Simić, Vladimir

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  • Simić, Vladimir (6)
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Author's Bibliography

Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia)

Perunović, Tamara; Stojanović, Ksenija A.; Kašanin-Grubin, Milica; Šajnović, Aleksandra; Simić, Vladimir; Jovančićević, Branimir; Brčeski, Ilija

(Serbian Chemical Soc, Belgrade, 2015)

TY  - JOUR
AU  - Perunović, Tamara
AU  - Stojanović, Ksenija A.
AU  - Kašanin-Grubin, Milica
AU  - Šajnović, Aleksandra
AU  - Simić, Vladimir
AU  - Jovančićević, Branimir
AU  - Brčeski, Ilija
PY  - 2015
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/1991
AB  - The geochemical composition of the soils and underlying sediments in the Kremna Basin was investigated. The aim was to assess whether the observed heavy metal concentrations in the soil samples represent geogenic or anthropogenic contamination. The second objective was to show that geochemical data of underlying sediments should be used as a tool in the determination of the potential hazard for soil contamination. For this purpose, the contents of As, Cr, Cu, Hg, Ni, Pb and Zn of soil samples were compared with standard values, a reference soil sample and local background values of the underlying sediments. The soil samples were unpolluted regarding the contents of As, Hg, Pb and Zn. All samples had higher contents of Cr and Ni, whereas three samples had higher contents of Cu than the limit standard values. Geochemical parameters showed that the higher concentrations of Cr, Cu and Ni in the soils could be attributed to geogenic impact. This conclusion was supported by the Chemical Proxy of Alteration and Chemical Index of Weathering values, which indicated intense weathering of the sediments. The obtained results showed that the Kremna area is under slight to moderate hazard if a land use change would occur, and proved the importance of the geochemical composition of underlying sediments in the interpretation of heavy metal pollution.
PB  - Serbian Chemical Soc, Belgrade
T2  - Journal of the Serbian Chemical Society
T1  - Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia)
VL  - 80
IS  - 8
SP  - 1087
DO  - 10.2298/JSC140917108P
ER  - 
@article{
author = "Perunović, Tamara and Stojanović, Ksenija A. and Kašanin-Grubin, Milica and Šajnović, Aleksandra and Simić, Vladimir and Jovančićević, Branimir and Brčeski, Ilija",
year = "2015",
abstract = "The geochemical composition of the soils and underlying sediments in the Kremna Basin was investigated. The aim was to assess whether the observed heavy metal concentrations in the soil samples represent geogenic or anthropogenic contamination. The second objective was to show that geochemical data of underlying sediments should be used as a tool in the determination of the potential hazard for soil contamination. For this purpose, the contents of As, Cr, Cu, Hg, Ni, Pb and Zn of soil samples were compared with standard values, a reference soil sample and local background values of the underlying sediments. The soil samples were unpolluted regarding the contents of As, Hg, Pb and Zn. All samples had higher contents of Cr and Ni, whereas three samples had higher contents of Cu than the limit standard values. Geochemical parameters showed that the higher concentrations of Cr, Cu and Ni in the soils could be attributed to geogenic impact. This conclusion was supported by the Chemical Proxy of Alteration and Chemical Index of Weathering values, which indicated intense weathering of the sediments. The obtained results showed that the Kremna area is under slight to moderate hazard if a land use change would occur, and proved the importance of the geochemical composition of underlying sediments in the interpretation of heavy metal pollution.",
publisher = "Serbian Chemical Soc, Belgrade",
journal = "Journal of the Serbian Chemical Society",
title = "Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia)",
volume = "80",
number = "8",
pages = "1087",
doi = "10.2298/JSC140917108P"
}
Perunović, T., Stojanović, K. A., Kašanin-Grubin, M., Šajnović, A., Simić, V., Jovančićević, B.,& Brčeski, I.. (2015). Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia). in Journal of the Serbian Chemical Society
Serbian Chemical Soc, Belgrade., 80(8), 1087.
https://doi.org/10.2298/JSC140917108P
Perunović T, Stojanović KA, Kašanin-Grubin M, Šajnović A, Simić V, Jovančićević B, Brčeski I. Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia). in Journal of the Serbian Chemical Society. 2015;80(8):1087.
doi:10.2298/JSC140917108P .
Perunović, Tamara, Stojanović, Ksenija A., Kašanin-Grubin, Milica, Šajnović, Aleksandra, Simić, Vladimir, Jovančićević, Branimir, Brčeski, Ilija, "Geochemical investigation as a tool in the determination of the potential hazard for soil contamination (Kremna Basin, Serbia)" in Journal of the Serbian Chemical Society, 80, no. 8 (2015):1087,
https://doi.org/10.2298/JSC140917108P . .
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Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina)

Grba, Nenad; Šajnović, Aleksandra ; Stojanović, Ksenija A.; Simić, Vladimir; Jovančićević, Branimir; Roglić, Goran; Eric, Vladisav

(Elsevier Gmbh, Urban & Fischer Verlag, Jena, 2014)

