TY  - JOUR
AU  - Xie, Chunxia
AU  - Antić, Nevena
AU  - Nadal-Romero, Estela
AU  - Yan, Luobin
AU  - Tosti, Tomislav
AU  - Đogo-Mračević, Svetlana
AU  - Tu, Xinjun
AU  - Kašanin-Grubin, Milica
PY  - 2022
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/4240
AB  - Climate variables including temperature, rainfall intensity, rainfall acidity, and lithological properties are among the most important factors affecting rock weathering. However, the relative contribution of these four factors on rock weathering, especially on chemical weathering, is still unclear. In this study, we carried out a series of weathering-leaching rainfall simulations on four types of badland sediments under controlled conditions of two levels of temperature, rainfall intensity, and rainfall acidity based on the real field data from representative weather scenarios. The main objectives are 1) to explore the progressive change of sample surface and leachate characteristics and 2) to reveal the independent effects of temperature, rainfall intensity, rainfall acidity, and lithology and their relative contribution as well, on both mechanical and chemical weathering. Qualitative analysis on crack development and fragmentation of sample surface and quantitative analysis on the leachate volume, pH, electrical conductivity, and total cation and anion releases of sample leachate together demonstrated that for the investigated sediments, under the conditions of temperature, intensity, and acidity of rain that can be achieved in nature, high drying temperature obviously increases mechanical disintegration by promoting the rate and magnitude of moisture variations (wetting–drying alterations), while high rainfall intensity and acid rain have no obvious effect. Impact and importance of the drying process caused by high temperature between wetting events need more attention, rather than high rainfall intensity. Low temperature, high rainfall intensity, and acid rain contributing more hydrogen ions required for cation exchanges, rock type with more soluble minerals, all promote chemical weathering, and the influence of climatic and lithological factors on chemical weathering decreases in the following order: mineral composition＞ rainfall intensity ＞ temperature ＞ rainfall acidity. Climatic variations on temperature can modify weathering processes and in that way conditioned hydro-geomorphological processes in badland areas. Such changes should be considered for direct and indirect implications on badland dynamics.
PB  - Frontiers Media S.A.
T2  - Frontiers in Earth Science
T1  - The Influences of Climatic and Lithological Factors on Weathering of Sediments in Humid Badland Areas
VL  - 10
DO  - 10.3389/feart.2022.900314
ER  - 

@article{
author = "Xie, Chunxia and Antić, Nevena and Nadal-Romero, Estela and Yan, Luobin and Tosti, Tomislav and Đogo-Mračević, Svetlana and Tu, Xinjun and Kašanin-Grubin, Milica",
year = "2022",
abstract = "Climate variables including temperature, rainfall intensity, rainfall acidity, and lithological properties are among the most important factors affecting rock weathering. However, the relative contribution of these four factors on rock weathering, especially on chemical weathering, is still unclear. In this study, we carried out a series of weathering-leaching rainfall simulations on four types of badland sediments under controlled conditions of two levels of temperature, rainfall intensity, and rainfall acidity based on the real field data from representative weather scenarios. The main objectives are 1) to explore the progressive change of sample surface and leachate characteristics and 2) to reveal the independent effects of temperature, rainfall intensity, rainfall acidity, and lithology and their relative contribution as well, on both mechanical and chemical weathering. Qualitative analysis on crack development and fragmentation of sample surface and quantitative analysis on the leachate volume, pH, electrical conductivity, and total cation and anion releases of sample leachate together demonstrated that for the investigated sediments, under the conditions of temperature, intensity, and acidity of rain that can be achieved in nature, high drying temperature obviously increases mechanical disintegration by promoting the rate and magnitude of moisture variations (wetting–drying alterations), while high rainfall intensity and acid rain have no obvious effect. Impact and importance of the drying process caused by high temperature between wetting events need more attention, rather than high rainfall intensity. Low temperature, high rainfall intensity, and acid rain contributing more hydrogen ions required for cation exchanges, rock type with more soluble minerals, all promote chemical weathering, and the influence of climatic and lithological factors on chemical weathering decreases in the following order: mineral composition＞ rainfall intensity ＞ temperature ＞ rainfall acidity. Climatic variations on temperature can modify weathering processes and in that way conditioned hydro-geomorphological processes in badland areas. Such changes should be considered for direct and indirect implications on badland dynamics.",
publisher = "Frontiers Media S.A.",
journal = "Frontiers in Earth Science",
title = "The Influences of Climatic and Lithological Factors on Weathering of Sediments in Humid Badland Areas",
volume = "10",
doi = "10.3389/feart.2022.900314"
}

