojanović, Jovica
AU  - Sekulić, Živko
AU  - Kragović, Milan
PY  - 2018
UR  - https://ritnms.itnms.ac.rs/handle/123456789/464
AB  - This study presents investigations of zeolitic tuff samples from the “Igroš--Vidojevići” deposit. The aim of the research was to determine the quality of samples taken from all deposit parts. Thus, samples were taken from the footwall (“Zeolit 1”), and four samples from the central deposit part (“Zeolit 2”, “Zeolit 3”, “Zeolit 4” and “Zeolit 5”). Characterization of the samples included chemical analysis, determination of the adsorption coefficient for methylene blue dye and cation-exchange capacity (CEC), X-ray powder diffraction analysis (XRPD), differential thermal and thermogravimetric analysis (DTA and TGA), and Fourier transform Infrared spectroscopic analysis (FTIR). Results have shown that the footwall consists mostly of clays, whereas zeolite minerals dominate in the rest of the deposit. XRD analysis of the “Zeolit 1” sample confirmed presence of smectite and kaolinite clays, while zeolite of analcime type and quartz are present as smaller fractions. Chemical composition analysis and determination of heavy metal contents showed a significant amount (7.58%) of Fe2 O3 in this sample. Therefore, further research can be pursued to find a method for removal of magnetic impurities in this deposit portion in order to utilize the clay fraction. On the other hand, according to XRD, FTIR, DTA/TGA and SEM/EDS analyses, samples which belong to the central deposit part (“Zeolit 2–5”) consist of clinoptilolite zeolite type, while clays are present in less than 10%. Thus, clays (smectites and kaolinite) accompanied with analcime and quartz are the most abundant footwall minerals while central deposit parts contain predominantly clinoptilolite accompanied with small amounts of clays. Mineragenetically, zeolites are most abundant in the “Zeolit 2” and “Zeolit 3” samples. The smallest value of CEC was determined for the “Zeolit 1” sample (46.98 mmol/100g). According to CEC values determined for “Zeolit 2” and “Zeolit 3” (141.99 and 121.01 mmol/100 g, respect-ively) these samples are of the best quality, and could be utilized as adsorbents of inorganic pollutants from contaminated waters. Moreover, they could be potentially used for removal of mycotoxins from cattle feed. “Zeolit 4” and “Zeolit 5” samples have shown slightly lower CEC values (89.48 and 83.75 mmol/100 g, respectively), which implies lower quality, and, therefore, could be used for soil quality improvement. Finally, determination of the external CEC has revealed a significant difference between “Zeolit 1” and “Zeolit 5” samples (17.9 and 5.31 mmol/100 g, respectively).
PB  - Savez hemijskih inženjera, Beograd
T2  - Hemijska industrija
T1  - Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects
EP  - 37
IS  - 1
SP  - 29
VL  - 72
DO  - 10.2298/HEMIND170428015K
UR  - conv_1030
ER  - 
@article{
author = "Kašić, Vladan and Mihajlović, Slavica and Životić, Dragana and Simić, Vladimir and Stojanović, Jovica and Sekulić, Živko and Kragović, Milan",
year = "2018",
abstract = "This study presents investigations of zeolitic tuff samples from the “Igroš--Vidojevići” deposit. The aim of the research was to determine the quality of samples taken from all deposit parts. Thus, samples were taken from the footwall (“Zeolit 1”), and four samples from the central deposit part (“Zeolit 2”, “Zeolit 3”, “Zeolit 4” and “Zeolit 5”). Characterization of the samples included chemical analysis, determination of the adsorption coefficient for methylene blue dye and cation-exchange capacity (CEC), X-ray powder diffraction analysis (XRPD), differential thermal and thermogravimetric analysis (DTA and TGA), and Fourier transform Infrared spectroscopic analysis (FTIR). Results have shown that the footwall consists mostly of clays, whereas zeolite minerals dominate in the rest of the deposit. XRD analysis of the “Zeolit 1” sample confirmed presence of smectite and kaolinite clays, while zeolite of analcime type and quartz are present as smaller fractions. Chemical composition analysis and determination of heavy metal contents showed a significant amount (7.58%) of Fe2 O3 in this sample. Therefore, further research can be pursued to find a method for removal of magnetic impurities in this deposit portion in order to utilize the clay fraction. On the other hand, according to XRD, FTIR, DTA/TGA and SEM/EDS analyses, samples which belong to the central deposit part (“Zeolit 2–5”) consist of clinoptilolite zeolite type, while clays are present in less than 10%. Thus, clays (smectites and kaolinite) accompanied with analcime and quartz are the most abundant footwall minerals while central deposit parts contain predominantly clinoptilolite accompanied with small amounts of clays. Mineragenetically, zeolites are most abundant in the “Zeolit 2” and “Zeolit 3” samples. The smallest value of CEC was determined for the “Zeolit 1” sample (46.98 mmol/100g). According to CEC values determined for “Zeolit 2” and “Zeolit 3” (141.99 and 121.01 mmol/100 g, respect-ively) these samples are of the best quality, and could be utilized as adsorbents of inorganic pollutants from contaminated waters. Moreover, they could be potentially used for removal of mycotoxins from cattle feed. “Zeolit 4” and “Zeolit 5” samples have shown slightly lower CEC values (89.48 and 83.75 mmol/100 g, respectively), which implies lower quality, and, therefore, could be used for soil quality improvement. Finally, determination of the external CEC has revealed a significant difference between “Zeolit 1” and “Zeolit 5” samples (17.9 and 5.31 mmol/100 g, respectively).",
publisher = "Savez hemijskih inženjera, Beograd",
journal = "Hemijska industrija",
title = "Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects",
pages = "37-29",
number = "1",
volume = "72",
doi = "10.2298/HEMIND170428015K",
url = "conv_1030"
}
Kašić, V., Mihajlović, S., Životić, D., Simić, V., Stojanović, J., Sekulić, Ž.,& Kragović, M.. (2018). Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects. in Hemijska industrija
Savez hemijskih inženjera, Beograd., 72(1), 29-37.
https://doi.org/10.2298/HEMIND170428015K
conv_1030
Kašić V, Mihajlović S, Životić D, Simić V, Stojanović J, Sekulić Ž, Kragović M. Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects. in Hemijska industrija. 2018;72(1):29-37.
doi:10.2298/HEMIND170428015K
conv_1030 .
Kašić, Vladan, Mihajlović, Slavica, Životić, Dragana, Simić, Vladimir, Stojanović, Jovica, Sekulić, Živko, Kragović, Milan, "Characterization of the zeolitic tuff from the “igroš-vidojevići” deposit regarding geological and technological aspects" in Hemijska industrija, 72, no. 1 (2018):29-37,
https://doi.org/10.2298/HEMIND170428015K .,
conv_1030 .
4
5

Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia

Kašić, Vladan; Simić, Vladimir; Životić, Dragana; Radosavljević-Mihajlović, Ana; Stojanović, Jovica

(Beograd : Srpsko hemijsko društvo, 2017)

TY  - JOUR
AU  - Kašić, Vladan
AU  - Simić, Vladimir
AU  - Životić, Dragana
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1019
AB  - Veliki broj pojava i ležišta prirodnih zeolita piroklastičnog porekla široko rasprostranjenih u
miocenskim sedimentima Srbije, su predmet detaljnih istraživanja. Najznačajnija srpska
ležišta zeolitskih tufova su: Zlatokop (Vranjski basen), Igroš (Kopaonik), Beočin (Fruška
Gora), Toponica i Slanci (Dunavski ključ kod Beograda). Ležišta ovih zeolitskih tufova, prostorno
i genetski vezana su za vulkanske i vulkanoklastične stene marinskih sredina senonske
i neogenske starosti i jezerskih sedimenata neogene starosti. U procesima devitrifikacije
i dijageneze vulkanskog stakla kod zeolitskih tufova došlo je do obrazovanje hipokristalasto
porfirske odnosno vitroklastične strukture. Sami zeolitski tufovi u najvećem delu
sastavljeni su od hojlandita, koji je prisutan u obliku malih igličastih do pločastih kristala
dimenzija od 0,1 do 100 μm (u asocijaciji sa drugim silikatnim i alumosilikatnim fazama
približno sličnih specifičnih gustina). U zavisnosti od vrste i sadržaja izmenljivog katjona,
kao i termičke stabilnosti ispitivanog zeolitskog tufa razlikujemo Ca-klinoptilolite i Ca-hojlandite.
Kapaciteti katjonske izmene zeolitskih tufova imaju vrednosti od 96 do 166
meq/100 g, a spoljašnji kapaciteti se kreću od 8,0 do 10,5 meq/100 g. Ovaj rad se bavi
detaljnom karakterizacijom prirodnih zeolita najznačajnijih srpskih ležišta, gde je kristalohemijski
sastav zeolita u direktnoj vezi sa genetskim i paragenetskim karakteristikama
njihovih ležišta.
AB  - The results of perennial research of several Serbian zeolitic tuffs enriched with
HEU-type minerals are presented in this paper. There are several recognized zeo-
litic tuff deposits containing HEU-type minerals: Zlatokop, Igroš, Beočin, Toponica
and Slanci, but their comparative mineralogical and crystallochemical features
have not been studied in detail so far. These zeolitic tuff deposits are spatially and
genetically connected to volcanic and pyroclastic rocks of marine and lake envi-
ronments of Senonian and Eocene, and Neogene age, respectively. As a result of
devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypo-
crystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are
mainly composed of heulandite occuring in a form of needle- to plate-like crystals
of 0.1 do 100 μm in length, associated with other silicates. Depending on the type
and content of exchangeable cations as well as the thermal stability of these raw
materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of
cation exchange capacity and surface area capacity range from 96 to 166
meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can
be distinguished either by a Si/Al ratio or arrangement of extra framework cations
within the crystal structure of these minerals.
PB  - Beograd : Srpsko hemijsko društvo
T2  - Hemijska Industrija
T1  - Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia
EP  - 60
IS  - 1
SP  - 49
VL  - 71
DO  - 10.2298/HEMIND151019017K
ER  - 
@article{
author = "Kašić, Vladan and Simić, Vladimir and Životić, Dragana and Radosavljević-Mihajlović, Ana and Stojanović, Jovica",
year = "2017",
abstract = "Veliki broj pojava i ležišta prirodnih zeolita piroklastičnog porekla široko rasprostranjenih u
miocenskim sedimentima Srbije, su predmet detaljnih istraživanja. Najznačajnija srpska
ležišta zeolitskih tufova su: Zlatokop (Vranjski basen), Igroš (Kopaonik), Beočin (Fruška
Gora), Toponica i Slanci (Dunavski ključ kod Beograda). Ležišta ovih zeolitskih tufova, prostorno
i genetski vezana su za vulkanske i vulkanoklastične stene marinskih sredina senonske
i neogenske starosti i jezerskih sedimenata neogene starosti. U procesima devitrifikacije
i dijageneze vulkanskog stakla kod zeolitskih tufova došlo je do obrazovanje hipokristalasto
porfirske odnosno vitroklastične strukture. Sami zeolitski tufovi u najvećem delu
sastavljeni su od hojlandita, koji je prisutan u obliku malih igličastih do pločastih kristala
dimenzija od 0,1 do 100 μm (u asocijaciji sa drugim silikatnim i alumosilikatnim fazama
približno sličnih specifičnih gustina). U zavisnosti od vrste i sadržaja izmenljivog katjona,
kao i termičke stabilnosti ispitivanog zeolitskog tufa razlikujemo Ca-klinoptilolite i Ca-hojlandite.
Kapaciteti katjonske izmene zeolitskih tufova imaju vrednosti od 96 do 166
meq/100 g, a spoljašnji kapaciteti se kreću od 8,0 do 10,5 meq/100 g. Ovaj rad se bavi
detaljnom karakterizacijom prirodnih zeolita najznačajnijih srpskih ležišta, gde je kristalohemijski
sastav zeolita u direktnoj vezi sa genetskim i paragenetskim karakteristikama
njihovih ležišta., The results of perennial research of several Serbian zeolitic tuffs enriched with
HEU-type minerals are presented in this paper. There are several recognized zeo-
litic tuff deposits containing HEU-type minerals: Zlatokop, Igroš, Beočin, Toponica
and Slanci, but their comparative mineralogical and crystallochemical features
have not been studied in detail so far. These zeolitic tuff deposits are spatially and
genetically connected to volcanic and pyroclastic rocks of marine and lake envi-
ronments of Senonian and Eocene, and Neogene age, respectively. As a result of
devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypo-
crystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are
mainly composed of heulandite occuring in a form of needle- to plate-like crystals
of 0.1 do 100 μm in length, associated with other silicates. Depending on the type
and content of exchangeable cations as well as the thermal stability of these raw
materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of
cation exchange capacity and surface area capacity range from 96 to 166
meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can
be distinguished either by a Si/Al ratio or arrangement of extra framework cations
within the crystal structure of these minerals.",
publisher = "Beograd : Srpsko hemijsko društvo",
journal = "Hemijska Industrija",
title = "Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia",
pages = "60-49",
number = "1",
volume = "71",
doi = "10.2298/HEMIND151019017K"
}
Kašić, V., Simić, V., Životić, D., Radosavljević-Mihajlović, A.,& Stojanović, J.. (2017). Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia. in Hemijska Industrija
Beograd : Srpsko hemijsko društvo., 71(1), 49-60.
https://doi.org/10.2298/HEMIND151019017K
Kašić V, Simić V, Životić D, Radosavljević-Mihajlović A, Stojanović J. Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia. in Hemijska Industrija. 2017;71(1):49-60.
doi:10.2298/HEMIND151019017K .
Kašić, Vladan, Simić, Vladimir, Životić, Dragana, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, "Mineralogy and crystallochemical characteristics of HEU-type minerals from zeolitic tuff deposits of Serbia" in Hemijska Industrija, 71, no. 1 (2017):49-60,
https://doi.org/10.2298/HEMIND151019017K . .

Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia

Kašić, Vladan; Simić, Vladimir; Životić, Dragana; Radosavljević-Mihajlović, Ana; Stojanović, Jovica

(Savez hemijskih inženjera, Beograd, 2017)

TY  - JOUR
AU  - Kašić, Vladan
AU  - Simić, Vladimir
AU  - Životić, Dragana
AU  - Radosavljević-Mihajlović, Ana
AU  - Stojanović, Jovica
PY  - 2017
UR  - https://ritnms.itnms.ac.rs/handle/123456789/451
AB  - The results of perennial research of several Serbian zeolitic tuffs enriched with HEU-type minerals are presented in this paper. There are several recognized zeolitic tuff deposits containing HEU-type minerals: Zlatokop, Igros, Beocin, Toponica and Slanci, but their comparative mineralogical and crystallochemical features have not been studied in detail so far. These zeolitic tuff deposits are spatially and genetically connected to volcanic and pyroclastic rocks of marine and lake environments of Senonian and Eocene, and Neogene age, respectively. As a result of devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypocrystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are mainly composed of heulandite occuring in a form of needle-to plate-like crystals of 0.1 do 100 mu m in length, associated with other silicates. Depending on the type and content of exchangeable cations as well as the thermal stability of these raw materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of cation exchange capacity and surface area capacity range from 96 to 166 meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can be distinguished either by a Si/Al ratio or arrangement of extra framework cations within the crystal structure of these minerals.
PB  - Savez hemijskih inženjera, Beograd
T2  - Hemijska industrija
T1  - Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia
EP  - 60
IS  - 1
SP  - 49
VL  - 71
DO  - 10.2298/HEMIND151019017K
UR  - conv_790
ER  - 
@article{
author = "Kašić, Vladan and Simić, Vladimir and Životić, Dragana and Radosavljević-Mihajlović, Ana and Stojanović, Jovica",
year = "2017",
abstract = "The results of perennial research of several Serbian zeolitic tuffs enriched with HEU-type minerals are presented in this paper. There are several recognized zeolitic tuff deposits containing HEU-type minerals: Zlatokop, Igros, Beocin, Toponica and Slanci, but their comparative mineralogical and crystallochemical features have not been studied in detail so far. These zeolitic tuff deposits are spatially and genetically connected to volcanic and pyroclastic rocks of marine and lake environments of Senonian and Eocene, and Neogene age, respectively. As a result of devitrification and diagenesis process of volcanic glass within zeolitic tuffs hypocrystalline porphiry and vitroclastic textures occur. The studied zeolitic tuffs are mainly composed of heulandite occuring in a form of needle-to plate-like crystals of 0.1 do 100 mu m in length, associated with other silicates. Depending on the type and content of exchangeable cations as well as the thermal stability of these raw materials, clinoptilolite-Ca and heulandite-Ca can be distinguished. The values of cation exchange capacity and surface area capacity range from 96 to 166 meq/100 g, and from 8.0 to 10.5 meq/100 g, respectively. HEU-type minerals can be distinguished either by a Si/Al ratio or arrangement of extra framework cations within the crystal structure of these minerals.",
publisher = "Savez hemijskih inženjera, Beograd",
journal = "Hemijska industrija",
title = "Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia",
pages = "60-49",
number = "1",
volume = "71",
doi = "10.2298/HEMIND151019017K",
url = "conv_790"
}
Kašić, V., Simić, V., Životić, D., Radosavljević-Mihajlović, A.,& Stojanović, J.. (2017). Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia. in Hemijska industrija
Savez hemijskih inženjera, Beograd., 71(1), 49-60.
https://doi.org/10.2298/HEMIND151019017K
conv_790
Kašić V, Simić V, Životić D, Radosavljević-Mihajlović A, Stojanović J. Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia. in Hemijska industrija. 2017;71(1):49-60.
doi:10.2298/HEMIND151019017K
conv_790 .
Kašić, Vladan, Simić, Vladimir, Životić, Dragana, Radosavljević-Mihajlović, Ana, Stojanović, Jovica, "Mineralogy and crystallochemical characteristics of heu-type minerals from zeolitic tuff deposits of Serbia" in Hemijska industrija, 71, no. 1 (2017):49-60,
https://doi.org/10.2298/HEMIND151019017K .,
conv_790 .
1
2