TY  - JOUR
AU  - Grba, Nenad
AU  - Šajnović, Aleksandra

AU  - Stojanović, Ksenija A.
AU  - Simić, Vladimir
AU  - Jovančićević, Branimir
AU  - Roglić, Goran
AU  - Eric, Vladisav
PY  - 2014
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/1777
AB  - Sedimentary rocks from the saline formation of the Lopare Basin were investigated. Sediments contain a moderate amount of immature to marginally mature algal organic matter deposited under slightly reducing to anoxic and slightly saline to hypersaline conditions. Almost all of the samples contain beta-carotane in a relatively high quantity, and in some, it represents the most abundant compound in the total distribution of hydrocarbons. The objective of the study was to determine the conditions that are favourable to precursors of beta-carotene and/or the preservation of the carotenoid hydrocarbon skeleton. Moreover, the dominant transformation pathways of beta-carotene under different redox and salinity conditions, which lead to the formation of aromatic carotenoids were defined. Based on the content of beta-carotane, the examined sedimentary rocks are divided into groups A, B and C. Group A does not contain or contains up to 1% of beta-carotane, group B contains between 1 and 5% of beta-carotane, while group C contains more than 5% of 13-carotane in the overall distribution of hydrocarbons. The organic matter (OM) of the sediments of group A is characterized by a higher contribution of prokaryotic precursor organisms, in comparison with the other samples. The OM was deposited in a slightly saline reductive environment, with an increased erosion activity. This environment was unfavourable for the precursors of beta-carotene and/or for preservation of its hydrocarbon skeleton. Evidence for the degradation of the poliene chain in beta-carotene is the domination of monoaromatic compounds in the aromatic carotenoids distribution. The OM of sediments of groups B and C is similar, predominantly of algal origin deposited in a reducing to anoxic calm carbonate environment with salinity changes from hypersaline to saline. Such reduced to anoxic saline, but not hypersaline environments are most appropriate for precursors of beta-carotene and for the preservation of carotenoid skeleton. Cyclization and aromatization of polyene isoprenoid chain, whereby terminal groups remain the main pattern, is the main pathway of beta-carotene aromatization in anoxic hypersaline environments, whereas aromatization of terminal 1,1,5-trimethylcyclohexen-5-enyl groups and expulsion of toluene and m-xylene are typical for the reduced to anoxic saline environments. (C) 2013 Elsevier GmbH. All rights reserved.
PB  - Elsevier Gmbh, Urban & Fischer Verlag, Jena
T2  - Chemie der Erde-geochemistry
T1  - Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina)
VL  - 74
IS  - 1
SP  - 107
EP  - 123
DO  - 10.1016/j.chemer.2013.10.002
ER  - 
@article{
author = "Grba, Nenad and Šajnović, Aleksandra
 and Stojanović, Ksenija A. and Simić, Vladimir and Jovančićević, Branimir and Roglić, Goran and Eric, Vladisav",
year = "2014",
abstract = "Sedimentary rocks from the saline formation of the Lopare Basin were investigated. Sediments contain a moderate amount of immature to marginally mature algal organic matter deposited under slightly reducing to anoxic and slightly saline to hypersaline conditions. Almost all of the samples contain beta-carotane in a relatively high quantity, and in some, it represents the most abundant compound in the total distribution of hydrocarbons. The objective of the study was to determine the conditions that are favourable to precursors of beta-carotene and/or the preservation of the carotenoid hydrocarbon skeleton. Moreover, the dominant transformation pathways of beta-carotene under different redox and salinity conditions, which lead to the formation of aromatic carotenoids were defined. Based on the content of beta-carotane, the examined sedimentary rocks are divided into groups A, B and C. Group A does not contain or contains up to 1% of beta-carotane, group B contains between 1 and 5% of beta-carotane, while group C contains more than 5% of 13-carotane in the overall distribution of hydrocarbons. The organic matter (OM) of the sediments of group A is characterized by a higher contribution of prokaryotic precursor organisms, in comparison with the other samples. The OM was deposited in a slightly saline reductive environment, with an increased erosion activity. This environment was unfavourable for the precursors of beta-carotene and/or for preservation of its hydrocarbon skeleton. Evidence for the degradation of the poliene chain in beta-carotene is the domination of monoaromatic compounds in the aromatic carotenoids distribution. The OM of sediments of groups B and C is similar, predominantly of algal origin deposited in a reducing to anoxic calm carbonate environment with salinity changes from hypersaline to saline. Such reduced to anoxic saline, but not hypersaline environments are most appropriate for precursors of beta-carotene and for the preservation of carotenoid skeleton. Cyclization and aromatization of polyene isoprenoid chain, whereby terminal groups remain the main pattern, is the main pathway of beta-carotene aromatization in anoxic hypersaline environments, whereas aromatization of terminal 1,1,5-trimethylcyclohexen-5-enyl groups and expulsion of toluene and m-xylene are typical for the reduced to anoxic saline environments. (C) 2013 Elsevier GmbH. All rights reserved.",
publisher = "Elsevier Gmbh, Urban & Fischer Verlag, Jena",
journal = "Chemie der Erde-geochemistry",
title = "Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina)",
volume = "74",
number = "1",
pages = "107-123",
doi = "10.1016/j.chemer.2013.10.002"
}
Grba, N., Šajnović, A., Stojanović, K. A., Simić, V., Jovančićević, B., Roglić, G.,& Eric, V.. (2014). Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina). in Chemie der Erde-geochemistry
Elsevier Gmbh, Urban & Fischer Verlag, Jena., 74(1), 107-123.
https://doi.org/10.1016/j.chemer.2013.10.002
Grba N, Šajnović A, Stojanović KA, Simić V, Jovančićević B, Roglić G, Eric V. Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina). in Chemie der Erde-geochemistry. 2014;74(1):107-123.
doi:10.1016/j.chemer.2013.10.002 .
Grba, Nenad, Šajnović, Aleksandra
, Stojanović, Ksenija A., Simić, Vladimir, Jovančićević, Branimir, Roglić, Goran, Eric, Vladisav, "Preservation of diagenetic products of beta-carotene in sedimentary rocks from the Lopare Basin (Bosnia and Herzegovina)" in Chemie der Erde-geochemistry, 74, no. 1 (2014):107-123,
https://doi.org/10.1016/j.chemer.2013.10.002 . .
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Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia

Perunović, Tamara; Stojanović, Ksenija A.; Simić, Vladimir; Kašanin-Grubin, Milica; Šajnović, Aleksandra; Eric, Vladisav; Schwarzbauer, Jan; Vasić, Nebojša; Jovančićević, Branimir; Brčeski, Ilija

(Polish Geological Soc, Krakow, 2014)

TY  - JOUR
AU  - Perunović, Tamara
AU  - Stojanović, Ksenija A.
AU  - Simić, Vladimir
AU  - Kašanin-Grubin, Milica
AU  - Šajnović, Aleksandra
AU  - Eric, Vladisav
AU  - Schwarzbauer, Jan
AU  - Vasić, Nebojša
AU  - Jovančićević, Branimir
AU  - Brčeski, Ilija
PY  - 2014
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/1645
AB  - The Kremna Basin is located in south west Serbia, in the Zlatibor area, which is part of the Internal Dinarides. This basin is note worthy because of the type of bedrock drainage, which it represents. It was formed on ultrabasic rocks and volcanic materials that influenced the occurrence of organic matter (OM) in the basin fill. The objective of the study was to determine the organic geochemical characteristics of sediments from the central part of the Kremna Basin. The sediments studied belong to an intrabasinal facies, in which two sequences were distinguished. The lower sequence occurs at depths of 216-343 m, while the upper sequence is found from 13.5-216 m. At the start of basin development (265-343 m) sedimentation took place in shallow alkaline water, rich in Mg ions. Through time, a slight deepening of the basin occurred. This was followed by chemical deposition of carbonates (216-265 m). The most important change in the sedimentary environment occurred with the formation of sediments marking the transition between the sequences (at about 200 m). Sediments from the lower sequence are characterized by the dominance of dolomite and magnesite. There are indications of volcanic activity, i.e. tuff layers and the presence of searlesite. The upper sequence is characterized by the prevalence of calcite and dolomite. The amounts of MgO, Na2O and B are higher in the lower sequence, whereas the CaO content is higher in the upper sequence. The sediments contain different amounts of immature OM (late diagenesis). Biomarker analysis shows diverse precursors of the sedimentary OM: methanogenic archaea, photosynthetic green sulfur bacteria (Chlorobiaceae), bacterivorous ciliates, various bacteria, both photosynthetic and non-photosynthetic, the green unicellular microalga, Botryococcus braunii race A (exclusively in the upper sequence) and terrestrial plants. The lower sequence contains lower amount OM, composed primarily of kerogen II/III and III types, indicating a higher contribution of the allochtonous biomass of land plants from the lake catchment, particularly in the lower part. The sediments of the upper sequence are enriched in autochthonous aquatic OM, which comprises mostly kerogen I, I/II and II types. The transition from the lower sequence to the upper one is associated with a decrease in pristane to phytane ratio, gammacerane index and content of C-28 steroids, absence or significantly lower amount of squalane, absence of C-24 and C-25 regular isoprenoids, 8-methyl-2-methyl-2-(4,8,12-trimethyltridecyl) chroman and C-30 hop-17(21)-ene. Pyrolytic experiments showed that the sediments of the upper sequence, rich in aquatic OM, at a catagenetic stage could be a source of liquid hydrocarbons. The values of hopane, sterane and phenanthrene maturation parameters indicate that through pyrolysis at 400 degrees C the samples investigated reached a value of vitrinite reflectance equivalent of approximately 0.70%. It was estimated that the sediments should be found at depths of 2300-2900 m in order to become active source rocks. The calculated minimum temperature, necessary for catagenetic hydrocarbon generation, is between 103 and 107 degrees C.
PB  - Polish Geological Soc, Krakow
T2  - Annales Societatis Geologorum Poloniae
T1  - Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia
VL  - 84
IS  - 3
SP  - 185
EP  - 212
UR  - https://hdl.handle.net/21.15107/rcub_cherry_1645
ER  - 
@article{
author = "Perunović, Tamara and Stojanović, Ksenija A. and Simić, Vladimir and Kašanin-Grubin, Milica and Šajnović, Aleksandra and Eric, Vladisav and Schwarzbauer, Jan and Vasić, Nebojša and Jovančićević, Branimir and Brčeski, Ilija",
year = "2014",