Xie, C., Antić, N., Nadal-Romero, E., Yan, L., Tosti, T., Đogo-Mračević, S., Tu, X.,& Kašanin-Grubin, M.. (2022). The Influences of Climatic and Lithological Factors on Weathering of Sediments in Humid Badland Areas. in Frontiers in Earth Science
Frontiers Media S.A.., 10.
https://doi.org/10.3389/feart.2022.900314

Xie C, Antić N, Nadal-Romero E, Yan L, Tosti T, Đogo-Mračević S, Tu X, Kašanin-Grubin M. The Influences of Climatic and Lithological Factors on Weathering of Sediments in Humid Badland Areas. in Frontiers in Earth Science. 2022;10.
doi:10.3389/feart.2022.900314 .

Xie, Chunxia, Antić, Nevena, Nadal-Romero, Estela, Yan, Luobin, Tosti, Tomislav, Đogo-Mračević, Svetlana, Tu, Xinjun, Kašanin-Grubin, Milica, "The Influences of Climatic and Lithological Factors on Weathering of Sediments in Humid Badland Areas" in Frontiers in Earth Science, 10 (2022),
https://doi.org/10.3389/feart.2022.900314 . .

TY  - JOUR
AU  - Kašanin-Grubin, Milica
AU  - Hukić, Emira
AU  - Bellan, Michal
AU  - Bielak, Kamil
AU  - Bosela, Michal
AU  - Coll, Lluis
AU  - Czacharowski, Marcin
AU  - Gajica, Gordana
AU  - Giammarchi, Francesco
AU  - Gömöryová, Erika
AU  - Del Rio, Miren
AU  - Dinca, Lucian
AU  - Đogo-Mračević, Svetlana
AU  - Klopčić, Matija
AU  - Mitrović, Suzana
AU  - Pach, Maciej
AU  - Ranđelović, Dragana
AU  - Ruiz-Peinado, Ricardo
AU  - Skrzyszewski, Jerzy
AU  - Orlić, Jovana
AU  - Štrbac, Snežana
AU  - Stojadinović, Sanja
AU  - Tonon, Giustino
AU  - Tosti, Tomislav
AU  - Uhl, Enno
AU  - Veselinović, Gorica
AU  - Veselinović, Milorad
AU  - Zlatanov, Tzvetan
AU  - Tognetti, Roberto
PY  - 2022
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/4027
PB  - Canadian Science Publishing
T2  - Canadian Journal of Forest Research
T1  - Correction to: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361)
VL  - 52
IS  - 1
SP  - 135
DO  - 10.1139/cjfr-2021-0347
ER  - 

@article{
author = "Kašanin-Grubin, Milica and Hukić, Emira and Bellan, Michal and Bielak, Kamil and Bosela, Michal and Coll, Lluis and Czacharowski, Marcin and Gajica, Gordana and Giammarchi, Francesco and Gömöryová, Erika and Del Rio, Miren and Dinca, Lucian and Đogo-Mračević, Svetlana and Klopčić, Matija and Mitrović, Suzana and Pach, Maciej and Ranđelović, Dragana and Ruiz-Peinado, Ricardo and Skrzyszewski, Jerzy and Orlić, Jovana and Štrbac, Snežana and Stojadinović, Sanja and Tonon, Giustino and Tosti, Tomislav and Uhl, Enno and Veselinović, Gorica and Veselinović, Milorad and Zlatanov, Tzvetan and Tognetti, Roberto",
year = "2022",
publisher = "Canadian Science Publishing",
journal = "Canadian Journal of Forest Research",
title = "Correction to: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361)",
volume = "52",
number = "1",
pages = "135",
doi = "10.1139/cjfr-2021-0347"
}