The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments

Vuković, Nikola; Životić, Dragana; Mendonca Filho, Joao Graciano; Kravić-Stevović, Tamara; Hamor-Vido, Maria; Mendonca, Joalice de Oliveira; Stojanović, Ksenija

(Elsevier, Amsterdam, 2016)

TY  - JOUR
AU  - Vuković, Nikola
AU  - Životić, Dragana
AU  - Mendonca Filho, Joao Graciano
AU  - Kravić-Stevović, Tamara
AU  - Hamor-Vido, Maria
AU  - Mendonca, Joalice de Oliveira
AU  - Stojanović, Ksenija
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/414
AB  - The artificial maturation changes of the humic coal organic matter (OM) from late diagenesis to the semianthracite stage of coalification were investigated using the closed-system pyrolysis. Two extracted coal samples, a subbituminous coal 26C (with a random vitrinite reflectance Rr = 0.42%) and a high volatile bituminous coal 30C (Rr = 0.56%), were pyrolysed during 4 hat two different temperatures, 250 degrees C and 400 degrees C. The applied petrographic and organic geochemical analyses showed that the humic coal OM is sensitive to the artificial thermal stress. A good correlation between the changes in petrographic characteristics and the derived liquid products was observed. The contents of all vitrinite macerals, as well as total vitrinite, increased during the thermal maturation. The abundance of liptinite macerals decreased during the maturation and they practically disappeared after 4 h of the pyrolysis at 400 degrees C. The total inertinite contents increased after the pyrolysis at 250 degrees C, yet to be decreased after the pyrolysis at 400 degrees C. The content of organic carbon increased from coals to the solid residues at 400 degrees C, whereas the contents of total hydrogen and sulphur decreased. The yields of gases, liquid products and solid residues at respective temperatures were very similar for both coals, regardless of the rank. As expected, the pyrolysis at 400 degrees C gave higher gas and liquid yields than at 250 degrees C. Regarding the liquid pyrolysates, more pronounced changes were observed in the distribution of aromatic compounds than in saturated biomarkers. The distributions of the aromatics indicate that apart from cracking and isomerisation (the formation of thermodynamically more stable isomers), the reactions of dehydrocyclization, condensation (the formation of more stable conjugated systems) and aromatization, as well as reactions involving H2S, elemental sulphur and reactive phenyl radicals released during the pyrolysis, also play an important role. It was shown that bentonitic clay plays a more important role in the subsequent aromatization of the OM than the initial maturity of the coal OM. n-Alkane parameters were useful at lower maturities (up to similar to 0.75% Rr), whereas sterane, naphthalene and phenanthrene maturity ratios are applicable at higher maturities (>0.75% Rr). Hopane parameters showed variable sensitivities over the investigated maturity range (0.5-1.8% Rr). The most sensitive maturity parameters in the wide range of the humic OM maturity (0.5-1.8% Rr) are vitrinite reflectance, phenylnaphthalene ratio, methylchrysene index 2 and a parameter proposed in this study, based on the distribution of methylfluorenes (MF): (2- + 3-MF) / (1- + 4-MF). Generally, maturity parameters based solely on the isomerisation reactions of alkylaromatics, which do not include alkylation/dealkylation processes, are more appropriate for the humic OM, particularly at higher maturities.
PB  - Elsevier, Amsterdam
T2  - International Journal of Coal Geology
T1  - The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments
EP  - 239
SP  - 213
VL  - 154-155
DO  - 10.1016/j.coal.2016.01.007
UR  - conv_752
ER  - 
@article{
author = "Vuković, Nikola and Životić, Dragana and Mendonca Filho, Joao Graciano and Kravić-Stevović, Tamara and Hamor-Vido, Maria and Mendonca, Joalice de Oliveira and Stojanović, Ksenija",
year = "2016",
abstract = "The artificial maturation changes of the humic coal organic matter (OM) from late diagenesis to the semianthracite stage of coalification were investigated using the closed-system pyrolysis. Two extracted coal samples, a subbituminous coal 26C (with a random vitrinite reflectance Rr = 0.42%) and a high volatile bituminous coal 30C (Rr = 0.56%), were pyrolysed during 4 hat two different temperatures, 250 degrees C and 400 degrees C. The applied petrographic and organic geochemical analyses showed that the humic coal OM is sensitive to the artificial thermal stress. A good correlation between the changes in petrographic characteristics and the derived liquid products was observed. The contents of all vitrinite macerals, as well as total vitrinite, increased during the thermal maturation. The abundance of liptinite macerals decreased during the maturation and they practically disappeared after 4 h of the pyrolysis at 400 degrees C. The total inertinite contents increased after the pyrolysis at 250 degrees C, yet to be decreased after the pyrolysis at 400 degrees C. The content of organic carbon increased from coals to the solid residues at 400 degrees C, whereas the contents of total hydrogen and sulphur decreased. The yields of gases, liquid products and solid residues at respective temperatures were very similar for both coals, regardless of the rank. As expected, the pyrolysis at 400 degrees C gave higher gas and liquid yields than at 250 degrees C. Regarding the liquid pyrolysates, more pronounced changes were observed in the distribution of aromatic compounds than in saturated biomarkers. The distributions of the aromatics indicate that apart from cracking and isomerisation (the formation of thermodynamically more stable isomers), the reactions of dehydrocyclization, condensation (the formation of more stable conjugated systems) and aromatization, as well as reactions involving H2S, elemental sulphur and reactive phenyl radicals released during the pyrolysis, also play an important role. It was shown that bentonitic clay plays a more important role in the subsequent aromatization of the OM than the initial maturity of the coal OM. n-Alkane parameters were useful at lower maturities (up to similar to 0.75% Rr), whereas sterane, naphthalene and phenanthrene maturity ratios are applicable at higher maturities (>0.75% Rr). Hopane parameters showed variable sensitivities over the investigated maturity range (0.5-1.8% Rr). The most sensitive maturity parameters in the wide range of the humic OM maturity (0.5-1.8% Rr) are vitrinite reflectance, phenylnaphthalene ratio, methylchrysene index 2 and a parameter proposed in this study, based on the distribution of methylfluorenes (MF): (2- + 3-MF) / (1- + 4-MF). Generally, maturity parameters based solely on the isomerisation reactions of alkylaromatics, which do not include alkylation/dealkylation processes, are more appropriate for the humic OM, particularly at higher maturities.",
publisher = "Elsevier, Amsterdam",
journal = "International Journal of Coal Geology",
title = "The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments",
pages = "239-213",
volume = "154-155",
doi = "10.1016/j.coal.2016.01.007",
url = "conv_752"
}
Vuković, N., Životić, D., Mendonca Filho, J. G., Kravić-Stevović, T., Hamor-Vido, M., Mendonca, J. d. O.,& Stojanović, K.. (2016). The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments. in International Journal of Coal Geology
Elsevier, Amsterdam., 154-155, 213-239.
https://doi.org/10.1016/j.coal.2016.01.007
conv_752
Vuković N, Životić D, Mendonca Filho JG, Kravić-Stevović T, Hamor-Vido M, Mendonca JDO, Stojanović K. The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments. in International Journal of Coal Geology. 2016;154-155:213-239.
doi:10.1016/j.coal.2016.01.007
conv_752 .
Vuković, Nikola, Životić, Dragana, Mendonca Filho, Joao Graciano, Kravić-Stevović, Tamara, Hamor-Vido, Maria, Mendonca, Joalice de Oliveira, Stojanović, Ksenija, "The assessment of maturation changes of humic coal organic matter - Insights from closed-system pyrolysis experiments" in International Journal of Coal Geology, 154-155 (2016):213-239,
https://doi.org/10.1016/j.coal.2016.01.007 .,
conv_752 .
29
17
33