abstract = "The Kremna Basin is located in south west Serbia, in the Zlatibor area, which is part of the Internal Dinarides. This basin is note worthy because of the type of bedrock drainage, which it represents. It was formed on ultrabasic rocks and volcanic materials that influenced the occurrence of organic matter (OM) in the basin fill. The objective of the study was to determine the organic geochemical characteristics of sediments from the central part of the Kremna Basin. The sediments studied belong to an intrabasinal facies, in which two sequences were distinguished. The lower sequence occurs at depths of 216-343 m, while the upper sequence is found from 13.5-216 m. At the start of basin development (265-343 m) sedimentation took place in shallow alkaline water, rich in Mg ions. Through time, a slight deepening of the basin occurred. This was followed by chemical deposition of carbonates (216-265 m). The most important change in the sedimentary environment occurred with the formation of sediments marking the transition between the sequences (at about 200 m). Sediments from the lower sequence are characterized by the dominance of dolomite and magnesite. There are indications of volcanic activity, i.e. tuff layers and the presence of searlesite. The upper sequence is characterized by the prevalence of calcite and dolomite. The amounts of MgO, Na2O and B are higher in the lower sequence, whereas the CaO content is higher in the upper sequence. The sediments contain different amounts of immature OM (late diagenesis). Biomarker analysis shows diverse precursors of the sedimentary OM: methanogenic archaea, photosynthetic green sulfur bacteria (Chlorobiaceae), bacterivorous ciliates, various bacteria, both photosynthetic and non-photosynthetic, the green unicellular microalga, Botryococcus braunii race A (exclusively in the upper sequence) and terrestrial plants. The lower sequence contains lower amount OM, composed primarily of kerogen II/III and III types, indicating a higher contribution of the allochtonous biomass of land plants from the lake catchment, particularly in the lower part. The sediments of the upper sequence are enriched in autochthonous aquatic OM, which comprises mostly kerogen I, I/II and II types. The transition from the lower sequence to the upper one is associated with a decrease in pristane to phytane ratio, gammacerane index and content of C-28 steroids, absence or significantly lower amount of squalane, absence of C-24 and C-25 regular isoprenoids, 8-methyl-2-methyl-2-(4,8,12-trimethyltridecyl) chroman and C-30 hop-17(21)-ene. Pyrolytic experiments showed that the sediments of the upper sequence, rich in aquatic OM, at a catagenetic stage could be a source of liquid hydrocarbons. The values of hopane, sterane and phenanthrene maturation parameters indicate that through pyrolysis at 400 degrees C the samples investigated reached a value of vitrinite reflectance equivalent of approximately 0.70%. It was estimated that the sediments should be found at depths of 2300-2900 m in order to become active source rocks. The calculated minimum temperature, necessary for catagenetic hydrocarbon generation, is between 103 and 107 degrees C.",
publisher = "Polish Geological Soc, Krakow",
journal = "Annales Societatis Geologorum Poloniae",
title = "Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia",
volume = "84",
number = "3",
pages = "185-212",
url = "https://hdl.handle.net/21.15107/rcub_cherry_1645"
}
Perunović, T., Stojanović, K. A., Simić, V., Kašanin-Grubin, M., Šajnović, A., Eric, V., Schwarzbauer, J., Vasić, N., Jovančićević, B.,& Brčeski, I.. (2014). Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia. in Annales Societatis Geologorum Poloniae
Polish Geological Soc, Krakow., 84(3), 185-212.
https://hdl.handle.net/21.15107/rcub_cherry_1645
Perunović T, Stojanović KA, Simić V, Kašanin-Grubin M, Šajnović A, Eric V, Schwarzbauer J, Vasić N, Jovančićević B, Brčeski I. Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia. in Annales Societatis Geologorum Poloniae. 2014;84(3):185-212.
https://hdl.handle.net/21.15107/rcub_cherry_1645 .
Perunović, Tamara, Stojanović, Ksenija A., Simić, Vladimir, Kašanin-Grubin, Milica, Šajnović, Aleksandra, Eric, Vladisav, Schwarzbauer, Jan, Vasić, Nebojša, Jovančićević, Branimir, Brčeski, Ilija, "Organic Geochemical Study of the Lower Miocene Kremna Basin, Serbia" in Annales Societatis Geologorum Poloniae, 84, no. 3 (2014):185-212,
https://hdl.handle.net/21.15107/rcub_cherry_1645 .
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Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia)