Kašanin-Grubin, M., Hukić, E., Bellan, M., Bielak, K., Bosela, M., Coll, L., Czacharowski, M., Gajica, G., Giammarchi, F., Gömöryová, E., Del Rio, M., Dinca, L., Đogo-Mračević, S., Klopčić, M., Mitrović, S., Pach, M., Ranđelović, D., Ruiz-Peinado, R., Skrzyszewski, J., Orlić, J., Štrbac, S., Stojadinović, S., Tonon, G., Tosti, T., Uhl, E., Veselinović, G., Veselinović, M., Zlatanov, T.,& Tognetti, R.. (2022). Correction to: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361). in Canadian Journal of Forest Research
Canadian Science Publishing., 52(1), 135.
https://doi.org/10.1139/cjfr-2021-0347

Kašanin-Grubin M, Hukić E, Bellan M, Bielak K, Bosela M, Coll L, Czacharowski M, Gajica G, Giammarchi F, Gömöryová E, Del Rio M, Dinca L, Đogo-Mračević S, Klopčić M, Mitrović S, Pach M, Ranđelović D, Ruiz-Peinado R, Skrzyszewski J, Orlić J, Štrbac S, Stojadinović S, Tonon G, Tosti T, Uhl E, Veselinović G, Veselinović M, Zlatanov T, Tognetti R. Correction to: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361). in Canadian Journal of Forest Research. 2022;52(1):135.
doi:10.1139/cjfr-2021-0347 .

Kašanin-Grubin, Milica, Hukić, Emira, Bellan, Michal, Bielak, Kamil, Bosela, Michal, Coll, Lluis, Czacharowski, Marcin, Gajica, Gordana, Giammarchi, Francesco, Gömöryová, Erika, Del Rio, Miren, Dinca, Lucian, Đogo-Mračević, Svetlana, Klopčić, Matija, Mitrović, Suzana, Pach, Maciej, Ranđelović, Dragana, Ruiz-Peinado, Ricardo, Skrzyszewski, Jerzy, Orlić, Jovana, Štrbac, Snežana, Stojadinović, Sanja, Tonon, Giustino, Tosti, Tomislav, Uhl, Enno, Veselinović, Gorica, Veselinović, Milorad, Zlatanov, Tzvetan, Tognetti, Roberto, "Correction to: Soil erodibility in European mountain beech forests (Can. J. For. Res. 51, 12, 1846–1855, 2021, 10.1139/cjfr-2020-0361)" in Canadian Journal of Forest Research, 52, no. 1 (2022):135,
https://doi.org/10.1139/cjfr-2021-0347 . .

TY  - JOUR
AU  - Kašanin-Grubin, Milica
AU  - Hukić, Emira
AU  - Bellan, Michal
AU  - Bialek, Kamil
AU  - Bosela, Michal
AU  - Coll, Lluis
AU  - Czacharowski, Marcin
AU  - Gajica, Gordana
AU  - Giammarchi, Francesco
AU  - Gömöryová, Erika
AU  - Del Rio, Miren
AU  - Dinca, Lucian
AU  - Đogo-Mračević, Svetlana
AU  - Klopčić, Matija
AU  - Mitrović, Suzana
AU  - Pach, Maciej
AU  - Ranđelović, Dragana
AU  - Ruiz-Peinado, Ricardo
AU  - Skrzyszewski, Jerzy
AU  - Orlić, Jovana
AU  - Štrbac, Snežana
AU  - Stojadinović, Sanja
AU  - Tonon, Giustino
AU  - Tosti, Tomislav
AU  - Uhl, Enno
AU  - Veselinović, Gorica
AU  - Veselinović, Milorad
AU  - Zlatanov, Tzvetan
AU  - Tognetti, Roberto
PY  - 2021
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/4008
AB  - Forests in Europe are currently not endangered by soil erosion. However, this can change with climate change or with intensified forest management practices. Using a newly established network of plots in beech forests across Europe, the aims of this study were to (i) distinguish soil properties and erodibility indices in relation to bedrock, (ii) determine geochemical properties and organic carbon (Corg ) influencing erodibility, and (iii) assess the effect of soil depth on erodibility indices. Seventy-six soil samples from 20 beech forests were collected in 11 countries to quantify soil properties influencing erodibility indices: clay ratio, modified clay ratio, sodium adsorption ratio, and oxides ratio. The results indicate that the dominant soil properties, determined by bedrock, that correlate with forest soil erodibility indices are Corg, pH, electrical conductivity, calcium and sodium ions concentrations, total water-soluble cations, and the percentage of sand. According to the tested indices, soil susceptibility to erosion follows the order granite > andesite > sandstone > quartzite > limestone. Deeper soil horizons on granite are more susceptible to erosion than surface horizons are, but this is not the case for soils on limestones. In conclusion, forest management should consider the predisposition of different soil types to erosion.
PB  - Canadian Science Publishing
T2  - Canadian Journal of Forest Research
T1  - Soil erodibility in european mountain beech forests
VL  - 51
IS  - 12
SP  - 1846
EP  - 1855
DO  - 10.1139/cjfr-2020-0361
ER  - 