Identification of a Novel Series of Benzohopanes and Their Geochemical Significance

Nytoft, H.P.; Vuković, Nikola; Kildahl-Andersen, Geir; Rise, Frode; Životić, Dragana; Stojanović, Ksenija

(Amer Chemical Soc, Washington, 2016)

TY  - JOUR
AU  - Nytoft, H.P.
AU  - Vuković, Nikola
AU  - Kildahl-Andersen, Geir
AU  - Rise, Frode
AU  - Životić, Dragana
AU  - Stojanović, Ksenija
PY  - 2016
UR  - https://ritnms.itnms.ac.rs/handle/123456789/394
AB  - series of novel C-33-C-35 hexacyclic benzohopanes (C(33)b-C(35)b) were identified in 39 samples of coal extracts and 39 crude oils of different ages from all over the world. C(33)b and C(34)b homologues were isolated, and their structures were determined by nuclear magnetic resonance. The structure of C(35)b benzohopane was proposed based on the mass spectrum and its similarity with the mass spectra of structurally defined C(33)b and C(34)b homologues. The structures of the C(33)b-C(35)b hexacyclic benzohopanes are closely related to isohopanes; both groups are typical for terrestrial organic matter and can be useful in the correlation analysis. A possible pathway of formation of these novel benzohopanes and their hopanoid precursors with an additional branch in the aliphatic side chain is proposed. C(33)b-C(35)b hexacyclic benzohopanes are stable up to the maturity level corresponding to random vitrinite reflectance (Rr) of similar to 0.80%, which was demonstrated by analyzing the samples of different maturity and by the maturation simulation experiments: hydrous pyrolysis of two bituminous coals (Rr = 0.55 and 0.59%) and pyrolysis of an extracted bituminous coal (Rr = 0.56%) and its asphaltenes. This represents a confirmation that the formation of these novel benzohopanes is related to specific depositional conditions and microbial activity during diagenesis. Mature samples (Rr = 0.8%) and hydrous pyrolysate of the bituminous coals (Rr  LT  0.60%) obtained at 330 degrees C show a distinct distribution of benzohopanes in comparison to immature and moderately mature samples, which is characterized by a low abundance of the b series benzohopanes and the presence of regular and numerous other benzohopane isomers. The latter most likely represent isomers of regular and novel benzohopanes with different substitution patterns on the aromatic ring. This isomerization of alkyl groups attached to the aromatic ring, leading to the formation of thermodynamically more stable isomers, is a well-known maturation scenario so far reported in the series of alkylated naphthalenes, phenanthrenes, and dibenzothiophenes. Therefore, in the same way, a distribution of benzohopanes can indicate thermal maturity. In addition to the novel benzohopanes, three series (2 alpha, 2 beta, and 3 beta) of their methylated derivatives were identified in numerous samples. Finally, a novel C-35 heptacyclic benzohopane with an additional cyclopentane ring was also observed in the studied samples, and its structure was tentatively identified based on the mass spectrum. Opposite to the hexacyclic C(33)b-C(35)b benzohopanes, the formation of the C-35 heptacyclic benzohopane does not require a specific hopanoid precursor with two branches in the side chain. Therefore, this compound seems to have less geochemical significance than the new hexacyclic benzohopanes.
PB  - Amer Chemical Soc, Washington
T2  - Energy & Fuels
T1  - Identification of a Novel Series of Benzohopanes and Their Geochemical Significance
EP  - 5575
IS  - 7
SP  - 5563
VL  - 30
DO  - 10.1021/acs.energyfuels.6b00799
UR  - conv_765
ER  - 
@article{
author = "Nytoft, H.P. and Vuković, Nikola and Kildahl-Andersen, Geir and Rise, Frode and Životić, Dragana and Stojanović, Ksenija",
year = "2016",
abstract = "series of novel C-33-C-35 hexacyclic benzohopanes (C(33)b-C(35)b) were identified in 39 samples of coal extracts and 39 crude oils of different ages from all over the world. C(33)b and C(34)b homologues were isolated, and their structures were determined by nuclear magnetic resonance. The structure of C(35)b benzohopane was proposed based on the mass spectrum and its similarity with the mass spectra of structurally defined C(33)b and C(34)b homologues. The structures of the C(33)b-C(35)b hexacyclic benzohopanes are closely related to isohopanes; both groups are typical for terrestrial organic matter and can be useful in the correlation analysis. A possible pathway of formation of these novel benzohopanes and their hopanoid precursors with an additional branch in the aliphatic side chain is proposed. C(33)b-C(35)b hexacyclic benzohopanes are stable up to the maturity level corresponding to random vitrinite reflectance (Rr) of similar to 0.80%, which was demonstrated by analyzing the samples of different maturity and by the maturation simulation experiments: hydrous pyrolysis of two bituminous coals (Rr = 0.55 and 0.59%) and pyrolysis of an extracted bituminous coal (Rr = 0.56%) and its asphaltenes. This represents a confirmation that the formation of these novel benzohopanes is related to specific depositional conditions and microbial activity during diagenesis. Mature samples (Rr = 0.8%) and hydrous pyrolysate of the bituminous coals (Rr  LT  0.60%) obtained at 330 degrees C show a distinct distribution of benzohopanes in comparison to immature and moderately mature samples, which is characterized by a low abundance of the b series benzohopanes and the presence of regular and numerous other benzohopane isomers. The latter most likely represent isomers of regular and novel benzohopanes with different substitution patterns on the aromatic ring. This isomerization of alkyl groups attached to the aromatic ring, leading to the formation of thermodynamically more stable isomers, is a well-known maturation scenario so far reported in the series of alkylated naphthalenes, phenanthrenes, and dibenzothiophenes. Therefore, in the same way, a distribution of benzohopanes can indicate thermal maturity. In addition to the novel benzohopanes, three series (2 alpha, 2 beta, and 3 beta) of their methylated derivatives were identified in numerous samples. Finally, a novel C-35 heptacyclic benzohopane with an additional cyclopentane ring was also observed in the studied samples, and its structure was tentatively identified based on the mass spectrum. Opposite to the hexacyclic C(33)b-C(35)b benzohopanes, the formation of the C-35 heptacyclic benzohopane does not require a specific hopanoid precursor with two branches in the side chain. Therefore, this compound seems to have less geochemical significance than the new hexacyclic benzohopanes.",
publisher = "Amer Chemical Soc, Washington",
journal = "Energy & Fuels",
title = "Identification of a Novel Series of Benzohopanes and Their Geochemical Significance",
pages = "5575-5563",
number = "7",
volume = "30",
doi = "10.1021/acs.energyfuels.6b00799",
url = "conv_765"
}
Nytoft, H.P., Vuković, N., Kildahl-Andersen, G., Rise, F., Životić, D.,& Stojanović, K.. (2016). Identification of a Novel Series of Benzohopanes and Their Geochemical Significance. in Energy & Fuels
Amer Chemical Soc, Washington., 30(7), 5563-5575.
https://doi.org/10.1021/acs.energyfuels.6b00799
conv_765
Nytoft H, Vuković N, Kildahl-Andersen G, Rise F, Životić D, Stojanović K. Identification of a Novel Series of Benzohopanes and Their Geochemical Significance. in Energy & Fuels. 2016;30(7):5563-5575.
doi:10.1021/acs.energyfuels.6b00799
conv_765 .
Nytoft, H.P., Vuković, Nikola, Kildahl-Andersen, Geir, Rise, Frode, Životić, Dragana, Stojanović, Ksenija, "Identification of a Novel Series of Benzohopanes and Their Geochemical Significance" in Energy & Fuels, 30, no. 7 (2016):5563-5575,
https://doi.org/10.1021/acs.energyfuels.6b00799 .,
conv_765 .
1
15
11
16