Životić, Dragana R.; Stojanović, Ksenija A.; Gržetić, Ivan; Jovančićević, Branimir; Cvetković, Olga; Šajnović, Aleksandra; Simić, Vladimir; Stojakovic, Rajko; Scheeder, Georg

(Elsevier Science Bv, Amsterdam, 2013)

TY  - JOUR
AU  - Životić, Dragana R.
AU  - Stojanović, Ksenija A.
AU  - Gržetić, Ivan
AU  - Jovančićević, Branimir
AU  - Cvetković, Olga
AU  - Šajnović, Aleksandra
AU  - Simić, Vladimir
AU  - Stojakovic, Rajko
AU  - Scheeder, Georg
PY  - 2013
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/1636
AB  - The Upper Miocene lignite from the Main coal seam in the D field, Kolubara basin, is a typical humic coal with huminite, liptinite and inertinite concentrations of up to 83.7 vol.%, 17.2 vol.% and 15.5 vol.%, respectively. In the huminite group, textinite and ulminite are the most abundant macerals with variable amounts of densinite and attrinite. Liptodetrinite and sporinite are the most common macerals of the liptinite group, while inertodetrinite is the most abundant maceral of the inertinite group. The mineral matter consists mostly of clay minerals. The main sources of organic matter were gymnosperms (conifers) and microbial biomass, followed by angiosperms. Based on composition of saturated and aromatic diterpenoids it has been established that coal forming plants belonged to the gymnosperm families Taxodiaceae, Podocarpaceae, Cupressaceae, Araucariaceae, Phyllocladaceae and Pinaceae. Peatification occurred in neutral to slightly acidic, fresh water environment Composition and distribution of biomarkers show that diagenetic changes of the organic matter were mainly governed by bacterial activity in a suboxic to oxic environment Based on distribution of aromatic diterpenoids a novel diagenetic pathway for transformation of abietane-type precursors under suboxic to oxic conditions is proposed. Variations in compositions of macerals and biomarkers are in concordance with pronounced seasonality during Pontian, which caused changes in the water level, redox conditions during peatification, and to some extent vegetation differences in the paleo-plant communities.
PB  - Elsevier Science Bv, Amsterdam
T2  - International Journal of Coal Geology
T1  - Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia)
VL  - 111
SP  - 5
EP  - 22
DO  - 10.1016/j.coal.2012.10.014
ER  - 
@article{
author = "Životić, Dragana R. and Stojanović, Ksenija A. and Gržetić, Ivan and Jovančićević, Branimir and Cvetković, Olga and Šajnović, Aleksandra and Simić, Vladimir and Stojakovic, Rajko and Scheeder, Georg",
year = "2013",
abstract = "The Upper Miocene lignite from the Main coal seam in the D field, Kolubara basin, is a typical humic coal with huminite, liptinite and inertinite concentrations of up to 83.7 vol.%, 17.2 vol.% and 15.5 vol.%, respectively. In the huminite group, textinite and ulminite are the most abundant macerals with variable amounts of densinite and attrinite. Liptodetrinite and sporinite are the most common macerals of the liptinite group, while inertodetrinite is the most abundant maceral of the inertinite group. The mineral matter consists mostly of clay minerals. The main sources of organic matter were gymnosperms (conifers) and microbial biomass, followed by angiosperms. Based on composition of saturated and aromatic diterpenoids it has been established that coal forming plants belonged to the gymnosperm families Taxodiaceae, Podocarpaceae, Cupressaceae, Araucariaceae, Phyllocladaceae and Pinaceae. Peatification occurred in neutral to slightly acidic, fresh water environment Composition and distribution of biomarkers show that diagenetic changes of the organic matter were mainly governed by bacterial activity in a suboxic to oxic environment Based on distribution of aromatic diterpenoids a novel diagenetic pathway for transformation of abietane-type precursors under suboxic to oxic conditions is proposed. Variations in compositions of macerals and biomarkers are in concordance with pronounced seasonality during Pontian, which caused changes in the water level, redox conditions during peatification, and to some extent vegetation differences in the paleo-plant communities.",
publisher = "Elsevier Science Bv, Amsterdam",
journal = "International Journal of Coal Geology",
title = "Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia)",
volume = "111",
pages = "5-22",
doi = "10.1016/j.coal.2012.10.014"
}
Životić, D. R., Stojanović, K. A., Gržetić, I., Jovančićević, B., Cvetković, O., Šajnović, A., Simić, V., Stojakovic, R.,& Scheeder, G.. (2013). Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia). in International Journal of Coal Geology
Elsevier Science Bv, Amsterdam., 111, 5-22.
https://doi.org/10.1016/j.coal.2012.10.014
Životić DR, Stojanović KA, Gržetić I, Jovančićević B, Cvetković O, Šajnović A, Simić V, Stojakovic R, Scheeder G. Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia). in International Journal of Coal Geology. 2013;111:5-22.
doi:10.1016/j.coal.2012.10.014 .
Životić, Dragana R., Stojanović, Ksenija A., Gržetić, Ivan, Jovančićević, Branimir, Cvetković, Olga, Šajnović, Aleksandra, Simić, Vladimir, Stojakovic, Rajko, Scheeder, Georg, "Petrological and geochemical composition of lignite from the D field, Kolubara basin (Serbia)" in International Journal of Coal Geology, 111 (2013):5-22,
https://doi.org/10.1016/j.coal.2012.10.014 . .
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Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia

Životić, Dragana R.; Wehner, Herman; Cvetković, Olga; Jovančićević, Branimir; Gržetić, Ivan; Scheeder, Georg; Vidal, Angelika; Šajnović, Aleksandra; Ercegovac, Marko; Simić, Vladimir

(Elsevier Science Bv, Amsterdam, 2008)