@article{
author = "Kašanin-Grubin, Milica and Hukić, Emira and Bellan, Michal and Bialek, Kamil and Bosela, Michal and Coll, Lluis and Czacharowski, Marcin and Gajica, Gordana and Giammarchi, Francesco and Gömöryová, Erika and Del Rio, Miren and Dinca, Lucian and Đogo-Mračević, Svetlana and Klopčić, Matija and Mitrović, Suzana and Pach, Maciej and Ranđelović, Dragana and Ruiz-Peinado, Ricardo and Skrzyszewski, Jerzy and Orlić, Jovana and Štrbac, Snežana and Stojadinović, Sanja and Tonon, Giustino and Tosti, Tomislav and Uhl, Enno and Veselinović, Gorica and Veselinović, Milorad and Zlatanov, Tzvetan and Tognetti, Roberto",
year = "2021",
abstract = "Forests in Europe are currently not endangered by soil erosion. However, this can change with climate change or with intensified forest management practices. Using a newly established network of plots in beech forests across Europe, the aims of this study were to (i) distinguish soil properties and erodibility indices in relation to bedrock, (ii) determine geochemical properties and organic carbon (Corg ) influencing erodibility, and (iii) assess the effect of soil depth on erodibility indices. Seventy-six soil samples from 20 beech forests were collected in 11 countries to quantify soil properties influencing erodibility indices: clay ratio, modified clay ratio, sodium adsorption ratio, and oxides ratio. The results indicate that the dominant soil properties, determined by bedrock, that correlate with forest soil erodibility indices are Corg, pH, electrical conductivity, calcium and sodium ions concentrations, total water-soluble cations, and the percentage of sand. According to the tested indices, soil susceptibility to erosion follows the order granite > andesite > sandstone > quartzite > limestone. Deeper soil horizons on granite are more susceptible to erosion than surface horizons are, but this is not the case for soils on limestones. In conclusion, forest management should consider the predisposition of different soil types to erosion.",
publisher = "Canadian Science Publishing",
journal = "Canadian Journal of Forest Research",
title = "Soil erodibility in european mountain beech forests",
volume = "51",
number = "12",
pages = "1846-1855",
doi = "10.1139/cjfr-2020-0361"
}

Kašanin-Grubin, M., Hukić, E., Bellan, M., Bialek, K., Bosela, M., Coll, L., Czacharowski, M., Gajica, G., Giammarchi, F., Gömöryová, E., Del Rio, M., Dinca, L., Đogo-Mračević, S., Klopčić, M., Mitrović, S., Pach, M., Ranđelović, D., Ruiz-Peinado, R., Skrzyszewski, J., Orlić, J., Štrbac, S., Stojadinović, S., Tonon, G., Tosti, T., Uhl, E., Veselinović, G., Veselinović, M., Zlatanov, T.,& Tognetti, R.. (2021). Soil erodibility in european mountain beech forests. in Canadian Journal of Forest Research
Canadian Science Publishing., 51(12), 1846-1855.
https://doi.org/10.1139/cjfr-2020-0361