GC-MS characterization of some novel benzohopanes in coals

Vuković, Nikola; Nytoft, Hans Peter; Životić, Dragana; Stojanović, Ksenija

(Stuttgart : Schweizerbart Science Publishers, 2015)

TY  - CONF
AU  - Vuković, Nikola
AU  - Nytoft, Hans Peter
AU  - Životić, Dragana
AU  - Stojanović, Ksenija
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/1161
PB  - Stuttgart : Schweizerbart Science Publishers
C3  - 67th Annual Meeting of the International Committee for Coal and Organic Petrology
T1  - GC-MS characterization of some novel benzohopanes in coals
EP  - 163
SP  - 162
ER  - 
@conference{
author = "Vuković, Nikola and Nytoft, Hans Peter and Životić, Dragana and Stojanović, Ksenija",
year = "2015",
publisher = "Stuttgart : Schweizerbart Science Publishers",
journal = "67th Annual Meeting of the International Committee for Coal and Organic Petrology",
title = "GC-MS characterization of some novel benzohopanes in coals",
pages = "163-162"
}
Vuković, N., Nytoft, H. P., Životić, D.,& Stojanović, K.. (2015). GC-MS characterization of some novel benzohopanes in coals. in 67th Annual Meeting of the International Committee for Coal and Organic Petrology
Stuttgart : Schweizerbart Science Publishers., 162-163.
Vuković N, Nytoft HP, Životić D, Stojanović K. GC-MS characterization of some novel benzohopanes in coals. in 67th Annual Meeting of the International Committee for Coal and Organic Petrology. 2015;:162-163..
Vuković, Nikola, Nytoft, Hans Peter, Životić, Dragana, Stojanović, Ksenija, "GC-MS characterization of some novel benzohopanes in coals" in 67th Annual Meeting of the International Committee for Coal and Organic Petrology (2015):162-163.

Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach

Đoković, Nataša; Mitrović, Danica; Bechtel, Achim; Vuković, Nikola; Medić, Ana; Vuković, Nikola; Životić, Dragana; Stojanović, Ksenija

(Beograd : Srpsko hemijsko društvo, 2015)