TY  - JOUR
AU  - Životić, Dragana R.
AU  - Wehner, Herman
AU  - Cvetković, Olga
AU  - Jovančićević, Branimir
AU  - Gržetić, Ivan
AU  - Scheeder, Georg
AU  - Vidal, Angelika
AU  - Šajnović, Aleksandra
AU  - Ercegovac, Marko
AU  - Simić, Vladimir
PY  - 2008
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/912
AB  - A petrological, organic geochemical and geochemical study was performed on coal samples from the Soko Mine, Soko Banja basin, Serbia. Ten coal and two carbonaceous clay samples were collected from fresh, working faces in the underground brown coal mine from different parts of the main coal seam. The Lower Miocene, low-rank coal of the Soko Mine is a typical humic coal with huminite concentrations of up to 76.2 vol.%, liptinite less than 14 vol.% and inertinite less than 11 vol.%. Ulminite is the most abundant maceral with variable amounts of densinite and clay minerals. Sporinite and resinite are the most common macerals of the liptinite group. Inertodetrinite is the most abundant maceral of the inertinite group. The mineral-bituminous groundmass identified in some coal samples, and carbonaceous marly clay, indicate sub-aquatic origin and strong bacterial decomposition. The mean random huminite reflectance (ulminite B) for the main coal seam is 0.40 +/- 0.05% Rr, which is typical for an immature to early mature stage of organic matter. The extract yields from the coal of the Soko Banja basin ranges from 9413 to 14,096 ppm, in which alkanes constituted 1.02-0.1%, aromatics 1.3-14.7%, asphaltenes 28.1-76.2% and resins 20.2-43.5%. The saturated hydrocarbon fractions included n-C-15 to n-C-32, with an odd carbon number that predominate in almost all the samples. The contents of n-C-27 and n-C-29 alkanes are extremely high in some samples, as a contribution of epicuticular waxes from higher plants. Acyclic isoprenoid hydrocarbons are minor constituents in the aliphatic fraction, and the pristane/phytane (Pr/Ph) ratio varies between 0.56 and 3.13, which implies anaerobic to oxic conditions during sedimentation. The most abundant diterpanes were abietane, dehydroabietane and 16 alpha(H)-phyllocladane. In samples from the upper part of the coal seam, diterpanes are the dominant constituents of the alkane fraction. Polycyclic alkanes of the triterpane type are important constituents of alkane fractions. The occurrence of beta beta- and alpha beta-type hopanes from C-27 to C-31, but without C-28, is typical for the Soko Banja coals. The major and trace elements in the coal were analysed using X-ray fluorescence (XRF), and inductively coupled plasma-mass spectrometry (ICP-MS). In comparison with world lignites, using the geometric mean value, the coal from the Soko Banja Basin has a high content of strontium (306.953 mg/kg). Higher values than the world lignites were obtained for Mo (3.614 mg/kg), Ni(8.119 mg/kg), Se (0.884 mg/kg), U (2.642 mg/kg) and W (0.148 mg/kg). Correlation analysis shows inorganic affinity for almost all the major and trace elements, except for S, which has an organic affinity. (c) 2007 Elsevier B.V. All rights reserved.
PB  - Elsevier Science Bv, Amsterdam
T2  - International Journal of Coal Geology
T1  - Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia
VL  - 73
IS  - 3-4
SP  - 285
EP  - 306
DO  - 10.1016/j.coal.2007.07.001
ER  - 
@article{
author = "Životić, Dragana R. and Wehner, Herman and Cvetković, Olga and Jovančićević, Branimir and Gržetić, Ivan and Scheeder, Georg and Vidal, Angelika and Šajnović, Aleksandra and Ercegovac, Marko and Simić, Vladimir",
year = "2008",
abstract = "A petrological, organic geochemical and geochemical study was performed on coal samples from the Soko Mine, Soko Banja basin, Serbia. Ten coal and two carbonaceous clay samples were collected from fresh, working faces in the underground brown coal mine from different parts of the main coal seam. The Lower Miocene, low-rank coal of the Soko Mine is a typical humic coal with huminite concentrations of up to 76.2 vol.%, liptinite less than 14 vol.% and inertinite less than 11 vol.%. Ulminite is the most abundant maceral with variable amounts of densinite and clay minerals. Sporinite and resinite are the most common macerals of the liptinite group. Inertodetrinite is the most abundant maceral of the inertinite group. The mineral-bituminous groundmass identified in some coal samples, and carbonaceous marly clay, indicate sub-aquatic origin and strong bacterial decomposition. The mean random huminite reflectance (ulminite B) for the main coal seam is 0.40 +/- 0.05% Rr, which is typical for an immature to early mature stage of organic matter. The extract yields from the coal of the Soko Banja basin ranges from 9413 to 14,096 ppm, in which alkanes constituted 1.02-0.1%, aromatics 1.3-14.7%, asphaltenes 28.1-76.2% and resins 20.2-43.5%. The saturated hydrocarbon fractions included n-C-15 to n-C-32, with an odd carbon number that predominate in almost all the samples. The contents of n-C-27 and n-C-29 alkanes are extremely high in some samples, as a contribution of epicuticular waxes from higher plants. Acyclic isoprenoid hydrocarbons are minor constituents in the aliphatic fraction, and the pristane/phytane (Pr/Ph) ratio varies between 0.56 and 3.13, which implies anaerobic to oxic conditions during sedimentation. The most abundant diterpanes were abietane, dehydroabietane and 16 alpha(H)-phyllocladane. In samples from the upper part of the coal seam, diterpanes are the dominant constituents of the alkane fraction. Polycyclic alkanes of the triterpane type are important constituents of alkane fractions. The occurrence of beta beta- and alpha beta-type hopanes from C-27 to C-31, but without C-28, is typical for the Soko Banja coals. The major and trace elements in the coal were analysed using X-ray fluorescence (XRF), and inductively coupled plasma-mass spectrometry (ICP-MS). In comparison with world lignites, using the geometric mean value, the coal from the Soko Banja Basin has a high content of strontium (306.953 mg/kg). Higher values than the world lignites were obtained for Mo (3.614 mg/kg), Ni(8.119 mg/kg), Se (0.884 mg/kg), U (2.642 mg/kg) and W (0.148 mg/kg). Correlation analysis shows inorganic affinity for almost all the major and trace elements, except for S, which has an organic affinity. (c) 2007 Elsevier B.V. All rights reserved.",
publisher = "Elsevier Science Bv, Amsterdam",
journal = "International Journal of Coal Geology",
title = "Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia",
volume = "73",
number = "3-4",
pages = "285-306",
doi = "10.1016/j.coal.2007.07.001"
}
Životić, D. R., Wehner, H., Cvetković, O., Jovančićević, B., Gržetić, I., Scheeder, G., Vidal, A., Šajnović, A., Ercegovac, M.,& Simić, V.. (2008). Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia. in International Journal of Coal Geology
Elsevier Science Bv, Amsterdam., 73(3-4), 285-306.
https://doi.org/10.1016/j.coal.2007.07.001
Životić DR, Wehner H, Cvetković O, Jovančićević B, Gržetić I, Scheeder G, Vidal A, Šajnović A, Ercegovac M, Simić V. Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia. in International Journal of Coal Geology. 2008;73(3-4):285-306.
doi:10.1016/j.coal.2007.07.001 .
Životić, Dragana R., Wehner, Herman, Cvetković, Olga, Jovančićević, Branimir, Gržetić, Ivan, Scheeder, Georg, Vidal, Angelika, Šajnović, Aleksandra, Ercegovac, Marko, Simić, Vladimir, "Petrological, organic geochemical and geochemical characteristics of coal from the Soko mine, Serbia" in International Journal of Coal Geology, 73, no. 3-4 (2008):285-306,
https://doi.org/10.1016/j.coal.2007.07.001 . .
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U and Th in some brown coals of Serbia and Montenegro and their environmental impact