Kašanin-Grubin M, Hukić E, Bellan M, Bialek K, Bosela M, Coll L, Czacharowski M, Gajica G, Giammarchi F, Gömöryová E, Del Rio M, Dinca L, Đogo-Mračević S, Klopčić M, Mitrović S, Pach M, Ranđelović D, Ruiz-Peinado R, Skrzyszewski J, Orlić J, Štrbac S, Stojadinović S, Tonon G, Tosti T, Uhl E, Veselinović G, Veselinović M, Zlatanov T, Tognetti R. Soil erodibility in european mountain beech forests. in Canadian Journal of Forest Research. 2021;51(12):1846-1855.
doi:10.1139/cjfr-2020-0361 .

Kašanin-Grubin, Milica, Hukić, Emira, Bellan, Michal, Bialek, Kamil, Bosela, Michal, Coll, Lluis, Czacharowski, Marcin, Gajica, Gordana, Giammarchi, Francesco, Gömöryová, Erika, Del Rio, Miren, Dinca, Lucian, Đogo-Mračević, Svetlana, Klopčić, Matija, Mitrović, Suzana, Pach, Maciej, Ranđelović, Dragana, Ruiz-Peinado, Ricardo, Skrzyszewski, Jerzy, Orlić, Jovana, Štrbac, Snežana, Stojadinović, Sanja, Tonon, Giustino, Tosti, Tomislav, Uhl, Enno, Veselinović, Gorica, Veselinović, Milorad, Zlatanov, Tzvetan, Tognetti, Roberto, "Soil erodibility in european mountain beech forests" in Canadian Journal of Forest Research, 51, no. 12 (2021):1846-1855,
https://doi.org/10.1139/cjfr-2020-0361 . .

TY  - JOUR
AU  - Kašanin-Grubin, Milica
AU  - Hagemann, Lukas
AU  - Gajica, Gordana
AU  - Štrbac, Snežana
AU  - Jovančićević, Branimir
AU  - Vasić, Nebojša
AU  - Šajnović, Aleksandra
AU  - Đogo-Mračević, Svetlana
AU  - Schwarzbauer, Jan
PY  - 2020
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/3620
AB  - The objective of this study is geochronological investigation of sedimentological and inorganic composition, in the Danube Djerdap Lake sediments in order to obtain reliable information about former pollution. Eleven samples were taken from the 135-cm-deep sediment core drilled at the Orlova location. Since the core represents sediments deposited during 1972–2016, the sedimentation rate of ~ 3 cm year−1 was estimated. Grain size, mineralogical and geochemical composition was determined. Sediments are sandy silts and clayey silts, and only the deepest and shallowest layers contain > 30% of sand-size fraction. The highest concentrations of minor elements are found in the oldest sediment (1972–1977) as a consequence of the high flux of the material from variable sources. During the sedimentation period (1975–1990), the concentrations of analyzed elements are generally decreasing until the beginning of 1990s. After this period, there are two distinct decreases and two distinct increases in concentrations of elements. The fluctuations in minor element concentrations are a consequence of both natural and anthropogenic sources. Granitic rocks situated south are source of minerals that carry minor elements. Enrichment Factor, Geoaccumulation Index, Contamination Factor and Pollution Load Index indicate that concentrations of certain minor elements at specific depositional periods have anthropogenic source.
PB  - Springer Nature B.V.
T2  - Environmental Geochemistry and Health
T1  - Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition
VL  - 42
IS  - 2
SP  - 693
EP  - 707
DO  - 10.1007/s10653-019-00403-6
ER  - 