TY  - CONF
AU  - Đoković, Nataša
AU  - Mitrović, Danica
AU  - Bechtel, Achim
AU  - Vuković, Nikola
AU  - Medić, Ana
AU  - Vuković, Nikola
AU  - Životić, Dragana
AU  - Stojanović, Ksenija
PY  - 2015
UR  - https://ritnms.itnms.ac.rs/handle/123456789/915
AB  - In present study, both lipid classes, fatty acids and neutral lipids (e.g. alcohols) were
analysed in lignite samples in order to assess organic matter source and study biogeochemical and
diagenetic alteration processes.
The choice of polar compounds as useful biomarker indicators is based on several
considerations. As lipids, fatty acids are involved in energy storage, mobilization and in
membrane structure in all living organisms, while sterols have roles in membrane function and
hormonal regulation of metabolic processes primarily only in eucaryotes [1].
Pulverised lignites were extracted by an azeotrope mixture of dichloromethane and
methanol (88:12, v:v) using a Soxhlet’s apparatus. Extracts were dissolved in a mixture of nheptane:
dichloromethane (80:1, v:v) and asphaltenes were precipitated. The heptane-soluble
organic compounds (maltenes) were separated into saturated hydrocarbons, aromatic
hydrocarbons and NSO fraction (polar fraction, which contains nitrogen, sulphur, and oxygen
compounds) using column chromatography. Portions of NSO fractions were concentrated after
which the extracts were saponified with a mixture of 6% KOH in CH3OH and distilled water (3:1,
v:v) at 80°C (pH = 14). Fatty acids (FAs) and alcohols were analysed using a method modified
from Wakeham and Beier (1991) [1]. Alcohols and FAs were extracted 3 times with n-hexane at
pH 14 and pH 1, respectively using Na2SO4 for removal of the excess water. Prior to gas
chromatography-mass spectrometry analysis (GC-MS), the FAs and alcohol fractions were
derivatised with BSTFA (N,O-bis(trimethylsilyl)trifluoroacetamide, Fluka) for 1 h at 80°C to
form trimethylsilyl esters and ethers.
The obtained results are as follows: the fatty alcohols ranging from n-C12 to n-C28 alkanols
with a high abundance of long-chain fatty alcohols (n-C22 – C28) and only trace levels of shortchain
fatty alcohols (n-C12 – C18) indicating the main terrestrial input into the system. The
monounsaturated n-C18:1 fatty alcohol, which has been found in some species of diatoms,
Skeletonema costatum [2], was also present in samples. Steroidal alcohols, β-sitosterol (5-
cholesten-24β-ethyl-3β-ol), stigmastanol (24α-ethyl-5α-cholestan-3β-ol) and cholesterol, which
are the major sterols found in higher plants, are also found in small quantities. The presence of
kauran-13-ol is in accordance with the premise of terrestrial origin, given that abietane, pimarane,
kaurane and podocarpane skeletons are produced primarily by conifer vascular plants.
n-Alcanoic acids ranging from n-C6 – C30 with a notable predominance of even chainlenghts
are present in samples, having the maximum at hexadecanoic acid (C16:0). Saturated
compounds dominate in distribution but two unsaturated fatty acids were also found, 9-
octadecanoic (C18:1) and 9-hexadecanoic acid (C16:1). Apart from fatty acids, the polar fraction contains 4,8,12,16-tetramethylheptadecan-4-olide (a fragment of chlorophyll molecule with a side
phytol chain).
Typically high concentrations of long-chain (C22 –C30) n-alkanoic acids and n-alkanols (C12
– C28) with a sharp predominance of even homologues, certain hydroxyacids and dicarboxylic
acids, diterpenoid acids, long-chain saturated alkyl (wax) esters are characteristic components of
higher vascular plant cutin and suberin [3]. Biomarker analysis of aliphatic and aromatic fraction
of lignite coal is in concordance with the results obtained in the investigation of polar compounds,
confirming that in the case of Kostolac lignite, conifer terrestrial input was dominant source of
organic matter.
PB  - Beograd : Srpsko hemijsko društvo
C3  - 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)
T1  - Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach
EP  - 228
SP  - 227
ER  - 
@conference{
author = "Đoković, Nataša and Mitrović, Danica and Bechtel, Achim and Vuković, Nikola and Medić, Ana and Vuković, Nikola and Životić, Dragana and Stojanović, Ksenija",
year = "2015",
abstract = "In present study, both lipid classes, fatty acids and neutral lipids (e.g. alcohols) were
analysed in lignite samples in order to assess organic matter source and study biogeochemical and
diagenetic alteration processes.