Životić, Dragana R.; Gržetić, Ivan; Lorenz, Hans; Simić, Vladimir

(Springer Heidelberg, Heidelberg, 2008)

TY  - JOUR
AU  - Životić, Dragana R.
AU  - Gržetić, Ivan
AU  - Lorenz, Hans
AU  - Simić, Vladimir
PY  - 2008
UR  - https://cherry.chem.bg.ac.rs/handle/123456789/927
AB  - Goal, Scope and Background. The objective of this paper is to determine and compare the concentrations of U and Th in soft to hard brown (lignite to sub-bituminous) coals of Serbia and Montenegro. It also presents comparison of the obtained data on U and Th concentrations with the published data on coals located in some other countries of the world. Almost the whole coal production of Serbia and Montenegro is used as feed coals for combustion in thermal power plants. Methods. Channel samples from open pit and underground mines and core samples were collected for hard and soft brown coals. For the analysis the samples were decomposed using microwave technique. Obtained solutions containing U and Th were analyzed by inductively coupled plasma mass spectroscopy (ICP-MS) using NIST standards. Results. Concentration of U from the investigated basins and the corresponding mine fields ranges within 0.60-70.10 mg/kg, 0.65-3.20 mg/kg, 0.95-6.59 rng/kg, 1.20-6.05 mg/kg, 0.80-6.66 mg/kg, 0.18-89.90 mg/kg, 0.19-4.14 mg/kg, and 0.28-3.52 mg/kg for the Kostolac, Kolubara, Krepoljin, Sjenica, Soko Banja, Bogovina East field, Senje-Resavica and Pljevlja basins, respectively. Concentration of Th ranges within 0.20-2.60 mg/kg, 0.846.57 mg/kg, 1.48-6.48 mg/kg, 0.12-2.71 mg/kg, 0.13-4.95 mg/kg, 0.14-3.48 mg/kg, 0.29-3.56 mg/kg, and 0.17-1.89 mg/kg for the Kostolac, Kolubara, Krepoljin, Sjenica, Soko Banja, Bogovina East field, Senje-Resavica and Pljevlja basins, respectively. Discussion. Brown coal from Senje-Resavica, Kolubara, Kostolac and Pljevlja ischaracterized by low U concentration. Coals form the Krepoljin, Soko Banja and Sjenica basins have slightly higher U concentrations than the mentioned group. The highest concentration of U is characteristic for the coal from the Bogovina East field. Concentration of Th in coals from Serbia and Montenegro has proved to be low. Out of all investigated coal basins, only the coal from the Krepoljin and Kolubara basins has high concentration of Th. The hydrothermally altered rocks of the Timok dacite-andesite complex, representing the basement of the Bogovina basin, could be a potential source of U, especially at the bottom part of the Lower seam of the Bogovina East field. Conclusions. This study shows that brown coals in Serbia and Montenegro (soft to hard brown coals or lignite to sub-bituminous) contain low levels of U (5.30 mg/kg, average value and 2.10 mg/kg geometric mean value) and Th (1.80 mg/kg, average value and 1.12 mg/kg geometric mean value). There are some obvious differences in concentration of U and Th in coals from different basins in Serbia and Montenegro. The approximate value for U and Th release mainly from power plants was 644.33 t and 983.46 t, respectively within the period 1965-2000 for the studied mines in Serbia, and 23.76 t and 15.05 t for the Potrlica mine (Montenegro) within the period 1965-1997. Recommendations. The coals in Serbia and Montenegro show no identifiable unfavourable impact on the surrounding environment, due to low natural radioactive concentration of U and Th, but further investigations concerning human health should be performed. Perspectives. Preliminary research revealed that in some Serbian coals (and, particularly, parts of the coal seam) U and Th content are rather high. Such coals should be carefully studied, as well as U and Th concentrations in ash, fly ash, waste disposals, nearby soil and ground water. Further studies should include determination of the radioactivity of all these products, and estimation of possible health impact.
PB  - Springer Heidelberg, Heidelberg
T2  - Environmental Science and Pollution Research
T1  - U and Th in some brown coals of Serbia and Montenegro and their environmental impact
VL  - 15
IS  - 2
SP  - 155
EP  - 161
DO  - 10.1065/espr2006.08.332
ER  - 
@article{
author = "Životić, Dragana R. and Gržetić, Ivan and Lorenz, Hans and Simić, Vladimir",
year = "2008",