@article{
author = "Kašanin-Grubin, Milica and Hagemann, Lukas and Gajica, Gordana and Štrbac, Snežana and Jovančićević, Branimir and Vasić, Nebojša and Šajnović, Aleksandra and Đogo-Mračević, Svetlana and Schwarzbauer, Jan",
year = "2020",
abstract = "The objective of this study is geochronological investigation of sedimentological and inorganic composition, in the Danube Djerdap Lake sediments in order to obtain reliable information about former pollution. Eleven samples were taken from the 135-cm-deep sediment core drilled at the Orlova location. Since the core represents sediments deposited during 1972–2016, the sedimentation rate of ~ 3 cm year−1 was estimated. Grain size, mineralogical and geochemical composition was determined. Sediments are sandy silts and clayey silts, and only the deepest and shallowest layers contain > 30% of sand-size fraction. The highest concentrations of minor elements are found in the oldest sediment (1972–1977) as a consequence of the high flux of the material from variable sources. During the sedimentation period (1975–1990), the concentrations of analyzed elements are generally decreasing until the beginning of 1990s. After this period, there are two distinct decreases and two distinct increases in concentrations of elements. The fluctuations in minor element concentrations are a consequence of both natural and anthropogenic sources. Granitic rocks situated south are source of minerals that carry minor elements. Enrichment Factor, Geoaccumulation Index, Contamination Factor and Pollution Load Index indicate that concentrations of certain minor elements at specific depositional periods have anthropogenic source.",
publisher = "Springer Nature B.V.",
journal = "Environmental Geochemistry and Health",
title = "Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition",
volume = "42",
number = "2",
pages = "693-707",
doi = "10.1007/s10653-019-00403-6"
}

Kašanin-Grubin, M., Hagemann, L., Gajica, G., Štrbac, S., Jovančićević, B., Vasić, N., Šajnović, A., Đogo-Mračević, S.,& Schwarzbauer, J.. (2020). Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition. in Environmental Geochemistry and Health
Springer Nature B.V.., 42(2), 693-707.
https://doi.org/10.1007/s10653-019-00403-6

Kašanin-Grubin M, Hagemann L, Gajica G, Štrbac S, Jovančićević B, Vasić N, Šajnović A, Đogo-Mračević S, Schwarzbauer J. Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition. in Environmental Geochemistry and Health. 2020;42(2):693-707.
doi:10.1007/s10653-019-00403-6 .

Kašanin-Grubin, Milica, Hagemann, Lukas, Gajica, Gordana, Štrbac, Snežana, Jovančićević, Branimir, Vasić, Nebojša, Šajnović, Aleksandra, Đogo-Mračević, Svetlana, Schwarzbauer, Jan, "Geochronological investigation of the Danube Djerdap Lake sediments (Serbia): sedimentology and inorganic composition" in Environmental Geochemistry and Health, 42, no. 2 (2020):693-707,
https://doi.org/10.1007/s10653-019-00403-6 . .

TY  - JOUR
AU  - Kašanin-Grubin, Milica
AU  - Štrbac, Snežana
AU  - Antonijević, Snežana
AU  - Đogo-Mračević, Svetlana
AU  - Ranđelović, Dragana
AU  - Orlić, Jovana
AU  - Šajnović, Aleksandra
PY  - 2019
UR  - https://farfar.pharmacy.bg.ac.rs/handle/123456789/3449
AB  - The Great War Island (GWI) is an area of importance for the protection of the environment, cultural and historical heritage of Belgrade, Serbia. According to the International Union for Conservation of Nature (IUCN) this area belongs to the IV category - Habitats and Other Regulated Areas. The main objectives of this paper are to evaluate the potential impacts of pollution on ecosystem services of the Great War Island and to explore different scenarios for future urban development of the Great War Island that will have implication for human well-being. The aims of this paper are set up based on the evaluation of ecosystem services of the Great War Island and assessment of the pollution status of the Great War Island. In order to evaluate pollution status of the GWI inorganic and organic composition of sediments were examined. Additionally, the content of microelements was determined in the leaves of the Salix alba L. Pollution indices indicate that all investigated sampling sites are polluted and correspond to high and very high degree of contamination. Cd and Cu show high to extremely high degree of contamination while Sb has extremely high degree of contamination. Content of As, Co, Cu, Ni and Zn in leaves of Salix alba L. is in sufficient to normal range, while content of Cd is between the sufficient and excessive values generalized for various species. Typical oil distributions of terpanes and steranes and values of the corresponding maturity parameters clearly indicated that the sediments of the GWI, in addition to native organic matter, contained oil pollutants of anthropogenic origin. GWI provides provisioning, regulating, supporting and cultural ecosystem services. In relation to ecosystem services two possible scenarios can be predicted: first - losing the status of a protected area due to urbanization; and the second - increasing the degree of protection by admission into international protection lists.
PB  - Elsevier
T2  - Journal of Environmental Management
T1  - Future environmental challenges of the urban protected area Great War Island (Belgrade, Serbia) based on valuation of the pollution status and ecosystem services
VL  - 251
SP  - 1
EP  - 12
DO  - 10.1016/j.jenvman.2019.109574
ER  - 