The choice of polar compounds as useful biomarker indicators is based on several
considerations. As lipids, fatty acids are involved in energy storage, mobilization and in
membrane structure in all living organisms, while sterols have roles in membrane function and
hormonal regulation of metabolic processes primarily only in eucaryotes [1].
Pulverised lignites were extracted by an azeotrope mixture of dichloromethane and
methanol (88:12, v:v) using a Soxhlet’s apparatus. Extracts were dissolved in a mixture of nheptane:
dichloromethane (80:1, v:v) and asphaltenes were precipitated. The heptane-soluble
organic compounds (maltenes) were separated into saturated hydrocarbons, aromatic
hydrocarbons and NSO fraction (polar fraction, which contains nitrogen, sulphur, and oxygen
compounds) using column chromatography. Portions of NSO fractions were concentrated after
which the extracts were saponified with a mixture of 6% KOH in CH3OH and distilled water (3:1,
v:v) at 80°C (pH = 14). Fatty acids (FAs) and alcohols were analysed using a method modified
from Wakeham and Beier (1991) [1]. Alcohols and FAs were extracted 3 times with n-hexane at
pH 14 and pH 1, respectively using Na2SO4 for removal of the excess water. Prior to gas
chromatography-mass spectrometry analysis (GC-MS), the FAs and alcohol fractions were
derivatised with BSTFA (N,O-bis(trimethylsilyl)trifluoroacetamide, Fluka) for 1 h at 80°C to
form trimethylsilyl esters and ethers.
The obtained results are as follows: the fatty alcohols ranging from n-C12 to n-C28 alkanols
with a high abundance of long-chain fatty alcohols (n-C22 – C28) and only trace levels of shortchain
fatty alcohols (n-C12 – C18) indicating the main terrestrial input into the system. The
monounsaturated n-C18:1 fatty alcohol, which has been found in some species of diatoms,
Skeletonema costatum [2], was also present in samples. Steroidal alcohols, β-sitosterol (5-
cholesten-24β-ethyl-3β-ol), stigmastanol (24α-ethyl-5α-cholestan-3β-ol) and cholesterol, which
are the major sterols found in higher plants, are also found in small quantities. The presence of
kauran-13-ol is in accordance with the premise of terrestrial origin, given that abietane, pimarane,
kaurane and podocarpane skeletons are produced primarily by conifer vascular plants.
n-Alcanoic acids ranging from n-C6 – C30 with a notable predominance of even chainlenghts
are present in samples, having the maximum at hexadecanoic acid (C16:0). Saturated
compounds dominate in distribution but two unsaturated fatty acids were also found, 9-
octadecanoic (C18:1) and 9-hexadecanoic acid (C16:1). Apart from fatty acids, the polar fraction contains 4,8,12,16-tetramethylheptadecan-4-olide (a fragment of chlorophyll molecule with a side
phytol chain).
Typically high concentrations of long-chain (C22 –C30) n-alkanoic acids and n-alkanols (C12
– C28) with a sharp predominance of even homologues, certain hydroxyacids and dicarboxylic
acids, diterpenoid acids, long-chain saturated alkyl (wax) esters are characteristic components of
higher vascular plant cutin and suberin [3]. Biomarker analysis of aliphatic and aromatic fraction
of lignite coal is in concordance with the results obtained in the investigation of polar compounds,
confirming that in the case of Kostolac lignite, conifer terrestrial input was dominant source of
organic matter.",
publisher = "Beograd : Srpsko hemijsko društvo",
journal = "7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)",
title = "Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach",
pages = "228-227"
}
Đoković, N., Mitrović, D., Bechtel, A., Vuković, N., Medić, A., Vuković, N., Životić, D.,& Stojanović, K.. (2015). Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach. in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015)
Beograd : Srpsko hemijsko društvo., 227-228.
Đoković N, Mitrović D, Bechtel A, Vuković N, Medić A, Vuković N, Životić D, Stojanović K. Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach. in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015). 2015;:227-228..
Đoković, Nataša, Mitrović, Danica, Bechtel, Achim, Vuković, Nikola, Medić, Ana, Vuković, Nikola, Životić, Dragana, Stojanović, Ksenija, "Distribution of fatty acids and alcohols in lignites, from the Smederevsko Pomoravlje field, Kostolac Basin – biogeochemical approach" in 7. simpozijum „Hemija i zaštita životne sredine“ sa međunarodnim učešćem (EnviroChem 2015) (2015):227-228.