abstract = "Goal, Scope and Background. The objective of this paper is to determine and compare the concentrations of U and Th in soft to hard brown (lignite to sub-bituminous) coals of Serbia and Montenegro. It also presents comparison of the obtained data on U and Th concentrations with the published data on coals located in some other countries of the world. Almost the whole coal production of Serbia and Montenegro is used as feed coals for combustion in thermal power plants. Methods. Channel samples from open pit and underground mines and core samples were collected for hard and soft brown coals. For the analysis the samples were decomposed using microwave technique. Obtained solutions containing U and Th were analyzed by inductively coupled plasma mass spectroscopy (ICP-MS) using NIST standards. Results. Concentration of U from the investigated basins and the corresponding mine fields ranges within 0.60-70.10 mg/kg, 0.65-3.20 mg/kg, 0.95-6.59 rng/kg, 1.20-6.05 mg/kg, 0.80-6.66 mg/kg, 0.18-89.90 mg/kg, 0.19-4.14 mg/kg, and 0.28-3.52 mg/kg for the Kostolac, Kolubara, Krepoljin, Sjenica, Soko Banja, Bogovina East field, Senje-Resavica and Pljevlja basins, respectively. Concentration of Th ranges within 0.20-2.60 mg/kg, 0.846.57 mg/kg, 1.48-6.48 mg/kg, 0.12-2.71 mg/kg, 0.13-4.95 mg/kg, 0.14-3.48 mg/kg, 0.29-3.56 mg/kg, and 0.17-1.89 mg/kg for the Kostolac, Kolubara, Krepoljin, Sjenica, Soko Banja, Bogovina East field, Senje-Resavica and Pljevlja basins, respectively. Discussion. Brown coal from Senje-Resavica, Kolubara, Kostolac and Pljevlja ischaracterized by low U concentration. Coals form the Krepoljin, Soko Banja and Sjenica basins have slightly higher U concentrations than the mentioned group. The highest concentration of U is characteristic for the coal from the Bogovina East field. Concentration of Th in coals from Serbia and Montenegro has proved to be low. Out of all investigated coal basins, only the coal from the Krepoljin and Kolubara basins has high concentration of Th. The hydrothermally altered rocks of the Timok dacite-andesite complex, representing the basement of the Bogovina basin, could be a potential source of U, especially at the bottom part of the Lower seam of the Bogovina East field. Conclusions. This study shows that brown coals in Serbia and Montenegro (soft to hard brown coals or lignite to sub-bituminous) contain low levels of U (5.30 mg/kg, average value and 2.10 mg/kg geometric mean value) and Th (1.80 mg/kg, average value and 1.12 mg/kg geometric mean value). There are some obvious differences in concentration of U and Th in coals from different basins in Serbia and Montenegro. The approximate value for U and Th release mainly from power plants was 644.33 t and 983.46 t, respectively within the period 1965-2000 for the studied mines in Serbia, and 23.76 t and 15.05 t for the Potrlica mine (Montenegro) within the period 1965-1997. Recommendations. The coals in Serbia and Montenegro show no identifiable unfavourable impact on the surrounding environment, due to low natural radioactive concentration of U and Th, but further investigations concerning human health should be performed. Perspectives. Preliminary research revealed that in some Serbian coals (and, particularly, parts of the coal seam) U and Th content are rather high. Such coals should be carefully studied, as well as U and Th concentrations in ash, fly ash, waste disposals, nearby soil and ground water. Further studies should include determination of the radioactivity of all these products, and estimation of possible health impact.",
publisher = "Springer Heidelberg, Heidelberg",
journal = "Environmental Science and Pollution Research",
title = "U and Th in some brown coals of Serbia and Montenegro and their environmental impact",
volume = "15",
number = "2",
pages = "155-161",
doi = "10.1065/espr2006.08.332"
}
Životić, D. R., Gržetić, I., Lorenz, H.,& Simić, V.. (2008). U and Th in some brown coals of Serbia and Montenegro and their environmental impact. in Environmental Science and Pollution Research
Springer Heidelberg, Heidelberg., 15(2), 155-161.
https://doi.org/10.1065/espr2006.08.332
Životić DR, Gržetić I, Lorenz H, Simić V. U and Th in some brown coals of Serbia and Montenegro and their environmental impact. in Environmental Science and Pollution Research. 2008;15(2):155-161.
doi:10.1065/espr2006.08.332 .
Životić, Dragana R., Gržetić, Ivan, Lorenz, Hans, Simić, Vladimir, "U and Th in some brown coals of Serbia and Montenegro and their environmental impact" in Environmental Science and Pollution Research, 15, no. 2 (2008):155-161,
https://doi.org/10.1065/espr2006.08.332 . .
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