@article{
author = "Kašanin-Grubin, Milica and Štrbac, Snežana and Antonijević, Snežana and Đogo-Mračević, Svetlana and Ranđelović, Dragana and Orlić, Jovana and Šajnović, Aleksandra",
year = "2019",
abstract = "The Great War Island (GWI) is an area of importance for the protection of the environment, cultural and historical heritage of Belgrade, Serbia. According to the International Union for Conservation of Nature (IUCN) this area belongs to the IV category - Habitats and Other Regulated Areas. The main objectives of this paper are to evaluate the potential impacts of pollution on ecosystem services of the Great War Island and to explore different scenarios for future urban development of the Great War Island that will have implication for human well-being. The aims of this paper are set up based on the evaluation of ecosystem services of the Great War Island and assessment of the pollution status of the Great War Island. In order to evaluate pollution status of the GWI inorganic and organic composition of sediments were examined. Additionally, the content of microelements was determined in the leaves of the Salix alba L. Pollution indices indicate that all investigated sampling sites are polluted and correspond to high and very high degree of contamination. Cd and Cu show high to extremely high degree of contamination while Sb has extremely high degree of contamination. Content of As, Co, Cu, Ni and Zn in leaves of Salix alba L. is in sufficient to normal range, while content of Cd is between the sufficient and excessive values generalized for various species. Typical oil distributions of terpanes and steranes and values of the corresponding maturity parameters clearly indicated that the sediments of the GWI, in addition to native organic matter, contained oil pollutants of anthropogenic origin. GWI provides provisioning, regulating, supporting and cultural ecosystem services. In relation to ecosystem services two possible scenarios can be predicted: first - losing the status of a protected area due to urbanization; and the second - increasing the degree of protection by admission into international protection lists.",
publisher = "Elsevier",
journal = "Journal of Environmental Management",
title = "Future environmental challenges of the urban protected area Great War Island (Belgrade, Serbia) based on valuation of the pollution status and ecosystem services",
volume = "251",
pages = "1-12",
doi = "10.1016/j.jenvman.2019.109574"
}

Kašanin-Grubin, M., Štrbac, S., Antonijević, S., Đogo-Mračević, S., Ranđelović, D., Orlić, J.,& Šajnović, A.. (2019). Future environmental challenges of the urban protected area Great War Island (Belgrade, Serbia) based on valuation of the pollution status and ecosystem services. in Journal of Environmental Management
Elsevier., 251, 1-12.
https://doi.org/10.1016/j.jenvman.2019.109574

Kašanin-Grubin M, Štrbac S, Antonijević S, Đogo-Mračević S, Ranđelović D, Orlić J, Šajnović A. Future environmental challenges of the urban protected area Great War Island (Belgrade, Serbia) based on valuation of the pollution status and ecosystem services. in Journal of Environmental Management. 2019;251:1-12.
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Kašanin-Grubin, Milica, Štrbac, Snežana, Antonijević, Snežana, Đogo-Mračević, Svetlana, Ranđelović, Dragana, Orlić, Jovana, Šajnović, Aleksandra, "Future environmental challenges of the urban protected area Great War Island (Belgrade, Serbia) based on valuation of the pollution status and ecosystem services" in Journal of Environmental Management, 251 (2019):1-12,
https://doi.org/10.1016/j.jenvman.2019.109574 . .